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Friday, October 7, 2022

Phylogenetic comparative methods

From Wikipedia, the free encyclopedia

Phylogenetic comparative methods (PCMs) use information on the historical relationships of lineages (phylogenies) to test evolutionary hypotheses. The comparative method has a long history in evolutionary biology; indeed, Charles Darwin used differences and similarities between species as a major source of evidence in The Origin of Species. However, the fact that closely related lineages share many traits and trait combinations as a result of the process of descent with modification means that lineages are not independent. This realization inspired the development of explicitly phylogenetic comparative methods. Initially, these methods were primarily developed to control for phylogenetic history when testing for adaptation; however, in recent years the use of the term has broadened to include any use of phylogenies in statistical tests. Although most studies that employ PCMs focus on extant organisms, many methods can also be applied to extinct taxa and can incorporate information from the fossil record.

PCMs can generally be divided into two types of approaches: those that infer the evolutionary history of some character (phenotypic or genetic) across a phylogeny and those that infer the process of evolutionary branching itself (diversification rates), though there are some approaches that do both simultaneously. Typically the tree that is used in conjunction with PCMs has been estimated independently (see computational phylogenetics) such that both the relationships between lineages and the length of branches separating them is assumed to be known.

Applications

Phylogenetic comparative approaches can complement other ways of studying adaptation, such as studying natural populations, experimental studies, and mathematical models. Interspecific comparisons allow researchers to assess the generality of evolutionary phenomena by considering independent evolutionary events. Such an approach is particularly useful when there is little or no variation within species. And because they can be used to explicitly model evolutionary processes occurring over very long time periods, they can provide insight into macroevolutionary questions, once the exclusive domain of paleontology.

Home range areas of 49 species of mammals in relation to their body size. Larger-bodied species tend to have larger home ranges, but at any given body size members of the order Carnivora (carnivores and omnivores) tend to have larger home ranges than ungulates (all of which are herbivores). Whether this difference is considered statistically significant depends on what type of analysis is applied
 
Testes mass of various species of Primates in relation to their body size and mating system. Larger-bodied species tend to have larger testes, but at any given body size species in which females tend to mate with multiple males have males with larger testes.

Phylogenetic comparative methods are commonly applied to such questions as:

Example: how does brain mass vary in relation to body mass?

Example: do canids have larger hearts than felids?

Example: do carnivores have larger home ranges than herbivores?

Example: where did endothermy evolve in the lineage that led to mammals?

Example: where, when, and why did placentas and viviparity evolve?

  • Does a trait exhibit significant phylogenetic signal in a particular group of organisms? Do certain types of traits tend to "follow phylogeny" more than others?

Example: are behavioral traits more labile during evolution?

  • Do species differences in life history traits trade-off, as in the so-called fast-slow continuum?

Example: why do small-bodied species have shorter life spans than their larger relatives?

Phylogenetically independent contrasts

The standardized contrasts are used in conventional statistical procedures, with the constraint that all regressions, correlations, analysis of covariance, etc., must pass through the origin.

Felsenstein proposed the first general statistical method in 1985 for incorporating phylogenetic information, i.e., the first that could use any arbitrary topology (branching order) and a specified set of branch lengths. The method is now recognized as an algorithm that implements a special case of what are termed phylogenetic generalized least-squares models. The logic of the method is to use phylogenetic information (and an assumed Brownian motion like model of trait evolution) to transform the original tip data (mean values for a set of species) into values that are statistically independent and identically distributed.

The algorithm involves computing values at internal nodes as an intermediate step, but they are generally not used for inferences by themselves. An exception occurs for the basal (root) node, which can be interpreted as an estimate of the ancestral value for the entire tree (assuming that no directional evolutionary trends [e.g., Cope's rule] have occurred) or as a phylogenetically weighted estimate of the mean for the entire set of tip species (terminal taxa). The value at the root is equivalent to that obtained from the "squared-change parsimony" algorithm and is also the maximum likelihood estimate under Brownian motion. The independent contrasts algebra can also be used to compute a standard error or confidence interval.

Phylogenetic generalized least squares (PGLS)

Probably the most commonly used PCM is phylogenetic generalized least squares (PGLS). This approach is used to test whether there is a relationship between two (or more) variables while accounting for the fact that lineage are not independent. The method is a special case of generalized least squares (GLS) and as such the PGLS estimator is also unbiased, consistent, efficient, and asymptotically normal. In many statistical situations where GLS (or, ordinary least squares [OLS]) is used residual errors ε are assumed to be independent and identically distributed random variables that are assumed to be normal

whereas in PGLS the errors are assumed to be distributed as

where V is a matrix of expected variance and covariance of the residuals given an evolutionary model and a phylogenetic tree. Therefore, it is the structure of residuals and not the variables themselves that show phylogenetic signal. This has long been a source of confusion in the scientific literature. A number of models have been proposed for the structure of V such as Brownian motion Ornstein-Uhlenbeck, and Pagel's λ model. (When a Brownian motion model is used, PGLS is identical to the independent contrasts estimator.) In PGLS, the parameters of the evolutionary model are typically co-estimated with the regression parameters.

PGLS can only be applied to questions where the dependent variable is continuously distributed; however, the phylogenetic tree can also be incorporated into the residual distribution of generalized linear models, making it possible to generalize the approach to a broader set of distributions for the response.

Phylogenetically informed Monte Carlo computer simulations

Data for a continuous-valued trait can be simulated in such a way that taxa at the tips of a hypothetical phylogenetic tree will exhibit phylogenetic signal, i.e., closely related species will tend to resemble each other.

Martins and Garland proposed in 1991 that one way to account for phylogenetic relations when conducting statistical analyses was to use computer simulations to create many data sets that are consistent with the null hypothesis under test (e.g., no correlation between two traits, no difference between two ecologically defined groups of species) but that mimic evolution along the relevant phylogenetic tree. If such data sets (typically 1,000 or more) are analyzed with the same statistical procedure that is used to analyze a real data set, then results for the simulated data sets can be used to create phylogenetically correct (or "PC") null distributions of the test statistic (e.g., a correlation coefficient, t, F). Such simulation approaches can also be combined with such methods as phylogenetically independent contrasts or PGLS (see above).

Phylogenetic Pseudoreplication.jpg

Sulfur cycle

From Wikipedia, the free encyclopedia
 
Sulfur cycle in general

The sulfur cycle is a biogeochemical cycle in which the sulfur moves between rocks, waterways and living systems. It is important in geology as it affects many minerals and in life because sulfur is an essential element (CHNOPS), being a constituent of many proteins and cofactors, and sulfur compounds can be used as oxidants or reductants in microbial respiration. The global sulfur cycle involves the transformations of sulfur species through different oxidation states, which play an important role in both geological and biological processes. Steps of the sulfur cycle are:

These are often termed as follows:

Assimilative sulfate reduction (see also sulfur assimilation) in which sulfate (SO2−
4
) is reduced by plants, fungi and various prokaryotes. The oxidation states of sulfur are +6 in sulfate and –2 in R–SH.
Desulfurization in which organic molecules containing sulfur can be desulfurized, producing hydrogen sulfide gas (H2S, oxidation state = –2). An analogous process for organic nitrogen compounds is deamination.
Oxidation of hydrogen sulfide produces elemental sulfur (S8), oxidation state = 0. This reaction occurs in the photosynthetic green and purple sulfur bacteria and some chemolithotrophs. Often the elemental sulfur is stored as polysulfides.
Oxidation in elemental sulfur by sulfur oxidizers produces sulfate.
Dissimilative sulfur reduction in which elemental sulfur can be reduced to hydrogen sulfide.
Dissimilative sulfate reduction in which sulfate reducers generate hydrogen sulfide from sulfate.

Sulfur oxidation state

Sulfur has four main oxidation states in nature, which are −2, +2, +4, and +6. The common sulfur species of each oxidation state are listed as follows:

S2−: H2S, (CH3)2S, BaS

S0: native, or elemental, sulfur

S2+: SCl2

S4+: SO2, sulfite (SO2−
3
)

S6+: SO2−
4
(H2SO4, CaSO4), SF6

Sulfur sources and sinks

Sulfur is found in oxidation states ranging from +6 in SO2−
4
to −2 in sulfides. Thus, elemental sulfur can either give or receive electrons depending on its environment. On the anoxic early Earth, most sulfur was present in minerals such as pyrite (FeS2). Over Earth history, the amount of mobile sulfur increased through volcanic activity as well as weathering of the crust in an oxygenated atmosphere. Earth's main sulfur sink is the oceans SO2−
4
, where it is the major oxidizing agent.

Mean acidifying emissions of different foods per 100 grams of protein
Food Types Acidifying Emissions (g SO2eq per 100 g protein)
Beef
343.6
Cheese
165.5
Pork
142.7
Lamb and Mutton
139.0
Farmed Crustaceans
133.1
Poultry
102.4
Farmed Fish
65.9
Eggs
53.7
Groundnuts
22.6
Peas
8.5
Tofu
6.7

When SO2−
4
is assimilated by organisms, it is reduced and converted to organic sulfur, which is an essential component of proteins. However, the biosphere does not act as a major sink for sulfur, instead the majority of sulfur is found in seawater or sedimentary rocks including: pyrite rich shales, evaporite rocks (anhydrite and baryte), and calcium and magnesium carbonates (i.e. carbonate-associated sulfate). The amount of sulfate in the oceans is controlled by three major processes:

  1. input from rivers
  2. sulfate reduction and sulfide re-oxidation on continental shelves and slopes
  3. burial of anhydrite and pyrite in the oceanic crust.

The primary natural source of sulfur to the atmosphere is sea spray or windblown sulfur-rich dust, neither of which is long lived in the atmosphere. In recent times, the large annual input of sulfur from the burning of coal and other fossil fuels has added a substantial amount SO2 which acts as an air pollutant. In the geologic past, igneous intrusions into coal measures have caused large scale burning of these measures, and consequential release of sulfur to the atmosphere. This has led to substantial disruption to the climate system, and is one of the proposed causes of the Permian–Triassic extinction event.

Dimethylsulfide [(CH3)2S or DMS] is produced by the decomposition of dimethylsulfoniopropionate (DMSP) from dying phytoplankton cells in the ocean's photic zone, and is the major biogenic gas emitted from the sea, where it is responsible for the distinctive “smell of the sea” along coastlines. DMS is the largest natural source of sulfur gas, but still only has a residence time of about one day in the atmosphere and a majority of it is redeposited in the oceans rather than making it to land. However, it is a significant factor in the climate system, as it is involved in the formation of clouds.

Biologically and thermochemically driven sulfate reduction

3′-phosphoadenosine-5′-phosphosulfate
(key intermediate in the sulfur cycle)

Through the dissimilatory sulfate reduction pathway, sulfate can be reduced either bacterially (bacterial sulfate reduction) or inorganically (thermochemical sulfate reduction). This pathway involves the reduction of sulfate by organic compounds to produce hydrogen sulfide, which occurs in both processes.

The main products and reactants of bacterial sulfate reduction (BSR) and thermochemical sulfate reduction (TSR) are very similar. For both, various organic compounds and dissolved sulfate are the reactants, and the products or by-products are as follows: H2S, CO2, carbonates, elemental sulfur and metal sulfides. However, the reactive organic compounds differ for BSR and TSR because of the mutually exclusive temperature regimes. Organic acids are the main organic reactants for BSR and branched/n-alkanes are the main organic reactants for TSR. The inorganic reaction products in BSR and TSR are H2S (HS) and HCO
3
(CO2).

These processes occur because there are two very different thermal regimes in which sulfate is reduced, particularly in low-temperature and high-temperature environments. BSR usually occurs at lower temperatures from 0−80 °C, while TSR happens at much higher temperatures around 100–140 °C. Temperatures for TSR are not as well defined; the lowest confirmed temperature is 127 °C and the highest temperatures occur in settings around 160−180 °C. These two different regimes appear because at higher temperatures most sulfate-reducing microbes can no longer metabolize due to the denaturation of proteins or deactivation of enzymes, so TSR takes over. However, in hot sediments around hydrothermal vents BSR can happen at temperatures up to 110 °C.

BSR and TSR occur at different depths. BSR takes place in low-temperature environments, which are shallower settings such as oil and gas fields. BSR can also take place in modern marine sedimentary environments such as stratified inland seas, continental shelves, organic-rich deltas, and hydrothermal sediments which have intense microbial sulfate reduction because of the high concentration of dissolved sulfate in the seawater. Additionally, the high amounts of hydrogen sulfide found in oil and gas fields is thought to arise from the oxidation of petroleum hydrocarbons by sulfate. Such reactions are known to occur by microbial processes but it is generally accepted that TSR is responsible for the bulk of these reactions, especially in deep or hot reservoirs. Thus, TSR occurs in deep reservoirs where the temperatures are much higher. BSR is geologically instantaneous in most geologic settings, while TSR occurs at rates in the order of hundreds of thousands of years. Although much slower than BSR, even TSR appears to be a geologically fairly fast process.

BSR in shallow environments and TSR in deep reservoirs are key processes in the oceanic sulfur cycle.  Approximately, 10% (of the total gas) of H2S is produced in BSR settings, whereas 90% of the H2S is produced in TSR settings. If there is more than a few percent of H2S in any deep reservoir, then it is assumed that TSR has taken over. This is due to the fact that thermal cracking of hydrocarbons doesn't provide more than a couple percent of H2S. The amount of H2S is affected by several factors such as, the availability of organic reactants and sulfate and the presence/availability of base and transition metals.

Sulfur-oxidizing bacteria in hydrothermal vents

Hydrothermal vents emit hydrogen sulfide that support the carbon fixation of chemolithotrophic bacteria that oxidize hydrogen sulfide with oxygen to produce elemental sulfur or sulfate. The chemical reactions are as follows:

CO2 + 4 H2S + O2 → CH2O + 4 S0 + 3 H2O
CO2 + H2S + O2 + H2O → CH2O + SO2–
4
+ 2 H+

In modern oceans, Thiomicrospira, Halothiobacillus, and Beggiatoa are primary sulfur oxidizing bacteria, and form chemosynthetic symbioses with animal hosts. The host provides metabolic substrates (e.g., CO2, O2, H2O) to the symbiont while the symbiont generates organic carbon for sustaining the metabolic activities of the host. The produced sulfate usually combines with the leached calcium ions to form gypsum, which can form widespread deposits on near mid-ocean spreading centers.

δ34S

Although there are 25 known isotopes of sulfur, only four are stable and of geochemical importance. Of those four, two (32S, light and 34S, heavy) comprise (99.22%) of sulfur on Earth. The vast majority (95.02%) of sulfur occurs as 32S with only 4.21% in 34S. The ratio of these two isotopes is fixed in the Solar System and has been since its formation. The bulk Earth sulfur isotopic ratio is thought to be the same as the ratio of 22.22 measured from the Canyon Diablo troilite (CDT), a meteorite. That ratio is accepted as the international standard and is therefore set at δ = 0.00. Deviation from 0.00 is expressed as the δ34S which is a ratio in per mill (‰). Positive values correlate to increased levels of 34S, whereas negative values correlate with greater 32S in a sample.

Formation of sulfur minerals through non-biogenic processes does not substantially differentiate between the light and heavy isotopes, therefore sulfur isotope ratios in gypsum or barite should be the same as the overall isotope ratio in the water column at their time of precipitation. Sulfate reduction through biologic activity strongly differentiates between the two isotopes because of the more rapid enzymic reaction with 32S. Sulfate metabolism results in an isotopic depletion of −18‰, and repeated cycles of oxidation and reduction can result in values up to −50‰. Average present day seawater values of δ34S are on the order of +21‰.

Throughout geologic history the sulfur cycle and the isotopic ratios have coevolved with the biosphere becoming overall more negative with the increases in biologically driven sulfate reduction, but also show substantial positive excursion. In general positive excursions in the sulfur isotopes mean that there is an excess of pyrite deposition rather than oxidation of sulfide minerals exposed on land.

Marine sulfur cycle

The sulfur cycle in marine environments has been well-studied via the tool of sulfur isotope systematics expressed as δ34S. The modern global oceans have sulfur storage of 1.3×1018 kg, mainly occurring as sulfate with the δ34S value of +21‰. The overall input flux is 1.0×1011 kg/a with the sulfur isotope composition of ~3‰. Riverine sulfate derived from the terrestrial weathering of sulfide minerals (δ34S = +6‰) is the primary input of sulfur to the oceans. Other sources are metamorphic and volcanic degassing and hydrothermal activity (δ34S = 0‰), which release reduced sulfur species (such as H2S and S0). There are two major outputs of sulfur from the oceans. The first sink is the burial of sulfate either as marine evaporites (such as gypsum) or carbonate-associated sulfate (CAS), which accounts for 6×1010 kg/a (δ34S = +21‰). The second sulfur sink is pyrite burial in shelf sediments or deep seafloor sediments (4×1010 kg/a; δ34S = −20‰). The total marine sulfur output flux is 1.0×1011 kg/a which matches the input fluxes, implying the modern marine sulfur budget is at steady state. The residence time of sulfur in modern global oceans is 13,000,000 years.

Evolution of the sulfur cycle

The isotopic composition of sedimentary sulfides provides primary information on the evolution of the sulfur cycle.

The total inventory of sulfur compounds on the surface of the Earth (nearly 1019 kg of sulfur) represents the total outgassing of sulfur through geologic time. Rocks analyzed for sulfur content are generally organic-rich shales meaning they are likely controlled by biogenic sulfur reduction. Average seawater curves are generated from evaporites deposited throughout geologic time because again, since they do not discriminate between the heavy and light sulfur isotopes, they should mimic the ocean composition at the time of deposition.

4.6 billion years ago (Ga) the Earth formed and had a theoretical δ34S value of 0. Since there was no biologic activity on early Earth there would be no isotopic fractionation. All sulfur in the atmosphere would be released during volcanic eruptions. When the oceans condensed on Earth, the atmosphere was essentially swept clean of sulfur gases, owing to their high solubility in water. Throughout the majority of the Archean (4.6–2.5 Ga) most systems appeared to be sulfate-limited. Some small Archean evaporite deposits require that at least locally elevated concentrations (possibly due to local volcanic activity) of sulfate existed in order for them to be supersaturated and precipitate out of solution.

3.8–3.6 Ga marks the beginning of the exposed geologic record because this is the age of the oldest rocks on Earth. Metasedimentary rocks from this time still have an isotopic value of 0 because the biosphere was not developed enough (possibly at all) to fractionate sulfur.

3.5 Ga anoxyogenic photosynthesis is established and provides a weak source of sulfate to the global ocean with sulfate concentrations incredibly low the δ34S is still basically 0. Shortly after, at 3.4 Ga the first evidence for minimal fractionation in evaporitic sulfate in association with magmatically derived sulfides can be seen in the rock record. This fractionation shows possible evidence for anoxygenic phototrophic bacteria.

2.8 Ga marks the first evidence for oxygen production through photosynthesis. This is important because there cannot be sulfur oxidation without oxygen in the atmosphere. This exemplifies the coevolution of the oxygen and sulfur cycles as well as the biosphere.

2.7–2.5 Ga is the age of the oldest sedimentary rocks to have a depleted δ 34S which provide the first compelling evidence for sulfate reduction.

2.3 Ga sulfate increases to more than 1 mM; this increase in sulfate is coincident with the "Great Oxygenation Event", when redox conditions on Earth's surface are thought by most workers to have shifted fundamentally from reducing to oxidizing. This shift would have led to an incredible increase in sulfate weathering which would have led to an increase in sulfate in the oceans. The large isotopic fractionations that would likely be associated with bacteria reduction are produced for the first time. Although there was a distinct rise in seawater sulfate at this time it was likely still only less than 5–15% of present-day levels.

At 1.8 Ga, Banded iron formations (BIF) are common sedimentary rocks throughout the Archean and Paleoproterozoic; their disappearance marks a distinct shift in the chemistry of ocean water. BIFs have alternating layers of iron oxides and chert. BIFs only form if the water is allowed to supersaturate in dissolved iron (Fe2+) meaning there cannot be free oxygen or sulfur in the water column because it would form Fe3+ (rust) or pyrite and precipitate out of solution. Following this supersaturation, the water must become oxygenated in order for the ferric rich bands to precipitate it must still be sulfur poor otherwise pyrite would form instead of Fe3+. It has been hypothesized that BIFs formed during the initial evolution of photosynthetic organisms that had phases of population growth, causing over production of oxygen. Due to this over production they would poison themselves causing a mass die off, which would cut off the source of oxygen and produce a large amount of CO2 through the decomposition of their bodies, allowing for another bacterial bloom. After 1.8 Ga sulfate concentrations were sufficient to increase rates of sulfate reduction to greater than the delivery flux of iron to the oceans.

Along with the disappearance of BIF, the end of the Paleoproterozoic also marks the first large scale sedimentary exhalative deposits showing a link between mineralization and a likely increase in the amount of sulfate in sea water. In the Paleoproterozoic the sulfate in seawater had increased to an amount greater than in the Archean, but was still lower than present day values. The sulfate levels in the Proterozoic also act as proxies for atmospheric oxygen because sulfate is produced mostly through weathering of the continents in the presence of oxygen. The low levels in the Proterozoic simply imply that levels of atmospheric oxygen fell between the abundances of the Phanerozoic and the deficiencies of the Archean.

750 million years ago (Ma) there is a renewed deposition of BIF which marks a significant change in ocean chemistry. This was likely due to snowball Earth episodes where the entire globe including the oceans was covered in a layer of ice cutting off oxygenation. In the late Neoproterozoic high carbon burial rates increased the atmospheric oxygen level to >10% of its present-day value. In the Latest Neoproterozoic another major oxidizing event occurred on Earth's surface that resulted in an anoxic deep ocean and possibly allowed for the appearance of multicellular life.

During the last 600 million years, seawater SO4 has generally varied between +10‰ and +30‰ in δ34S, with an average value close to that of today. Notably changes in seawater δ34S occurred during extinction and climatic events during this time.

Over a shorter time scale (ten million years) changes in the sulfur cycle are easier to observe and can be even better constrained with oxygen isotopes. Oxygen is continually incorporated into the sulfur cycle through sulfate oxidation and then released when that sulfate is reduced once again. Since different sulfate sources within the ocean have distinct oxygen isotopic values it may be possible to use oxygen to trace the sulfur cycle. Biological sulfate reduction preferentially selects lighter oxygen isotopes for the same reason that lighter sulfur isotopes are preferred. By studying oxygen isotopes in ocean sediments over the last 10 million years were able to better constrain the sulfur concentrations in sea water through that same time. They found that the sea level changes due to Pliocene and Pleistocene glacial cycles changed the area of continental shelves which then disrupted the sulfur processing, lowering the concentration of sulfate in the sea water. This was a drastic change as compared to preglacial times before 2 million years ago.

The Great Oxidation Event and sulfur isotope mass-independent fractionation

The Great Oxygenation Event (GOE) is characterized by the disappearance of sulfur isotope mass-independent fractionation (MIF) in the sedimentary records at around 2.45 billion years ago (Ga). The MIF of sulfur isotope (Δ33S) is defined by the deviation of measured δ33S value from the δ33S value inferred from the measured δ34S value according to the mass dependent fractionation law. The Great Oxidation Event represented a massive transition of global sulfur cycles. Before the Great Oxidation Event, the sulfur cycle was heavily influenced by the ultraviolet (UV) radiation and the associated photochemical reactions, which induced the sulfur isotope mass-independent fractionation (Δ33S ≠ 0). The preservation of sulfur isotope mass-independent fractionation signals requires the atmospheric O2 lower than 10−5 of present atmospheric level (PAL). The disappearance of sulfur isotope mass-independent fractionation at ~2.45 Ga indicates that atmospheric pO2 exceeded 10−5 present atmospheric level after the Great Oxygenation Event. Oxygen played an essential role in the global sulfur cycles after the Great Oxygenation Event, such as oxidative weathering of sulfides. The burial of pyrite in sediments in turn contributes to the accumulation of free O2 in Earth's surface environment.

Economic importance

Sulfur is intimately involved in production of fossil fuels and a majority of metal deposits because of its ability to act as an oxidizing or reducing agent. The vast majority of the major mineral deposits on Earth contain a substantial amount of sulfur including, but not limited to: sedimentary exhalative deposits (SEDEX), Carbonate-hosted lead-zinc ore deposits (Mississippi Valley-Type MVT) and porphyry copper deposits. Iron sulfides, galena and sphalerite will form as by-products of hydrogen sulfide generation, as long as the respective transition or base metals are present or transported to a sulfate reduction site. If the system runs out of reactive hydrocarbons economically viable elemental sulfur deposits may form. Sulfur also acts as a reducing agent in many natural gas reservoirs and generally ore forming fluids have a close relationship with ancient hydrocarbon seeps or vents.

Important sources of sulfur in ore deposits are generally deep-seated, but they can also come from local country rocks, sea water, or marine evaporites. The presence or absence of sulfur is one of the limiting factors on both the concentration of precious metals and its precipitation from solution. pH, temperature and especially redox states determine whether sulfides will precipitate. Most sulfide brines will remain in concentration until they reach reducing conditions, a higher pH or lower temperatures.

Ore fluids are generally linked to metal rich waters that have been heated within a sedimentary basin under the elevated thermal conditions typically in extensional tectonic settings. The redox conditions of the basin lithologies exert an important control on the redox state of the metal-transporting fluids and deposits can form from both oxidizing and reducing fluids. Metal-rich ore fluids tend to be by necessity comparatively sulfide deficient, so a substantial portion of the sulfide must be supplied from another source at the site of mineralization. Bacterial reduction of seawater sulfate or a euxinic (anoxic and H2S-containing) water column is a necessary source of that sulfide. When present, the δ34S values of barite are generally consistent with a seawater sulfate source, suggesting baryte formation by reaction between hydrothermal barium and sulfate in ambient seawater.

Once fossil fuels or precious metals are discovered and either burned or milled, the sulfur become a waste product which must be dealt with properly or it can become a pollutant. There has been a great increase in the amount of sulfur in our present day atmosphere because of the burning of fossil fuels. Sulfur acts as a pollutant and an economic resource at the same time.

Human impact

Human activities have a major effect on the global sulfur cycle. The burning of coal, natural gas, and other fossil fuels has greatly increased the amount of sulfur in the atmosphere and ocean and depleted the sedimentary rock sink. Without human impact sulfur would stay tied up in rocks for millions of years until it was uplifted through tectonic events and then released through erosion and weathering processes. Instead it is being drilled, pumped and burned at a steadily increasing rate. Over the most polluted areas there has been a 30-fold increase in sulfate deposition.

Although the sulfur curve shows shifts between net sulfur oxidation and net sulfur reduction in the geologic past, the magnitude of the current human impact is probably unprecedented in the geologic record. Human activities greatly increase the flux of sulfur to the atmosphere, some of which is transported globally. Humans are mining coal and extracting petroleum from the Earth's crust at a rate that mobilizes 150 x 1012 gS/yr, which is more than double the rate of 100 years ago. The result of human impact on these processes is to increase the pool of oxidized sulfur (SO4) in the global cycle, at the expense of the storage of reduced sulfur in the Earth's crust. Therefore, human activities do not cause a major change in the global pools of sulfur, but they do produce massive changes in the annual flux of sulfur through the atmosphere.

When SO2 is emitted as an air pollutant, it forms sulfuric acid through reactions with water in the atmosphere. Once the acid is completely dissociated in water the pH can drop to 4.3 or lower causing damage to both man-made and natural systems. According to the EPA, acid rain is a broad term referring to a mixture of wet and dry deposition (deposited material) from the atmosphere containing higher than normal amounts of nitric and sulfuric acids. Distilled water (water without any dissolved constituents), which contains no carbon dioxide, has a neutral pH of 7. Rain naturally has a slightly acidic pH of 5.6, because carbon dioxide and water in the air react together to form carbonic acid, a very weak acid. Around Washington, D.C., however, the average rain pH is between 4.2 and 4.4. Since pH is on a log scale dropping by 1 (the difference between normal rain water and acid rain) has a dramatic effect on the strength of the acid. In the United States, roughly two thirds of all SO2 and one fourth of all NO3 come from electric power generation that relies on burning fossil fuels, like coal.

As it is an important nutrient for plants, sulfur is increasingly used as a component of fertilizers. Recently sulfur deficiency has become widespread in many countries in Europe. Because of actions taken to limit acid rains atmospheric inputs of sulfur continue to decrease, As a result, the deficit in the sulfur input is likely to increase unless sulfur fertilizers are used.

Peak uranium

From Wikipedia, the free encyclopedia

Peak uranium is the point in time that the maximum global uranium production rate is reached. After that peak, according to Hubbert peak theory, the rate of production enters a terminal decline. While uranium is used in nuclear weapons, its primary use is for energy generation via nuclear fission of the uranium-235 isotope in a nuclear power reactor. Each kilogram of uranium-235 fissioned releases the energy equivalent of millions of times its mass in chemical reactants, as much energy as 2700 tons of coal, but uranium-235 accounts for only 0.7% of the mass of natural uranium. While Uranium-235 can be "bred" from 234
U
, a natural decay product of 238
U
present at 55 ppm in all natural uranium samples, Uranium-235 is ultimately a finite non-renewable resource. Due to the currently low price of uranium, the majority of commercial light water reactors operate on a "once through fuel cycle" which leaves virtually all the energy contained in the original 238
U
- which makes up over 99% of natural uranium - unused. Nuclear reprocessing is a technology currently used at industrial scale in France, Russia and Japan, which can recover part of that energy by producing MOX fuel or Remix Fuel for use in conventional power generating light water reactors. However, at current uranium prices, this is widely deemed uneconomical if only the "input" side is considered.

Advances in breeder reactor technology could allow the current reserves of uranium to provide power for humanity for billions of years, thus making nuclear power a sustainable energy. However, in 2010 the International Panel on Fissile Materials said "After six decades and the expenditure of the equivalent of tens of billions of dollars, the promise of breeder reactors remains largely unfulfilled and efforts to commercialize them have been steadily cut back in most countries." But in 2016, the Russian BN-800 fast-neutron breeder reactor started producing commercially at full power (800 MWe), joining the previous BN-600. As of 2020, the Chinese CFR-600 is under construction after the success of the China Experimental Fast Reactor, based on the BN-800. These reactors are currently generating mostly electricity rather than new fuel because the abundance and low price of mined and reprocessed uranium oxide makes breeding uneconomical, but they can switch to breed new fuel and close the cycle as needed.

The CANDU reactor which was designed to be fueled with natural uranium is capable of using spent fuel from Light Water Reactors as fuel, since it contains more fissile material than natural uranium. Research into "DUPIC" - direct use of PWR spent fuel in CANDU type reactors - is ongoing and could increase the usability of fuel without the need for reprocessing.

M. King Hubbert created his peak theory in 1956 for a variety of finite resources such as coal, oil, and natural gas. He and others since have argued that if the nuclear fuel cycle can be closed, uranium could become equivalent to renewable energy sources as concerns its availability. Breeding and nuclear reprocessing potentially would allow the extraction of the largest amount of energy from natural uranium. However, only a small amount of uranium is currently being bred into plutonium and only a small amount of fissile uranium and plutonium is being recovered from nuclear waste worldwide. Furthermore, the technologies to eliminate the waste in the nuclear fuel cycle do not yet exist. Since the nuclear fuel cycle is effectively not closed, Hubbert peak theory may be applicable.

Pessimistic predictions of future high-grade uranium production operate on the thesis that either the peak has already occurred in the 1980s or that a second peak may occur sometime around 2035.

As of 2017, identified uranium reserves recoverable at US$130/kg were 6.14 million tons (compared to 5.72 million tons in 2015). At the rate of consumption in 2017, these reserves are sufficient for slightly over 130 years of supply. The identified reserves as of 2017 recoverable at US$260/kg are 7.99 million tons (compared to 7.64 million tons in 2015).

Optimistic predictions of nuclear fuel supply are based upon one of three possible scenarios.

  1. LWRs only consume about half of one percent of their uranium fuel while fast breeder reactors will consume closer to 99%. Currently, more than 80% of the World's reactors are Light Water Reactors (LWRs).
  2. Current reserves of uranium are about 5.3 million tons. Theoretically, 4.5 billion tons of uranium are available from sea water at about 10 times the current price of uranium. Currently no high volume seawater extraction systems exist. The Earth's crust contains approximately 65 trillion tons of uranium, of which about 32 thousand tons flow into oceans per year via rivers, which are themselves fed via geological cycles of erosion, subduction and uplift.
  3. Thorium (3–4 times as abundant as uranium) might be used when supplies of uranium are depleted. However, in 2010, the UK's National Nuclear Laboratory (NNL) concluded that for the short to medium term, "...the thorium fuel cycle does not currently have a role to play," in that it is "technically immature, and would require a significant financial investment and risk without clear benefits," and concluded that the benefits have been "overstated." Currently there are no commercially practical thorium reactors in operation.

If these predictions became reality, it would have the potential to increase the supply of nuclear fuel significantly.

Optimistic predictions claim that the supply is far more than demand and do not predict peak uranium.

Hubbert's peak and uranium

Uranium-235, the fissile isotope of uranium used in nuclear reactors, makes up about 0.7% of uranium from ore. It is the only naturally occurring isotope capable of directly generating nuclear power, and is a finite, non-renewable resource. It is believed that its availability follows M. King Hubbert's peak theory, which was developed to describe peak oil. Hubbert saw oil as a resource which would soon run out, but he believed that uranium had much more promise as an energy source, and that breeder reactors and nuclear reprocessing, which were new technologies at the time, would allow uranium to be a power source for a very long time. The technologies Hubbert envisioned would substantially reduce the rate of depletion of uranium-235, but they are still more costly than the "once-through" cycle, and have not been widely deployed to date. If these and other more costly technologies such as seawater extraction are used, any possible peak would occur in the very distant future.

According to the Hubbert Peak Theory, Hubbert's peaks are the points where production of a resource, has reached its maximum, and from then on, the rate of resource production enters a terminal decline. After a Hubbert's peak, the rate of supply of a resource no longer fulfills the previous demand rate. As a result of the law of supply and demand, at this point the market shifts from a buyer's market to a seller's market.

Many countries are not able to supply their own uranium demands any longer - some of them never were - and must import uranium from other countries. Thirteen countries have hit peak and exhausted their economically recoverable uranium resources at current prices.

In a similar manner to every other natural metal resource, for every tenfold increase in the cost per kilogram of uranium, there is a three-hundredfold increase in available lower quality ores that would then become economical. The theory could be observed in practice during the Uranium bubble of 2007 when an unprecedented price hike led to investments in the development of uranium mining of lower quality deposits which mostly became stranded assets after uranium prices returned to a lower level.

Uranium demand

World consumption of primary energy by energy type in terawatt-hours (TWh)

The world demand for uranium in 1996 was over 68 kilotonnes (150×106 lb) per year, and that number had been expected to increase to between 80 kilotonnes (180×106 lb) and 100 kilotonnes (220×106 lb) per year by 2025 due to the number of new nuclear power plants coming on line. However following the shutdown of many nuclear power plants after the Fukushima Daiichi nuclear disaster in 2011, demand had fallen to about 60 kilotonnes (130×106 lb) in 2015 and rose to 62.8 kilotonnes (138×106 lb) in 2017, with future forecasts uncertain.

According to Cameco Corporation, the demand for uranium is directly linked to the amount of electricity generated by nuclear power plants. Reactor capacity is growing slowly, reactors are being run more productively, with higher capacity factors, and reactor power levels. Improved reactor performance translates into greater uranium consumption.

Nuclear power stations of 1000 megawatt electrical generation capacity require around 200 tonnes (440×103 lb) of natural uranium per year. For example, the United States has 103 operating reactors with an average generation capacity of 950 MWe demanded over 22 kilotonnes (49×106 lb) of natural uranium in 2005. As the number of nuclear power plants increase, so does the demand for uranium.

Another factor to consider is population growth. Electricity consumption is determined in part by economic and population growth. According to data from the CIA's World Factbook, the world population currently (July 2020 est.) is more than 7.7 billion and it is increasing by 1.167% per year. This means a growth of about 211,000 persons every day. According to the UN, by 2050 it is estimated that the Earth's population will be 9.07 billion. 62% of the people will live in Africa, Southern Asia and Eastern Asia. The largest energy-consuming class in the history of earth is being produced in world's most populated countries, China and India. Both plan massive nuclear energy expansion programs. China intends to build 32 nuclear plants with 40,000 MWe capacity by 2020. According to the World Nuclear Association, India plans on bringing 20,000 MWe nuclear capacity on line by 2020, and aims to supply 25% of electricity from nuclear power by 2050. The World Nuclear Association believes nuclear energy could reduce the fossil fuel burden of generating the new demand for electricity.

As more fossil fuels are used to supply the growing energy needs of an increasing population, the more greenhouse gases are produced. Some proponents of nuclear power believe that building more nuclear power plants can reduce greenhouse emissions. For example, the Swedish utility Vattenfall studied the full life cycle emissions of different ways to produce electricity, and concluded that nuclear power produced 3.3 g/kWh of carbon dioxide, compared to 400.0 for natural gas and 700.0 for coal. Another study however shows this figure to be 84–130 g of CO2/kWh, with the figure rising dramatically as less concentrated ores are used in the future. It uses a wider scope for consideration than other studies including dismantling and disposal of the power station. The study assumes diesel oil for the thermal parts of the uranium extraction process.

As some countries are not able to supply their own needs of uranium economically, countries have resorted to importing uranium ore from elsewhere. For example, owners of U.S. nuclear power reactors bought 67 million pounds (30 kt) of natural uranium in 2006. Out of that 84%, or 56 million pounds (25 kt), were imported from foreign suppliers, according to the Energy Department.

Because of the improvements in gas centrifuge technology in the 2000s, replacing former gaseous diffusion plants, cheaper separative work units have enabled the economic production of more enriched uranium from a given amount of natural uranium, by re-enriching tails ultimately leaving a depleted uranium tail of lower enrichment. This has somewhat lowered the demand for natural uranium.

As nuclear power plants take a long time to build and refuelling is undertaken at sporadic, predictable intervals, uranium demand is rather predictable in the short term. It is also less dependent on short-term economic boom-bust cycles as nuclear power has one of strongest fixed costs to variable costs ratios (i.e. The marginal costs of running, rather than leaving idle an already constructed power plant are very low, compared to the capital costs of construction) and it is thus nearly never advisable to leave a nuclear power plant idle for economic reasons. However, nuclear policy can lead to short term fluctuations in demand, as evidenced by the German nuclear phaseout, which was decided upon by the government of Gerhard Schröder (1998-2005) reversed during the second Merkel cabinet (2009-2013) only for a reversal of that reversal to occur as a consequence of the Fukushima nuclear accident, which also led to the temporary shutdown of several German nuclear power plants.

Uranium supply

Uranium occurs naturally in many rocks, and even in seawater. However, like other metals, it is seldom sufficiently concentrated to be economically recoverable. Like any resource, uranium cannot be mined at any desired concentration. No matter the technology, at some point it is too costly to mine lower grade ores. One highly criticized life cycle study by Jan Willem Storm van Leeuwen suggested that below 0.01–0.02% (100–200 ppm) in ore, the energy required to extract and process the ore to supply the fuel, operate reactors and dispose properly comes close to the energy gained by using the uranium as a fissible material in the reactor. Researchers at the Paul Scherrer Institute who analyzed the Jan Willem Storm van Leeuwen paper however have detailed the number of incorrect assumptions of Jan Willem Storm van Leeuwen that led them to this evaluation, including their assumption that all the energy used in the mining of Olympic Dam is energy used in the mining of uranium, when that mine is predominantly a copper mine and uranium is produced only as a co-product, along with gold and other metals. The report by Jan Willem Storm van Leeuwen also assumes that all enrichment is done in the older and more energy intensive gaseous diffusion technology, however the less energy intensive gas centrifuge technology has produced the majority of the world's enriched uranium now for a number of decades.

An appraisal of nuclear power by a team at MIT in 2003, and updated in 2009, have stated that:

Most commentators conclude that a half century of unimpeded growth is possible, especially since resources costing several hundred dollars per kilogram (not estimated in the Red Book) would also be economically usable...We believe that the world-wide supply of uranium ore is sufficient to fuel the deployment of 1000 reactors over the next half century.

In the early days of the nuclear industry, uranium was thought to be very scarce, so a closed fuel cycle would be needed. Fast breeder reactors would be needed to create nuclear fuel for other power producing reactors. In the 1960s, new discoveries of reserves, and new uranium enrichment techniques allayed these concerns.

Mining companies usually consider concentrations greater than 0.075% (750 ppm) as ore, or rock economical to mine at current uranium market prices. There is around 40 trillion tons of uranium in Earth's crust, but most is distributed at low parts per million trace concentration over its 3 * 1019 ton mass. Estimates of the amount concentrated into ores affordable to extract for under $130 per kg can be less than a millionth of that total.

Uranium Grades
Source Concentration
Very high-grade ore – 20% U 200,000 ppm U
High-grade ore – 2% U 20,000 ppm U
Low-grade ore – 0.1% U 1,000 ppm U
Very low-grade ore – 0.01% U 100 ppm U
Granite 4–5 ppm U
Sedimentary rock 2 ppm U
Earth's continental crust (av) 2.8 ppm U
Seawater 0.003 ppm U

According to the OECD Redbook, the world consumed 62.8 kilotonnes (138×106 lb) of uranium in 2017 (compared to 67 kt in 2002). Of that, 59 kt was produced from primary sources, with the balance coming from secondary sources, in particular stockpiles of natural and enriched uranium, decommissioned nuclear weapons, the reprocessing of natural and enriched uranium and the re-enrichment of depleted uranium tails.

Economically extractable reserves of uranium (0.01% ore or better)
Ore concentration tonnes of uranium Ore type
>1% 10000 vein deposits
0.2–1% 2 million pegmatites,unconformity deposits
0.1–0.2% 80 million fossil placers, sandstones
0.02–0.1% 100 million lower grade fossil placers, sandstones
100–200 ppm 2 billion volcanic deposits

The table above assumes the fuel will be used in a LWR burner. Uranium becomes far more economical when used in a fast burner reactor such as the Integral Fast Reactor.

Production

10 countries are responsible for 94% of all uranium extraction.
 
World production of uranium 1995–2006

Peak uranium refers to the peak of the entire planet's uranium production. Like other Hubbert peaks, the rate of uranium production on Earth will enter a terminal decline. According to Robert Vance of the OECD's Nuclear Energy Agency, the world production rate of uranium has already reached its peak in 1980, amounting to 69,683 tonnes (150×106 lb) of U3O8 from 22 countries. However, this is not due to lack of production capacity. Historically, uranium mines and mills around the world have operated at about 76% of total production capacity, varying within a range of 57% and 89%. The low production rates have been largely attributable to excess capacity. Slower growth of nuclear power and competition from secondary supply significantly reduced demand for freshly mined uranium until very recently. Secondary supplies include military and commercial inventories, enriched uranium tails, reprocessed uranium and mixed oxide fuel.

According to data from the International Atomic Energy Agency, world production of mined uranium has peaked twice in the past: once, circa 1960 in response to stockpiling for military use, and again in 1980, in response to stockpiling for use in commercial nuclear power. Up until about 1990, the mined uranium production was in excess of consumption by power plants. But since 1990, consumption by power plants has outstripped the uranium being mined; the deficit being made up by liquidation of the military (through decommissioning of nuclear weapons) and civilian stockpiles. Uranium mining has increased since the mid-1990s, but is still less than the consumption by power plants.

The world's top uranium producers are Kazakhstan (39% of world production), Canada (22%) and Australia (10%). Other major producers include Namibia (6.7%), Niger (6%), and Russia (5%). In 1996, the world produced 39 kilotonnes (86×106 lb) of uranium. In 2005, the world primary mining production was 41,720 tonnes (92×106 lb) of uranium, 62% of the requirements of the power utilities. In 2017 the production had increased to 59,462 tonnes, 93% of the demand. The balance comes from inventories held by utilities and other fuel cycle companies, inventories held by governments, used reactor fuel that has been reprocessed, recycled materials from military nuclear programs and uranium in depleted uranium stockpiles. The plutonium from dismantled Cold War nuclear weapon stockpiles will be exhausted by 2013. The industry is trying to find and develop new uranium mines, mainly in Canada, Australia and Kazakhstan. Those under development in 2006 would fill half the gap.

Of the ten largest uranium mines in the world (Mc Arthur River, Ranger, Rossing, Kraznokamensk, Olympic Dam, Rabbit Lake, Akouta, Arlit, Beverly, and McClean Lake), by 2020, six will be depleted, two will be in their final stages, one will be upgrading and one will be producing.

World primary mining production fell 5% in 2006 over that in 2005. The biggest producers, Canada and Australia saw falls of 15% and 20%, with only Kazakhstan showing an increase of 21%. This can be explained by two major events that have slowed world uranium production. Canada's Cameco mine at Cigar Lake is the largest, highest-grade uranium mine in the world. In 2006 it flooded, and then flooded again in 2008 (after Cameco had spent $43 million – most of the money set aside – to correct the problem), causing Cameco to push back its earliest start-up date for Cigar Lake to 2011. Also, in March 2007, the market endured another blow when a cyclone struck the Ranger mine in Australia, which produces 5,500 tonnes (12×106 lb) of uranium a year. The mine's owner, Energy Resources of Australia, declared force majeure on deliveries and said production would be impacted into the second half of 2007. This caused some to speculate that peak uranium has arrived. In January 2018, McArthur River mine in Canada suspended production, the mine was producing 7000-8000 tonnes of Uranium per year from 2007 to 2017. The mine's owner, Cameco cited low uranium market prices as the reason to halt production and claims ramping production up to normal will take 18–24 months when the decision to re-open the mine is made.

Primary sources

About 96% of the global uranium reserves are found in these ten countries: Australia, Canada, Kazakhstan, South Africa, Brazil, Namibia, Uzbekistan, the United States, Niger, and Russia. Out of those the main producers are Kazakhstan (39% of world production), Canada (22%) and Australia (10%) are the major producers. In 1996, the world produced 39,000 tonnes of uranium, and in 2005, the world produced a peak of 41,720 tonnes of uranium. In 2017 this had increased to 59,462 tonnes, 93% of the world demand.

Various agencies have tried to estimate how long these primary resources will last, assuming a once-through cycle. The European Commission said in 2001 that at the current level of uranium consumption, known uranium resources would last 42 years. When added to military and secondary sources, the resources could be stretched to 72 years. Yet this rate of usage assumes that nuclear power continues to provide only a fraction of the world's energy supply. If electric capacity were increased six-fold, then the 72-year supply would last just 12 years. The world's present measured resources of uranium, economically recoverable at a price of US$130/kg according to the industry groups Organisation for Economic Co-operation and Development (OECD), Nuclear Energy Agency (NEA) and International Atomic Energy Agency (IAEA), are enough to last for "at least a century" at current consumption rates.[62][63] According to the World Nuclear Association, yet another industry group, assuming the world's current rate of consumption at 66,500 tonnes of uranium per year and the world's present measured resources of uranium (4.7–5.5 Mt) are enough to last for some 70–80 years.

Reserves

Reserves are the most readily available resources. Resources that are known to exist and easy to mine are called "Known conventional resources". Resources that are thought to exist but have not been mined are classified under "Undiscovered conventional resources".

The known uranium resources represent a higher level of assured resources than is normal for most minerals. Further exploration and higher prices will certainly, on the basis of present geological knowledge, yield further resources as present ones are used up. There was very little uranium exploration between 1985 and 2005, so the significant increase in exploration effort that we are now seeing could readily double the known economic resources. On the basis of analogies with other metal minerals, a doubling of price from price levels in 2007 could be expected to create about a tenfold increase in measured resources, over time.

Known conventional resources

Known conventional resources are "Reasonably Assured Resources" and "Estimated Additional Resources-I".

In 2006, about 4 million tons of conventional resources were thought to be sufficient at current consumption rates for about six decades (4.06 million tonnes at 65,000 tonnes per year). In 2011, this was estimated to be 7 million tonnes. Exploration for uranium has increased. From 1981 to 2007, annual exploration expenditures grew modestly, from 4 million US$ to 7 million US$. This skyrocketed to US$11 million in 2011. Consumption of uranium runs at around 75 000 t a year. This is less than production, and requires draw down of existing stocks.

About 96% of the global uranium reserves are found in these ten countries: Australia, Canada, Kazakhstan, South Africa, Brazil, Namibia, Uzbekistan, the United States, Niger, and Russia. The world's largest deposits of uranium are found in three countries. Australia has just over 30% of the world's reasonably assured resources and inferred resources of uranium – about 1.673 megatonnes (3.69×109 lb). Kazakhstan has about 12% of the world's reserves, or about 651 kilotonnes (1.4×109 lb). And Canada has 485 kilotonnes (1,100×106 lb) of uranium, representing about 9%.

Several countries in Europe no longer mine uranium (East Germany (1990), France (2001), Spain (2002) and Sweden (1969)); they were not major producers.

Undiscovered conventional resources

Undiscovered conventional resources can be broken up into two classifications "Estimated Additional Resources-II" and "Speculative Resources".

It will take a significant exploration and development effort to locate the remaining deposits and begin mining them. However, since the entire earth's geography has not been explored for uranium at this time, there is still the potential to discover exploitable resources. The OECD Redbook cites areas still open to exploration throughout the world. Many countries are conducting complete aeromagnetic gradiometer radiometric surveys to get an estimate the size of their undiscovered mineral resources. Combined with a gamma-ray survey, these methods can locate undiscovered uranium and thorium deposits. The U.S. Department of Energy conducted the first and only national uranium assessment in 1980 – the National Uranium Resource Evaluation (NURE) program.

Secondary resources

Secondary resources are essentially recovered uranium from other sources such as nuclear weapons, inventories, reprocessing and re-enrichment. Since secondary resources have exceedingly low discovery costs and very low production costs, they may have displaced a significant portion of primary production. Secondary uranium was and is available essentially instantly. However, new primary production will not be. Essentially, secondary supply is a "one-time" finite supply, with the exception of the re-processed fuel.

Uranium mining activity is cyclical, in 2009 80% of the requirements of power utilities were supplied by mines, in 2017 this had risen to 93%. The balance comes from inventories held by utilities and other fuel cycle companies, inventories held by governments, used reactor fuel that has been reprocessed, recycled materials from military nuclear programs and uranium in depleted uranium stockpiles.

The plutonium from dismantled cold war nuclear weapon stockpiles was a major source of nuclear fuel under the "Megatons to Megawatts" program which ended in December 2013. The industry developed new uranium mines, especially in Kazakhstan which now attributes to 31% of the world supply.

Inventories

Inventories are kept by a variety of organizations – government, commercial and others.

The US DOE keeps inventories for security of supply in order to cover for emergencies where uranium is not available at any price. In the event of a major supply disruption, the department may not have sufficient uranium to meet a severe uranium shortage in the United States.

Decommissioning nuclear weapons

Both the US and Russia have committed to recycle their nuclear weapons into fuel for electricity production. This program is known as the Megatons to Megawatts Program. Down blending 500 tonnes (1,100×103 lb) of Russian weapons high enriched uranium (HEU) will result in about 15 kilotonnes (33,000×103 lb) of low enriched uranium (LEU) over 20 years. This is equivalent to about 152 kilotonnes (340×106 lb) of natural U, or just over twice annual world demand. Since 2000, 30 tonnes (66×103 lb) of military HEU is displacing about 10.6 kilotonnes (23×106 lb) of uranium oxide mine production per year which represents some 13% of world reactor requirements.

Plutonium recovered from nuclear weapons or other sources can be blended with uranium fuel to produce a mixed-oxide fuel. In June 2000, the US and Russia agreed to dispose of 34 kilotonnes (75×106 lb) each of weapons-grade plutonium by 2014. The US undertook to pursue a self-funded dual track program (immobilization and MOX). The G-7 nations provided US$1 billion to set up Russia's program. The latter was initially MOX specifically designed for VVER reactors, the Russian version of the Pressurized Water Reactor (PWR), the high cost being because this was not part of Russia's fuel cycle policy. This MOX fuel for both countries is equivalent to about 12 kilotonnes (26×106 lb) of natural uranium. The U.S. also has commitments to dispose of 151 tonnes (330×103 lb) of non-waste HEU.

The Megatons to Megawatts program came to an end in 2013.

Reprocessing and recycling

Nuclear reprocessing, sometimes called recycling, is one method of mitigating the eventual peak of uranium production. It is most useful as part of a nuclear fuel cycle utilizing fast-neutron reactors since reprocessed uranium and reactor-grade plutonium both have isotopic compositions not optimal for use in today's thermal-neutron reactors. Although reprocessing of nuclear fuel is done in a few countries (France, United Kingdom, and Japan) the United States President banned reprocessing in the late 1970s due to the high costs and the risk of nuclear proliferation via plutonium. In 2005, U.S. legislators proposed a program to reprocess the spent fuel that has accumulated at power plants. At present prices, such a program is significantly more expensive than disposing spent fuel and mining fresh uranium.

Currently, there are eleven reprocessing plants in the world. Of these, two are large-scale commercially operated plants for the reprocessing of spent fuel elements from light water reactors with throughputs of more than 1 kilotonne (2.2×106 lb) of uranium per year. These are La Hague, France with a capacity of 1.6 kilotonnes (3.5×106 lb) per year and Sellafield, England at 1.2 kilotonnes (2.6×106 lb) uranium per year. The rest are small experimental plants. The two large-scale commercial reprocessing plants together can reprocess 2,800 tonnes of uranium waste annually.

Most of the spent fuel components can be recovered and recycled. About two-thirds of the U.S. spent fuel inventory is uranium. This includes residual fissile uranium-235 that can be recycled directly as fuel for heavy water reactors or enriched again for use as fuel in light water reactors.

Plutonium and uranium can be chemically separated from spent fuel. When used nuclear fuel is reprocessed using the de facto standard PUREX method, both plutonium and uranium are recovered separately. The spent fuel contains about 1% plutonium. Reactor-grade plutonium contains Pu-240 which has a high rate of spontaneous fission, making it an undesirable contaminant in producing safe nuclear weapons. Nevertheless, nuclear weapons can be made with reactor grade plutonium.

The spent fuel is primarily composed of uranium, most of which has not been consumed or transmuted in the nuclear reactor. At a typical concentration of around 96% by mass in the used nuclear fuel, uranium is the largest component of used nuclear fuel. The composition of reprocessed uranium depends on the time the fuel has been in the reactor, but it is mostly uranium-238, with about 1% uranium-235, 1% uranium-236 and smaller amounts of other isotopes including uranium-232. However, reprocessed uranium is also a waste product because it is contaminated and undesirable for reuse in reactors. During its irradiation in a reactor, uranium is profoundly modified. The uranium that leaves the reprocessing plant contains all the isotopes of uranium between uranium-232 and uranium-238 except uranium-237, which is rapidly transformed into neptunium-237. The undesirable isotopic contaminants are:

  • Uranium-232 (whose decay products emit strong gamma radiation making handling more difficult), and
  • Uranium-234 (which is fertile material but can affect reactivity differently from uranium-238).
  • Uranium-236 (which affects reactivity and absorbs neutrons without fissioning, becoming neptunium-237 which is one of the most difficult isotopes for long-term disposal in a deep geological repository)
  • Daughter products of uranium-232: bismuth-212, thallium-208.

At present, reprocessing and the use of plutonium as reactor fuel is far more expensive than using uranium fuel and disposing of the spent fuel directly – even if the fuel is only reprocessed once. However, nuclear reprocessing becomes more economically attractive, compared to mining more uranium, as uranium prices increase.

The total recovery rate 5 kilotonnes (11×106 lb)/yr from reprocessing currently is only a small fraction compared to the growing gap between the rate demanded 64.615 kilotonnes (142.45×106 lb)/yr and the rate at which the primary uranium supply is providing uranium 46.403 kilotonnes (102.30×106 lb)/yr.

Energy Returned on Energy Invested (EROEI) on uranium reprocessing is highly positive, though not as positive as the mining and enrichment of uranium, and the process can be repeated. Additional reprocessing plants may bring some economies of scale.

The main problems with uranium reprocessing are the cost of mined uranium compared to the cost of reprocessing, nuclear proliferation risks, the risk of major policy change, the risk of incurring large cleanup costs, stringent regulations for reprocessing plants, and the anti-nuclear movement.

Unconventional resources

Unconventional resources are occurrences that require novel technologies for their exploitation and/or use. Often unconventional resources occur in low-concentration. The exploitation of unconventional uranium requires additional research and development efforts for which there is no imminent economic need, given the large conventional resource base and the option of reprocessing spent fuel. Phosphates, seawater, uraniferous coal ash, and some type of oil shales are examples of unconventional uranium resources.

Phosphates

The soaring price of uranium may cause long-dormant operations to extract uranium from phosphate. Uranium occurs at concentrations of 50 to 200 parts per million in phosphate-laden earth or phosphate rock. As uranium prices increase, there has been interest in some countries in extraction of uranium from phosphate rock, which is normally used as the basis of phosphate fertilizers.

Worldwide, approximately 400 wet-process phosphoric acid plants were in operation. Assuming an average recoverable content of 100 ppm of uranium, and that uranium prices do not increase so that the main use of the phosphates are for fertilizers, this scenario would result in a maximum theoretical annual output of 3.7 kilotonnes (8.2×106 lb) U3O8.

Historical operating costs for the uranium recovery from phosphoric acid range from $48–$119/kg U3O8. In 2011, the average price paid for U3O8 in the United States was $122.66/kg.

There are 22 million tons of uranium in phosphate deposits. Recovery of uranium from phosphates is a mature technology; it has been utilized in Belgium and the United States, but high recovery costs limit the utilization of these resources, with estimated production costs in the range of US$60–100/kgU including capital investment, according to a 2003 OECD report for a new 100 tU/year project.

Seawater

Unconventional uranium resources include up to 4,000 megatonnes (8,800×109 lb) of uranium contained in sea water. Several technologies to extract uranium from sea water have been demonstrated at the laboratory scale.

In the mid-1990s extraction costs were estimated at 260 USD/kgU (Nobukawa, et al., 1994) but scaling up laboratory-level production to thousands of tonnes is unproven and may encounter unforeseen difficulties.

One method of extracting uranium from seawater is using a uranium-specific nonwoven fabric as an absorbent. The total amount of uranium recovered in an experiment in 2003 from three collection boxes containing 350 kg of fabric was >1 kg of yellow cake after 240 days of submersion in the ocean. According to the OECD, uranium may be extracted from seawater using this method for about US$300/kgU.

In 2006 the same research group stated: "If 2g-U/kg-adsorbent is submerged for 60 days at a time and used 6 times, the uranium cost is calculated to be 88,000 JPY/kgU, including the cost of adsorbent production, uranium collection, and uranium purification. When an extraction 6g of U per kg of adsorbent and 20 repetitions or more becomes possible, the uranium cost reduces to 15,000 yen. This price level is equivalent to that of the highest cost of the minable uranium. The lowest cost attainable now is 25,000 yen with 4g-U/kg-adsorbent used in the sea area of Okinawa, with 18 repetition uses. In this case, the initial investment to collect the uranium from seawater is 107.7 billion yen, which is 1/3 of the construction cost of a one gigawatt nuclear power plant."

In 2012, ORNL researchers announced the successful development of a new absorbent material dubbed HiCap, which vastly outperforms previous best adsorbents, which perform surface retention of solid or gas molecules, atoms or ions. "We have shown that our adsorbents can extract five to seven times more uranium at uptake rates seven times faster than the world's best adsorbents", said Chris Janke, one of the inventors and a member of ORNL's Materials Science and Technology Division. HiCap also effectively removes toxic metals from water, according to results verified by researchers at Pacific Northwest National Laboratory.

Among the other methods to recover uranium from sea water, two seem promising: algae bloom to concentrate uranium and nanomembrane filtering.

So far, no more than a very small amount of uranium has been recovered from sea water in a laboratory.

Uraniferous coal ash

Annual release of "technologically enhanced"/concentrated Naturally occurring radioactive material, uranium and thorium radioisotopes naturally found in coal and concentrated in heavy/bottom coal ash and airborne fly ash. As predicted by ORNL to cumulatively amount to 2.9 million tons over the 1937–2040 period, from the combustion of an estimated 637 billion tons of coal worldwide.

In particular, nuclear power facilities produce about 200,000 metric tons of low and intermediate level waste (LILW) and 10,000 metric tons of high level waste (HLW) (including spent fuel designated as waste) each year worldwide.

Although only several parts per million average concentration in coal before combustion (albeit more concentrated in ash), the theoretical maximum energy potential of trace uranium and thorium in coal (in breeder reactors) actually exceeds the energy released by burning the coal itself, according to a study by Oak Ridge National Laboratory.

From 1965 to 1967 Union Carbide operated a mill in North Dakota, United States burning uraniferous lignite and extracting uranium from the ash. The plant produced about 150 metric tons of U3O8 before shutting down.

An international consortium has set out to explore the commercial extraction of uranium from uraniferous coal ash from coal power stations located in Yunnan province, China. The first laboratory scale amount of yellowcake uranium recovered from uraniferous coal ash was announced in 2007. The three coal power stations at Xiaolongtang, Dalongtang and Kaiyuan have piled up their waste ash. Initial tests from the Xiaolongtang ash pile indicate that the material contains (160–180 parts per million uranium), suggesting a total of some 2.085 kilotonnes (4.60×106 lb) U3O8 could be recovered from that ash pile alone.

Oil shales

Some oil shales contain uranium, which may be recovered as a byproduct. Between 1946 and 1952, a marine type of Dictyonema shale was used for uranium production in Sillamäe, Estonia, and between 1950 and 1989 alum shale was used in Sweden for the same purpose.

Breeding

A breeder reactor produces more nuclear fuel than it consumes and thus can extend the uranium supply. It typically turns the dominant isotope in natural uranium, uranium-238, into fissile plutonium-239. This results in hundredfold increase in the amount of energy to be produced per mass unit of uranium, because U-238, which constitute 99.3% of natural uranium, is not used in conventional reactors which instead use U-235 which only represent 0.7% of natural uranium. In 1983, physicist Bernard Cohen proposed that the world supply of uranium is effectively inexhaustible, and could therefore be considered a form of renewable energy. He claims that fast breeder reactors, fueled by naturally-replenished uranium-238 extracted from seawater, could supply energy at least as long as the sun's expected remaining lifespan of five billion years, making them as sustainable in fuel availability terms as renewable energy sources. Despite this hypothesis there is no known economically viable method to extract sufficient quantities from sea water. Experimental techniques are under investigation.

There are two types of breeders: Fast breeders and thermal breeders.

Fast breeder

A fast breeder, in addition to consuming U-235, converts fertile U-238 into Pu-239, a fissile fuel. Fast breeder reactors are more expensive to build and operate, including the reprocessing, and could only be justified economically if uranium prices were to rise to pre-1980 values in real terms. About 20 fast-neutron reactors have already been operating, some since the 1950s, and one supplies electricity commercially. Over 300 reactor-years of operating experience have been accumulated. In addition to considerably extending the exploitable fuel supply, these reactors have an advantage in that they produce less long-lived transuranic wastes, and can consume nuclear waste from current light water reactors, generating energy in the process. Several countries have research and development programs for improving these reactors. For instance, one scenario in France is for half of the present nuclear capacity to be replaced by fast breeder reactors by 2050. China, India, and Japan plan large scale utilization of breeder reactors during the coming decades. (Following the crisis at Japan's Fukishima Daiichi nuclear power plant in 2011, Japan is revising its plans regarding future use of nuclear power. (See: Fukushima Daiichi nuclear disaster: Energy policy implications.))

The breeding of plutonium fuel in Fast Breeder Reactors (FBR), known as the plutonium economy, was for a time believed to be the future of nuclear power. But many of the commercial breeder reactors that have been built have been riddled with technical and budgetary problems. Some sources critical of breeder reactors have gone so far to call them the Supersonic Transport of the '80s.

Uranium turned out to be far more plentiful than anticipated, and the price of uranium declined rapidly (with an upward blip in the 1970s). This is why the US halted their use in 1977 and the UK abandoned the idea in 1994.

Fast Breeder Reactors, are called fast because they have no moderator slowing down the neutrons (light water, heavy water or graphite) and breed more fuel than they consume. The word 'fast' in fast breeder thus refers to the speed of the neutrons in the reactor's core. The higher the energy the neutrons have, the higher the breeding ratio or the more uranium that is changed into plutonium.

Significant technical and materials problems were encountered with FBRs, and geological exploration showed that scarcity of uranium was not going to be a concern for some time. By the 1980s, due to both factors, it was clear that FBRs would not be commercially competitive with existing light water reactors. The economics of FBRs still depend on the value of the plutonium fuel which is bred, relative to the cost of fresh uranium. Research continues in several countries with working prototypes Phénix in France, the BN-600 reactor in Russia, and the Monju in Japan.

On February 16, 2006, the United States, France and Japan signed an arrangement to research and develop sodium-cooled fast breeder reactors in support of the Global Nuclear Energy Partnership. Breeder reactors are also being studied under the Generation IV reactor program.

Early prototypes have been plagued with problems. The liquid sodium coolant is highly flammable, bursting into flames if it comes into contact with air and exploding if it comes into contact with water. Japan's fast breeder Monju Nuclear Power Plant has been scheduled to re-open in 2008, 13 years after a serious accident and fire involving a sodium leak. In 1997 France shut down its Superphenix reactor, while the Phenix, built earlier, closed as scheduled in 2009.

At higher uranium prices breeder reactors may be economically justified. Many nations have ongoing breeder research programs. China, India, and Japan plan large scale utilization of breeder reactors during the coming decades. 300 reactor-years experience has been gained in operating them.

As of June 2008 there are only two running commercial breeders and the rate of reactor-grade plutonium production is very small (20 tonnes/yr). The reactor grade plutonium is being processed into MOX fuel. Next to the rate at which uranium is being mined (46,403 tonnes/yr), this is not enough to stave off peak uranium; however, this is only because mined and reprocessed uranium oxide is plentiful and cheap, so breeding new fuel is uneconomical. They can switch to breed large amounts of new fuel as needed, and many more breeding reactors can be built in a short time span.

Thermal breeder

Thorium is an alternate fuel cycle to uranium. Thorium is three times more plentiful than uranium. Thorium-232 is in itself not fissile, but fertile. It can be made into fissile uranium-233 in a breeder reactor. In turn, the uranium-233 can be fissioned, with the advantage that smaller amounts of transuranics are produced by neutron capture, compared to uranium-235 and especially compared to plutonium-239.

Despite the thorium fuel cycle having a number of attractive features, development on a large scale can run into difficulties:

  • The resulting U-233 fuel is expensive to fabricate.
  • The U-233 chemically separated from the irradiated thorium fuel is highly radioactive.
  • Separated U-233 is always contaminated with traces of U-232
  • Thorium is difficult to recycle due to highly radioactive Th-228
  • If the U-233 can be separated on its own, it becomes a weapons proliferation risk
  • And, there are technical problems in reprocessing.

Advocates for liquid core and molten salt reactors such as LFTR claim that these technologies negate the above-mentioned thorium's disadvantages present in solid fueled reactors.

The first successful commercial reactor at the Indian Point power station in Buchanan, New York (Indian Point Unit 1) ran on Thorium. The first core did not live up to expectations.

Indian interest in thorium is motivated by their substantial reserves. Almost a third of the world's thorium reserves are in India. India's Department of Atomic Energy (DAE) says that it will construct a 500 MWe prototype reactor in Kalpakkam. There are plans for four breeder reactors of 500 MWe each - two in Kalpakkam and two more in a yet undecided location.

China has initiated a research and development project in thorium molten-salt breeder reactor technology. It was formally announced at the Chinese Academy of Sciences (CAS) annual conference in January 2011. Its ultimate target is to investigate and develop a thorium based molten salt breeder nuclear system in about 20 years. A 5 MWe research MSR is apparently under construction at Shanghai Institute of Applied Physics (under the academy) with 2015 target operation.

Supply-demand gap

Due to reduction in nuclear weapons stockpiles, a large amount of former weapons uranium was released for use in civilian nuclear reactors. As a result, starting in 1990, a significant portion of uranium nuclear power requirements were supplied by former weapons uranium, rather than newly mined uranium. In 2002, mined uranium supplied only 54 percent of nuclear power requirements. But as the supply of former weapons uranium has been used up, mining has increased, so that in 2012, mining provided 95 percent of reactor requirements, and the OCED Nuclear Energy Agency and the International Atomic Energy Agency projected that the gap in supply would be completely erased in 2013.[

Uranium demand, mining production and deficit
Country Uranium required 2006–08 % of world demand Indigenous mining production 2006 Deficit (-surplus)
 United States 18,918 tonnes (42×106 lb) 29.3% 2,000 tonnes (4.4×106 lb) 16,918 tonnes (37×106 lb)
 France 10,527 tonnes (23×106 lb) 16.3% 0 10,527 tonnes (23×106 lb)
 Japan 7,659 tonnes (17×106 lb) 11.8% 0 7,659 tonnes (17×106 lb)
 Russia 3,365 tonnes (7.4×106 lb) 5.2% 4,009 tonnes (8.8×106 lb) −644 tonnes (−1.4×106 lb)
 Germany 3,332 tonnes (7.3×106 lb) 5.2% 68.03 tonnes (0.1500×106 lb) 3,264 tonnes (7.2×106 lb)
 South Korea 3,109 tonnes (6.9×106 lb) 4.8% 0 3,109 tonnes (6.9×106 lb)
 United Kingdom 2,199 tonnes (4.8×106 lb) 3.4% 0 2,199 tonnes (4.8×106 lb)
Rest of the World 15,506 tonnes (34×106 lb) 24.0% 40,327 tonnes (89×106 lb) −24,821 tonnes (−55×106 lb)
Total 64,615 tonnes (140×106 lb) 100.0% 46,403 tonnes (100×106 lb) 18,211 tonnes (40×106 lb)

For individual nations

Eleven countries, Germany, the Czech Republic, France, DR Congo, Gabon, Bulgaria, Tajikistan, Hungary, Romania, Spain, Portugal and Argentina, have seen uranium production peak, and rely on imports for their nuclear programs. Other countries have reached their peak production of uranium and are currently on a decline.

  • Germany – Between 1946 and 1990, SDAG Wismut, the former East German uranium mining company, produced a total of around 220 kilotonnes (490×106 lb) of uranium. During its peak, production exceeded 7 kilotonnes (15×106 lb) per year. In 1990, uranium mining was discontinued as a consequence of the German unification. The company could not compete on the world market. The production cost of its uranium was three times the world market price. West Germany remained a net uranium importer throughout its existence but ran a small scale uranium mine at Menzenschwand in the Black Forest called Krunkelbach Pit which was closed at the end of the Cold War
  • India – having already hit its production peak, India is finding itself in making a tough choice between using its modest and dwindling uranium resources as a source to keep its weapons programs rolling or it can use them to produce electricity. Since India has abundant thorium reserves, it is switching to nuclear reactors powered by the thorium fuel cycle.
  • Sweden – Sweden started uranium production in 1965 but was never profitable. They stopped mining uranium in 1969. Sweden then embarked on a massive project based on American light water reactors. Nowadays, Sweden imports its uranium mostly from Canada, Australia and the former Soviet Union.
  • UK – 1981: The UK's uranium production peaked in 1981 and the supply is running out. Yet the UK still plans to build more nuclear power plants.
  • France – 1988: In France uranium production attained a peak of 3,394 tonnes (7.5×106 lb) in 1988. At the time, this was enough for France to meet the half of its reactor demand from domestic sources. By 1997, production was 1/5 of the 1991 levels. France markedly reduced its market share since 1997. In 2002, France ran out of uranium.
US uranium production peaked in 1960, and again in 1980 (US Energy Information Administration)
  • U.S. – 1980: The United States was the world's leading producer of uranium from 1953 until 1980, when annual US production peaked at 16,810 tonnes (37×106 lb) (U3O8) according to the OECD redbook. According to the CRB yearbook, US production the peak was at 19,822 tonnes (44×106 lb). The U.S. production hit another maximum in 1996 at 6.3 million pounds (2.9 kt) of uranium oxide (U3O8), then dipped in production for a few years. Between 2003 and 2007, there has been a 125% increase in production as demand for uranium has increased. However, as of 2008, production levels have not come back to 1980 levels.
Uranium mining production in the United States
Year 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009
U3O8 (Mil lb) 3.1 3.4 6.0 6.3 5.6 4.7 4.6 4.0 2.6 2.3 2.0 2.3 2.7 4.1 4.5 3.9 4.1
U3O8 (tonnes) 1,410 1,540 2,700 2,860 2,540 2,130 2,090 1,800 1,180 1,040 910 1,040 1,220 1,860 2,040 1,770 1,860

Uranium mining declined with the last open pit mine shutting down in 1992 (Shirley Basin, Wyoming). United States production occurred in the following states (in descending order): New Mexico, Wyoming, Colorado, Utah, Texas, Arizona, Florida, Washington, and South Dakota. The collapse of uranium prices caused all conventional mining to cease by 1992. "In-situ" recovery or ISR has continued primarily in Wyoming and adjacent Nebraska as well has recently restarted in Texas.

  • Canada – 1959, 2001?: The first phase of Canadian uranium production peaked at more than 12 kilotonnes (26×106 lb) in 1959. The 1970s saw renewed interest in exploration and resulted in major discoveries in northern Saskatchewan's Athabasca Basin. Production peaked its uranium production a second time at 12,522 tonnes (28×106 lb) in 2001. Experts believe that it will take more than ten years to open new mines.

World peak uranium

Historical opinions of world uranium supply limits

In 1943, Alvin M. Weinberg et al. believed that there were serious limitations on nuclear energy if only U-235 were used as a nuclear power plant fuel. They concluded that breeding was required to usher in the age of nearly endless energy.

In 1956, M. King Hubbert declared world fissionable reserves adequate for at least the next few centuries, assuming breeding and reprocessing would be developed into economical processes.

In 1975 the US Department of the Interior, Geological Survey, distributed the press release "Known US Uranium Reserves Won't Meet Demand". It was recommended that the US not depend on foreign imports of uranium.

Pessimistic predictions

"We could use up all the uranium fuel we've found by as soon as 1989."
Panel from All-Atomic Comics (1976) citing pessimistic uranium supply predictions as an argument against nuclear power.

All the following sources predict peak uranium:

  • Edward Steidle, Dean of the School of Mineral Industries at Pennsylvania State College, predicted in 1952 that supplies of fissionable elements were too small to support commercial-scale energy production.
  • 1980 Robert Vance while looking back at 40 years of uranium production through all of the Red Books, found that peak global production was achieved in 1980 at 69,683 tonnes (150×106 lb) from 22 countries. In 2003, uranium production totaled 35,600 tonnes (78×106 lb) from 19 countries.
  • 1981 Michael Meacher, the former environment minister of the UK 1997–2003, and UK Member of Parliament, reports that peak uranium happened in 1981. He also predicts a major shortage of uranium sooner than 2013 accompanied with hoarding and its value pushed up to the levels of precious metals.
  • 1989–2015 M. C. Day projected that uranium reserves could run out as soon as 1989, but, more optimistically, would be exhausted by 2015.
  • 2034 Jan Willem Storm van Leeuwen, an independent analyst with Ceedata Consulting, contends that supplies of the high-grade uranium ore required to fuel nuclear power generation will, at current levels of consumption, last to about 2034. Afterwards, the cost of energy to extract the uranium will exceed the price the electric power provided.
  • 2035 The Energy Watch Group has calculated that, even with steep uranium prices, uranium production will have reached its peak by 2035 and that it will only be possible to satisfy the fuel demand of nuclear plants until then.

Various agencies have tried to estimate how long these resources will last.

  • The European Commission said in 2001 that at the current level of uranium consumption, known uranium resources would last 42 years. When added to military and secondary sources, the resources could be stretched to 72 years. Yet this rate of usage assumes that nuclear power continues to provide only a fraction of the world's energy supply. If electric capacity were increased six-fold, then the 72-year supply would last just 12 years.
  • OECD: The world's present measured resources of uranium, economically recoverable at a price of US$130/kg according to the industry groups OECD, NEA and IAEA, are enough to last for 100 years at current consumption.
  • According to the Australian Uranium Association, yet another industry group, assuming the world's current rate of consumption at 66,500 tonnes of uranium per year and the world's present measured resources of uranium (4.7 Mt) are enough to last for 70 years.

Optimistic predictions

All the following references claim that the supply is far more than demand. Therefore, they do not predict peak uranium.

  • In his 1956 landmark paper, M. King Hubbert wrote "There is promise, however, provided mankind can solve its international problems and not destroy itself with nuclear weapons, and provided world population (which is now expanding at such a rate as to double in less than a century) can somehow be brought under control, that we may at last have found an energy supply adequate for our needs for at least the next few centuries of the 'foreseeable future.'" Hubbert's study assumed that breeder reactors would replace light water reactors and that uranium would be bred into plutonium (and possibly thorium would be bred into uranium). He also assumed that economic means of reprocessing would be discovered. For political, economic and nuclear proliferation reasons, the plutonium economy never materialized. Without it, uranium is used up in a once-through process and will peak and run out much sooner. However, at present, it is generally found to be cheaper to mine new uranium out of the ground than to use reprocessed uranium, and therefore the use of reprocessed uranium is limited to only a few nations.
  • The OECD estimates that with the world nuclear electricity generating rates of 2002, with LWR, once-through fuel cycle, there are enough conventional resources to last 85 years using known resources and 270 years using known and as yet undiscovered resources. With breeders, this is extended to 8,500 years.

If one is willing to pay $300/kg for uranium, there is a vast quantity available in the ocean. It is worth noting that since fuel cost only amounts to a small fraction of nuclear energy total cost per kWh, and raw uranium price also constitutes a small fraction of total fuel costs, such an increase on uranium prices wouldn't involve a very significant increase in the total cost per kWh produced.

  • In 1983, physicist Bernard Cohen proposed that uranium is effectively inexhaustible, and could therefore be considered a renewable source of energy. He claims that fast breeder reactors, fueled by naturally replenished uranium extracted from seawater, could supply energy at least as long as the sun's expected remaining lifespan of five billion years. While uranium is a finite mineral resource within the earth, the hydrogen in the sun is finite too – thus, if the resource of nuclear fuel can last over such time scales, as Cohen contends, then nuclear energy is every bit as sustainable as solar power or any other source of energy, in terms of sustainability over the time scale of life surviving on this planet.

We thus conclude that all the world’s energy requirements for the remaining 5×109 yr of existence of life on Earth could be provided by breeder reactors without the cost of electricity rising by as much as 1% due to fuel costs. This is consistent with the definition of a "renewable" energy source in the sense in which that term is generally used.

His paper assumes extraction of uranium from seawater at the rate of 16 kilotonnes (35×106 lb) per year of uranium. The current demand for uranium is near 70 kilotonnes (150×106 lb) per year; however, the use of breeder reactors means that uranium would be used at least 60 times more efficiently than today.

  • James Hopf, a nuclear engineer writing for American Energy Independence in 2004, believes that there is several hundred years' supply of recoverable uranium even for standard reactors. For breeder reactors, "it is essentially infinite".

All the following references claim that the supply is far more than demand. Therefore, they believe that uranium will not deplete in the foreseeable future.

  • The IAEA estimates that using only known reserves at the current rate of demand and assuming a once-through nuclear cycle that there is enough uranium for at least 100 years. However, if all primary known reserves, secondary reserves, undiscovered and unconventional sources of uranium are used, uranium will be depleted in 47,000 years.
  • Kenneth S. Deffeyes estimates that if one can accept ore one tenth as rich then the supply of available uranium increased 300 times. His paper shows that uranium concentration in ores is log-normal distributed. There is relatively little high-grade uranium and a large supply of very low grade uranium.
  • Ernest Moniz, a professor at the Massachusetts Institute of Technology and the former United States Secretary of Energy, testified in 2009 that an abundance of uranium had put into question plans to reprocess spent nuclear fuel. The reprocessing plans dated from decades previous, when uranium was thought to be scarce. But now, "roughly speaking, we’ve got uranium coming out of our ears, for a long, long time," Professor Moniz said.

Possible effects and consequences

As uranium production declines, uranium prices would be expected to increase. However, the price of uranium makes up only 9% of the cost of running a nuclear power plant, much lower than the cost of coal in a coal-fired power plant (77%), or the cost of natural gas in a gas-fired power plant (93%).

Uranium is different from conventional energy resources, such as oil and coal, in several key aspects. Those differences limit the effects of short-term uranium shortages, but most have no bearing on the eventual depletion. Some key features are:

  • The uranium market is diverse, and no country has a monopoly influence on its prices.
  • Thanks to the extremely high energy density of uranium, stockpiling of several years' worth of fuel is feasible.
  • Significant secondary supplies of already mined uranium exist, including decommissioned nuclear weapons, depleted uranium tails suitable for reenrichment, and existing stockpiles.
  • Vast amounts of uranium, roughly 800 times the known reserves of mined uranium, are contained in extremely dilute concentrations in seawater.
  • Introduction of fast neutron reactors, combined with seawater uranium extraction, would make the uranium supply virtually inexhaustible. There are currently seven experimental fast neutron reactors running globally, in India, Japan, Russia and China.

Fast neutron reactors (breeder reactors) could utilize large amounts of Uranium-238 indirectly by conversion to Plutonium-239, rather than fissioning primarily just Uranium-235 (which is 0.7% of original mined uranium), for approximately a factor of 100 increase in uranium usage efficiency. Intermediate between conventional estimates of reserves and the 40 trillion tons total of uranium in Earth's crust (trace concentrations adding up over its 3 * 1019 ton mass), there are ores of lower grade than otherwise practical but of still higher concentration than the average rock. Accordingly, resource figures depend on economic and technological assumptions.

Uranium price

Monthly uranium spot price in US$.

The uranium spot price has increased from a low in Jan 2001 of US$6.40 per pound of U3O8 to a peak in June 2007 of US$135. The uranium prices have dropped substantially since. Currently (15 July 2013) the uranium spot is US$38.

The high price in 2007 resulted from shrinking weapons stockpiles and a flood at the Cigar Lake Mine, coupled with expected rises in demand due to more reactors coming online, leading to a uranium price bubble. Miners and Utilities are bitterly divided on uranium prices.

As prices go up, production responds from existing mines, and production from newer, harder to develop or lower quality uranium ores begins. Currently, much of the new production is coming from Kazakhstan. Production expansion is expected in Canada and in the United States. However, the number of projects waiting in the wings to be brought online now are far less than there were in the 1970s. There have been some encouraging signs that production from existing or planned mines is responding or will respond to higher prices. The supply of uranium has recently become very inelastic. As the demand increases, the prices respond dramatically.

As of 2018 the price of nuclear fuel was stable at around US$38.81 per pound, 81 cents more than in 2013 and 1 cent more than in 2017, way lower than inflation. At such a low and stable price, breeding is uneconomical.

Number of contracts

Unlike other metals such as gold, silver, copper or nickel, uranium is not widely traded on an organized commodity exchange such as the London Metal Exchange. It is traded on the NYMEX but on very low volume. Instead, it is traded in most cases through contracts negotiated directly between a buyer and a seller. The structure of uranium supply contracts varies widely. The prices are either fixed or based on references to economic indices such as GDP, inflation or currency exchange. Contracts traditionally are based on the uranium spot price and rules by which the price can escalate. Delivery quantities, schedules, and prices vary from contract to contract and often from delivery to delivery within the term of a contract.

Since the number of companies mining uranium is small, the number of available contracts is also small. Supplies are running short due to flooding of two of the world's largest mines and a dwindling amount of uranium salvaged from nuclear warheads being removed from service. While demand for the metal has been steady for years, the price of uranium is expected to surge as a host of new nuclear plants come online.

Mining

Rising uranium prices draw investments into new uranium mining projects. Mining companies are returning to abandoned uranium mines with new promises of hundreds of jobs and millions in royalties. Some locals want them back. Others say the risk is too great, and will try to stop those companies "until there's a cure for cancer."

Electric utilities

Since many utilities have extensive stockpiles and can plan many months in advance, they take a wait-and-see approach on higher uranium costs. In 2007, spot prices rose significantly due to announcements of planned reactors or new reactors coming online. Those trying to find uranium in a rising cost climate are forced to face the reality of a seller's market. Sellers remain reluctant to sell significant quantities. By waiting longer, sellers expect to get a higher price for the material they hold. Utilities on the other hand, are very eager to lock up long-term uranium contracts.

According to the NEA, the nature of nuclear generating costs allows for significant increases in the costs of uranium before the costs of generating electricity significantly increase. A 100% increase in uranium costs would only result in a 5% increase in electric cost. This is because uranium has to be converted to gas, enriched, converted back to yellow cake and fabricated into fuel elements. The cost of the finished fuel assemblies are dominated by the processing costs, not the cost of the raw materials. Furthermore, the cost of electricity from a nuclear power plant is dominated by the high capital and operating costs, not the cost of the fuel. Nevertheless, any increase in the price of uranium is eventually passed on to the consumer either directly or through a fuel surcharge. As of 2020, this has not happened and the price of nuclear fuel is low enough to make breeding uneconomical.

Substitutes

An alternative to uranium is thorium which is three times more common than uranium. Fast breeder reactors are not needed. Compared to conventional uranium reactors, thorium reactors using the thorium fuel cycle may produce some 40 times the amount of energy per unit of mass. However, creating the technology, infrastructure and know-how needed for a thorium-fuel economy is uneconomical at current and predicted uranium prices.

If nuclear power prices rise too quickly, or too high, power companies may look for substitutes in fossil energy (coal, oil, and gas) and/or renewable energy, such as hydro, bio-energy, solar thermal electricity, geothermal, wind, tidal energy. Both fossil energy and some renewable electricity sources (e.g. hydro, bioenergy, solar thermal electricity and geothermal) can be used as base-load.

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