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Tuesday, November 1, 2022

Baryon

From Wikipedia, the free encyclopedia

In particle physics, a baryon is a type of composite subatomic particle which contains an odd number of valence quarks (at least 3). Baryons belong to the hadron family of particles; hadrons are composed of quarks. Baryons are also classified as fermions because they have half-integer spin.

The name "baryon", introduced by Abraham Pais, comes from the Greek word for "heavy" (βαρύς, barýs), because, at the time of their naming, most known elementary particles had lower masses than the baryons. Each baryon has a corresponding antiparticle (antibaryon) where their corresponding antiquarks replace quarks. For example, a proton is made of two up quarks and one down quark; and its corresponding antiparticle, the antiproton, is made of two up antiquarks and one down antiquark.

Because they are composed of quarks, baryons participate in the strong interaction, which is mediated by particles known as gluons. The most familiar baryons are protons and neutrons, both of which contain three quarks, and for this reason they are sometimes called triquarks. These particles make up most of the mass of the visible matter in the universe and compose the nucleus of every atom. (Electrons, the other major component of the atom, are members of a different family of particles called leptons; leptons do not interact via the strong force.) Exotic baryons containing five quarks, called pentaquarks, have also been discovered and studied.

A census of the Universe's baryons indicates that 10% of them could be found inside galaxies, 50 to 60% in the circumgalactic medium, and the remaining 30 to 40% could be located in the warm–hot intergalactic medium (WHIM).

Background

Baryons are strongly interacting fermions; that is, they are acted on by the strong nuclear force and are described by Fermi–Dirac statistics, which apply to all particles obeying the Pauli exclusion principle. This is in contrast to the bosons, which do not obey the exclusion principle.

Baryons, along with mesons, are hadrons, particles composed of quarks. Quarks have baryon numbers of B = 1/3 and antiquarks have baryon numbers of B = −1/3. The term "baryon" usually refers to triquarks—baryons made of three quarks (B = 1/3 + 1/3 + 1/3 = 1).

Other exotic baryons have been proposed, such as pentaquarks—baryons made of four quarks and one antiquark (B = 1/3 + 1/3 + 1/3 + 1/3 − 1/3 = 1), but their existence is not generally accepted. The particle physics community as a whole did not view their existence as likely in 2006, and in 2008, considered evidence to be overwhelmingly against the existence of the reported pentaquarks. However, in July 2015, the LHCb experiment observed two resonances consistent with pentaquark states in the Λ0
b
→ J/ψK
p decay, with a combined statistical significance of 15σ.

In theory, heptaquarks (5 quarks, 2 antiquarks), nonaquarks (6 quarks, 3 antiquarks), etc. could also exist.

Baryonic matter

Nearly all matter that may be encountered or experienced in everyday life is baryonic matter, which includes atoms of any sort, and provides them with the property of mass. Non-baryonic matter, as implied by the name, is any sort of matter that is not composed primarily of baryons. This might include neutrinos and free electrons, dark matter, supersymmetric particles, axions, and black holes.

The very existence of baryons is also a significant issue in cosmology because it is assumed that the Big Bang produced a state with equal amounts of baryons and antibaryons. The process by which baryons came to outnumber their antiparticles is called baryogenesis.

Baryogenesis

Experiments are consistent with the number of quarks in the universe being a constant and, to be more specific, the number of baryons being a constant (if antimatter is counted as negative); in technical language, the total baryon number appears to be conserved. Within the prevailing Standard Model of particle physics, the number of baryons may change in multiples of three due to the action of sphalerons, although this is rare and has not been observed under experiment. Some grand unified theories of particle physics also predict that a single proton can decay, changing the baryon number by one; however, this has not yet been observed under experiment. The excess of baryons over antibaryons in the present universe is thought to be due to non-conservation of baryon number in the very early universe, though this is not well understood.

Properties

Isospin and charge

Combinations of three u, d or s quarks forming baryons with a spin-3/2 form the uds baryon decuplet
 
Combinations of three u, d or s quarks forming baryons with a spin-1/2 form the uds baryon octet

The concept of isospin was first proposed by Werner Heisenberg in 1932 to explain the similarities between protons and neutrons under the strong interaction. Although they had different electric charges, their masses were so similar that physicists believed they were the same particle. The different electric charges were explained as being the result of some unknown excitation similar to spin. This unknown excitation was later dubbed isospin by Eugene Wigner in 1937.

This belief lasted until Murray Gell-Mann proposed the quark model in 1964 (containing originally only the u, d, and s quarks). The success of the isospin model is now understood to be the result of the similar masses of u and d quarks. Since u and d quarks have similar masses, particles made of the same number then also have similar masses. The exact specific u and d quark composition determines the charge, as u quarks carry charge +2/3 while d quarks carry charge −1/3. For example, the four Deltas all have different charges (
Δ++
(uuu),
Δ+
(uud),
Δ0
(udd),
Δ
(ddd)), but have similar masses (~1,232 MeV/c2) as they are each made of a combination of three u or d quarks. Under the isospin model, they were considered to be a single particle in different charged states.

The mathematics of isospin was modeled after that of spin. Isospin projections varied in increments of 1 just like those of spin, and to each projection was associated a "charged state". Since the "Delta particle" had four "charged states", it was said to be of isospin I = 3/2. Its "charged states"
Δ++
,
Δ+
,
Δ0
, and
Δ
, corresponded to the isospin projections I3 = +3/2, I3 = +1/2, I3 = −1/2, and I3 = −3/2, respectively. Another example is the "nucleon particle". As there were two nucleon "charged states", it was said to be of isospin 1/2. The positive nucleon
N+
(proton) was identified with I3 = +1/2 and the neutral nucleon
N0
(neutron) with I3 = −1/2. It was later noted that the isospin projections were related to the up and down quark content of particles by the relation:

where the n's are the number of up and down quarks and antiquarks.

In the "isospin picture", the four Deltas and the two nucleons were thought to be the different states of two particles. However, in the quark model, Deltas are different states of nucleons (the N++ or N are forbidden by Pauli's exclusion principle). Isospin, although conveying an inaccurate picture of things, is still used to classify baryons, leading to unnatural and often confusing nomenclature.

Flavour quantum numbers

The strangeness flavour quantum number S (not to be confused with spin) was noticed to go up and down along with particle mass. The higher the mass, the lower the strangeness (the more s quarks). Particles could be described with isospin projections (related to charge) and strangeness (mass) (see the uds octet and decuplet figures on the right). As other quarks were discovered, new quantum numbers were made to have similar description of udc and udb octets and decuplets. Since only the u and d mass are similar, this description of particle mass and charge in terms of isospin and flavour quantum numbers works well only for octet and decuplet made of one u, one d, and one other quark, and breaks down for the other octets and decuplets (for example, ucb octet and decuplet). If the quarks all had the same mass, their behaviour would be called symmetric, as they would all behave in the same way to the strong interaction. Since quarks do not have the same mass, they do not interact in the same way (exactly like an electron placed in an electric field will accelerate more than a proton placed in the same field because of its lighter mass), and the symmetry is said to be broken.

It was noted that charge (Q) was related to the isospin projection (I3), the baryon number (B) and flavour quantum numbers (S, C, B′, T) by the Gell-Mann–Nishijima formula:

where S, C, B′, and T represent the strangeness, charm, bottomness and topness flavour quantum numbers, respectively. They are related to the number of strange, charm, bottom, and top quarks and antiquark according to the relations:

meaning that the Gell-Mann–Nishijima formula is equivalent to the expression of charge in terms of quark content:

Spin, orbital angular momentum, and total angular momentum

Spin (quantum number S) is a vector quantity that represents the "intrinsic" angular momentum of a particle. It comes in increments of 1/2 ħ (pronounced "h-bar"). The ħ is often dropped because it is the "fundamental" unit of spin, and it is implied that "spin 1" means "spin 1 ħ". In some systems of natural units, ħ is chosen to be 1, and therefore does not appear anywhere.

Quarks are fermionic particles of spin 1/2 (S = 1/2). Because spin projections vary in increments of 1 (that is 1 ħ), a single quark has a spin vector of length 1/2, and has two spin projections (Sz = +1/2 and Sz = −1/2). Two quarks can have their spins aligned, in which case the two spin vectors add to make a vector of length S = 1 and three spin projections (Sz = +1, Sz = 0, and Sz = −1). If two quarks have unaligned spins, the spin vectors add up to make a vector of length S = 0 and has only one spin projection (Sz = 0), etc. Since baryons are made of three quarks, their spin vectors can add to make a vector of length S = 3/2, which has four spin projections (Sz = +3/2, Sz = +1/2, Sz = −1/2, and Sz = −3/2), or a vector of length S = 1/2 with two spin projections (Sz = +1/2, and Sz = −1/2).

There is another quantity of angular momentum, called the orbital angular momentum (azimuthal quantum number L), that comes in increments of 1 ħ, which represent the angular moment due to quarks orbiting around each other. The total angular momentum (total angular momentum quantum number J) of a particle is therefore the combination of intrinsic angular momentum (spin) and orbital angular momentum. It can take any value from J = |LS| to J = |L + S|, in increments of 1.

Baryon angular momentum quantum numbers for L = 0, 1, 2, 3
Spin,
S
Orbital angular
momentum, L
Total angular
momentum, J
Parity,
P
Condensed
notation, JP
1/2 0 1/2 + 1/2+
1 3/2, 1/2 3/2, 1/2
2 5/2, 3/2 + 5/2+, 3/2+
3 7/2, 5/2 7/2, 5/2
3/2 0 3/2 + 3/2+
1 5/2, 3/2, 1/2 5/2, 3/2, 1/2
2 7/2, 5/2, 3/2, 1/2 + 7/2+, 5/2+, 3/2+, 1/2+
3 9/2, 7/2, 5/2, 3/2 9/2, 7/2, 5/2, 3/2

Particle physicists are most interested in baryons with no orbital angular momentum (L = 0), as they correspond to ground states—states of minimal energy. Therefore, the two groups of baryons most studied are the S = 1/2; L = 0 and S = 3/2; L = 0, which corresponds to J = 1/2+ and J = 3/2+, respectively, although they are not the only ones. It is also possible to obtain J = 3/2+ particles from S = 1/2 and L = 2, as well as S = 3/2 and L = 2. This phenomenon of having multiple particles in the same total angular momentum configuration is called degeneracy. How to distinguish between these degenerate baryons is an active area of research in baryon spectroscopy.

Parity

If the universe were reflected in a mirror, most of the laws of physics would be identical—things would behave the same way regardless of what we call "left" and what we call "right". This concept of mirror reflection is called "intrinsic parity" or simply "parity" (P). Gravity, the electromagnetic force, and the strong interaction all behave in the same way regardless of whether or not the universe is reflected in a mirror, and thus are said to conserve parity (P-symmetry). However, the weak interaction does distinguish "left" from "right", a phenomenon called parity violation (P-violation).

Based on this, if the wavefunction for each particle (in more precise terms, the quantum field for each particle type) were simultaneously mirror-reversed, then the new set of wavefunctions would perfectly satisfy the laws of physics (apart from the weak interaction). It turns out that this is not quite true: for the equations to be satisfied, the wavefunctions of certain types of particles have to be multiplied by −1, in addition to being mirror-reversed. Such particle types are said to have negative or odd parity (P = −1, or alternatively P = –), while the other particles are said to have positive or even parity (P = +1, or alternatively P = +).

For baryons, the parity is related to the orbital angular momentum by the relation:

As a consequence, baryons with no orbital angular momentum (L = 0) all have even parity (P = +).

Nomenclature

Baryons are classified into groups according to their isospin (I) values and quark (q) content. There are six groups of baryons: nucleon (
N
), Delta (
Δ
), Lambda (
Λ
), Sigma (
Σ
), Xi (
Ξ
), and Omega (
Ω
). The rules for classification are defined by the Particle Data Group. These rules consider the up (
u
), down (
d
) and strange (
s
) quarks to be light and the charm (
c
), bottom (
b
), and top (
t
) quarks to be heavy. The rules cover all the particles that can be made from three of each of the six quarks, even though baryons made of top quarks are not expected to exist because of the top quark's short lifetime. The rules do not cover pentaquarks.

  • Baryons with (any combination of) three
    u
    and/or
    d
    quarks are
    N
    s (I = 1/2) or
    Δ
    baryons (I = 3/2).
  • Baryons containing two
    u
    and/or
    d
    quarks are
    Λ
    baryons (I = 0) or
    Σ
    baryons (I = 1). If the third quark is heavy, its identity is given by a subscript.
  • Baryons containing one
    u
    or
    d
    quark are
    Ξ
    baryons (I = 1/2). One or two subscripts are used if one or both of the remaining quarks are heavy.
  • Baryons containing no
    u
    or
    d
    quarks are
    Ω
    baryons (I = 0), and subscripts indicate any heavy quark content.
  • Baryons that decay strongly have their masses as part of their names. For example, Σ0 does not decay strongly, but Δ++(1232) does.

It is also a widespread (but not universal) practice to follow some additional rules when distinguishing between some states that would otherwise have the same symbol.

  • Baryons in total angular momentum J = 3/2 configuration that have the same symbols as their J = 1/2 counterparts are denoted by an asterisk ( * ).
  • Two baryons can be made of three different quarks in J = 1/2 configuration. In this case, a prime ( ′ ) is used to distinguish between them.
    • Exception: When two of the three quarks are one up and one down quark, one baryon is dubbed Λ while the other is dubbed Σ.

Quarks carry a charge, so knowing the charge of a particle indirectly gives the quark content. For example, the rules above say that a
Λ+
c
contains a c quark and some combination of two u and/or d quarks. The c quark has a charge of (Q = +2/3), therefore the other two must be a u quark (Q = +2/3), and a d quark (Q = −1/3) to have the correct total charge (Q = +1).

History of coal mining in the United States

Total US coal production, 1870–2018
 
US Annual coal production by coal rank.
 
Trends in surface versus underground mining of coal in the US
 
Bowman Company coal mine, Indiana County, Pennsylvania, 1904.

The history of coal mining in the United States goes back to the 1300s, when the Hopi Indians used coal. The first commercial use came in 1701, within the Manakin-Sabot area of Richmond, Virginia. Coal was the dominant power source in the United States in the late 1800s and early 1900s, and although in rapid decline it remains a significant source of energy in 2019.

Coal became the largest source of energy in the 1880s, when it overtook wood, and remained the largest source until the early 1950s, when coal was exceeded by petroleum. Coal provided more than half of the nation's energy from the 1880s to the 1940s, and from 1906 to 1920 provided more than three-quarters of US energy.

19th century

At the start of the 19th century, coal mining was almost all bituminous coal. In 1810, 176,000 short tons of bituminous coal, and 2,000 tons of anthracite coal, were mined in the United States. American coal mining grew rapidly in the early 1820s, doubling or tripling every decade. Anthracite mining overtook bituminous coal mining in the 1840s; from 1843 through 1868, more anthracite was mined than bituminous coal. But the more limited deposits of anthracite could not satisfy the increasing demand for coal; from 1869, bituminous coal was the dominant grade of coal mined. Another reason for the decline in anthracite was the decline in its use in iron smelting, where it was displaced by coke in blast furnaces after the Civil War. Coke stayed hard and porous and was able to support the heavy column of ore and fuel in the large blast furnaces it enabled.

Anthracite (or "hard" coal) exploitation began before the War of 1812 spurred by the interest and opportunism of the Wurt brothers of Philadelphia. Burning clean and smokeless, anthracite became the preferred fuel in cities, replacing wood by about 1850, the same pattern seen in Europe. The East became deforested, driving up price of fuel wood. Anthracite from the Northeastern Pennsylvania Coal Region and later from West Virginia was valued for household use because it burns cleanly with little ash. It was also used in the early foundries of Philadelphia, New York, Newark and Allentown. The rich Pennsylvania anthracite fields were close to the big eastern cities, and nearly every major railroad in the Eastern United States such as the Reading Railroad, Lehigh & Erie, Central Railroad of New Jersey, Pennsylvania Railroad and Delaware and Hudson Railroad, extended lines into the anthracite fields. Many railroads began as mining company shortline railroads. By 1840, annual hard coal output had passed the million-short ton mark, and then quadrupled by 1850, and as it grew it pushed railroad construction, mining and steel production in a synergistic symbiosis.

In the mid-century Pittsburgh was the principal market. After 1850, soft coal, which is cheaper but dirtier, came into demand for railway locomotives and stationary steam engines, and was used to make coke for steel after 1870.

20th century

Total coal output soared until 1918; before 1890, it doubled every ten years, going from 8.4 million short tons in 1850 to 40 million in 1870, 270 million in 1900, and peaking at 680 million short tons in 1918. New soft coal fields opened in Ohio, Indiana and Illinois, as well as West Virginia, Kentucky and Alabama. The Great Depression of the 1930s lowered the demand to 360 million short tons in 1932.

Mining history by state

Breaker boys, Woodward Coal Mines, Kingston, Pennsylvania., ca. 1900
Breaker boys, Woodward Coal Mines, Kingston, Pennsylvania., ca. 1900

Pennsylvania

  • The first anthracite coal was mined in 1768 by Obadiah Gore, a blacksmith, in the Wyoming Valley (Kingston, PA). This was in the very early days of colonists settling in Northeastern Pennsylvania from Connecticut. The Susquehanna Company was an expedition that came into the Wyoming Valley and established the first 5 towns: Pittston, Plymouth, Wilkes-Barre, Nanticoke (later Hanover), and Forty Fort (later Kingston).
  • Nicholas Scull, a famous colonial surveyor issued a map in Philadelphia in 1770 that showed the location of 5 coal mines all in Schuylkill County: York Farm (Pottsville), near Silverton Junction, near Llewellyn, and 2 more around Ashland.
  • By 1807, fifty tons of coal was being sold by the Smith Brothers out of Plymouth, Pennsylvania. They exported it via barge on the Susquehanna River to Columbia, PA (Lancaster County).
  • In February 1808, Wilkes-Barre resident, Jesse Fell, experimented with a successful open-air grate that kept anthracite burning in low-yield household fires. The Smiths seized on Fell's discovery and returned to Columbia with more coal and instructions for local blacksmiths on preparing the grates.
  • Bituminous coal was first mined in Pennsylvania at "Coal Hill" (Mount Washington), just across the Monongahela River from the city of Pittsburgh. The coal was extracted from drift mines in the Pittsburgh coal seam, which outcrops along the hillside and transported by canoe to the nearby military garrison. By 1830, the city of Pittsburgh consumed more than 400 tons per day of bituminous coal for domestic and light industrial use.

The Lackawanna Valley in Pennsylvania was rich in anthracite coal and iron deposits. Brothers George W. Scranton and Seldon T. Scranton moved to the valley in 1840 and settled in the five-house town of Slocum's Hollow (now Scranton) to establish an iron forge. The Scrantons succeeded by using a technological innovation in iron smelting, the "hot blast", developed in Scotland in 1828. The Scrantons also used anthracite coal to make steel, rather than existing methods which used charcoal or bituminous coal.

Photo of coal miners in West Virginia, 1908

West Virginia

In 1883, thousands of European immigrants and a large number of African Americans migrated to southern West Virginia to work in coal mines. These coal miners worked in company mines with company tools and equipment, which they were required to lease. Along with these expenses, the miners were deducted pay for housing rent and items they purchased from company stores. Many coal companies paid miners with company scrip (private money), good only at company-owned stores.

In addition to the poor economic condition, safety in the mines was a great concern. West Virginia fell behind other states in regulating mining conditions, and between 1890 and 1912, had a higher mine death rate than any other state. West Virginia was the site of the worst coal mining disaster to date, the Monongah Mining disaster of Monongah, West Virginia in 1907. The disaster was caused by the ignition of methane gas (also called "firedamp"), which in turn ignited the coal dust, killing 362 men. The disaster impelled the United States Congress to create the Bureau of Mines.

Kentucky

Diana Baldwin and Anita Cherry are believed to have been the first women to work inside an American coal mine, and were the first women to work inside a mine who were members of the United Mine Workers of America. They began that work in 1973 in Jenkins, Kentucky.

This section needs expansion, with information about coal mining in eastern Kentucky.

Employment

Coal mining employment in the US, 1950-2017

Coal-mining employment increased rapidly in the late 1800s and early 1900s, and peaked in 1923 at 798,000. Since then, the number of miners has fallen considerably since, due to mechanization. By 2019 it had fallen below 55,000.

Accidents

Coal mining fatalities in the United States 1900-2014 (data from US Dept. of Labor)

The rate of coal-mining fatalities has been declining since the early 1900s, both in the raw number of fatalities, and in the fatality rate per miner.

United Mine Workers union

Coal Producing States, 1889
State Coal Production
(thousands of short tons)
Pennsylvania 81,719
Illinois 12,104
Ohio 9,977
West Virginia 6,232
Iowa 4,095
Alabama 3,573
Indiana 2,845
Colorado 2,544
Kentucky 2,400
Kansas 2,221
Tennessee 1,926

Since it was founded in 1890, the United Mine Workers (UMW) labor union has played a key role in United States coal mining.

Some notable labor strikes and events include:

Under John L. Lewis, the United Mine Workers became the dominant force in the coal fields in the 1930s and 1940s, producing high wages and benefits.

Mechanization

Surface coal mining in Wyoming

Irish mining engineer Richard Sutcliffe invented the first conveyor belt for use in the coal mines of Yorkshire in the early 1900s. Within the first forty years of the 20th century, more than sixty percent of US coal was loaded mechanically rather than by man power. The history of the industry is the history of increasing mechanization. As mechanization continued, fewer miners were needed, and some miners reacted with violence. One of the first machines to arrive at West Virginia's Kanawha field had to be escorted by armed guards. The same machine introduced at a mine in Illinois was operated at a slow speed because the superintendent feared labor troubles.

Despite resistance, mechanization replaced more and more laborers. By 1940, over 2/3 of coal loaded in the large West Virginia fields was done by machine. With the increase of mechanization came much higher wages for those still employed, but hard times for the former miners because there were very few other jobs in or near the camps. Most moved to the cities to find work, or back to the hills where they started.

US Coal production from 1949 to 2007(US Energy Information Administration)

In 1914 at the peak there were 180,000 anthracite miners; by 1970 only 6,000 remained. At the same time steam engines were phased out in railways and factories, and bituminous coal was used primarily for the generation of electricity. Employment in bituminous peaked at 705,000 men in 1923, falling to 140,000 by 1970 and 70,000 in 2003.

During World War II, the Solid Fuels Administration for War operated government-seized coal mines, either directly or through cooperation with successive Coal Mines Administrations.

In the 1960s a series of mergers saw coal production shift from small, independent coal companies to large, more diversified firms. Several oil companies and electricity producers acquired coal companies or leased Federal coal reserves in the west of the United States. Concerns that competition in the coal industry could decline as a result of these changes were heightened by a sharp rise in coal prices in the wake of the 1973 oil crisis. Coal prices fell in the 1980s, partly in response to oil price decline, but primarily in response to the large increase in supply worldwide which was brought about by the earlier price surge. During this period, the industry in the U.S. moved to low-sulfur coal.

In 1987 Wyoming became the largest coal producing state. As of 2014, all but one out of the 18 coal mines in Wyoming were strip mines. Wyoming's coal reserves total about 69.3 billion tons, or 14.2% of the U.S. coal reserve.

Coal is used primarily to generate electricity, but the rapid drop in natural gas prices after 2010 created severe competition.

Education

From Wikipedia, the free encyclopedia https://en.wikipedia.org/wiki/Education Education is the transmissio...