The periodic table is an arrangement of the chemical elements, which are organized on the basis of their atomic numbers, electron configurations and recurring chemical properties.
Elements are presented in order of increasing atomic number. The
standard form of the table consists of a grid with rows called periods and columns called groups.
The history of the periodic table reflects over two centuries of growth in the understanding of chemical properties, with major contributions made by Antoine-Laurent de Lavoisier, Johann Wolfgang Döbereiner, John Newlands, Julius Lothar Meyer, Dmitri Mendeleev, and Glenn T. Seaborg.
Antiquity to the 18th century
A number of physical elements (such as platinum, mercury, tin and zinc) have been known from antiquity, as they are found in their native form and are relatively simple to mine with primitive tools. Around 330 BCE, the Greek philosopher Aristotle proposed that everything is made up of a mixture of one or more roots, an idea that had originally been suggested by the Sicilian philosopher Empedocles. The four roots, which were later renamed as elements by Plato, were earth, water, air and fire. Similar ideas about these four elements also existed in other ancient traditions, such as Indian philosophy.
Hennig Brand
The history of the periodic table is also a history of the discovery of the chemical elements. The first person in history to discover a new element was Hennig Brand, a bankrupt German merchant. Brand tried to discover the Philosopher's Stone — a mythical object that was supposed to turn inexpensive base metals into gold. In 1669 (or later), his experiments with distilled human urine resulted in the production of a glowing white substance, which he called "cold fire" (kaltes Feuer). He kept his discovery secret until 1680, when Robert Boyle
rediscovered phosphorus and published his findings. The discovery of
phosphorus helped to raise the question of what it meant for a substance
to be an element.
In 1661, Boyle defined an element as "those primitive and simple
Bodies of which the mixt ones are said to be composed, and into which
they are ultimately resolved."
Antoine-Laurent de Lavoisier
Lavoisier's Traité Élémentaire de Chimie (Elementary Treatise of Chemistry), which was written in 1789 and first translated into English by the writer Robert Kerr, is considered to be the first modern textbook about chemistry. Lavoisier defined an element as a substance that cannot be broken down into a simpler substance by a chemical reaction. This simple definition served for a century and lasted until the discovery of subatomic particles.
Lavoisier's book contained a list of "simple substances" that Lavoisier
believed could not be broken down further, which included oxygen, nitrogen, hydrogen, phosphorus, mercury, zinc and sulfur, which formed the basis for the modern list of elements. Lavoisier's list also included 'light' and 'caloric',
which at the time were believed to be material substances. He
classified these substances into metals and non metals. While many
leading chemists refused to believe Lavoisier's new revelations, the Elementary Treatise
was written well enough to convince the younger generation. However,
Lavoisier's descriptions of his elements lack completeness, as he only
classified them as metals and non-metals.
19th century
William Prout
In 1815, the English physician and chemist William Prout noticed that atomic weights seemed to be multiples of that of hydrogen.
Johann Wolfgang Döbereiner
In 1817, Johann Wolfgang Döbereiner, a chemist, began to formulate one of the earliest attempts to classify the elements.
In 1829, he found that he could form some of the elements into groups
of three, with the members of each group having related properties. He
termed these groups triads.
Definition of Triad law:-"Chemically analogous elements arranged
in increasing order of their atomic weights formed well marked groups of
three called Triads in which the atomic weight of the middle element
was found to be generally the arithmetic mean of the atomic weight of
the other two elements in the triad.
- chlorine, bromine, and iodine
- calcium, strontium, and barium
- sulfur, selenium, and tellurium
- lithium, sodium, and potassium
Alexandre-Emile Béguyer de Chancourtois
Alexandre-Emile Béguyer de Chancourtois, a French geologist,
was the first person to notice the periodicity of the elements —
similar elements occurring at regular intervals when they are ordered by
their atomic weights. In 1862 he devised an early form of periodic
table, which he named Vis tellurique (the 'telluric helix'), after the element tellurium, which fell near the center of his diagram.
With the elements arranged in a spiral on a cylinder by order of
increasing atomic weight, de Chancourtois saw that elements with similar
properties lined up vertically. His 1863 publication included a chart
(which contained ions and compounds, in addition to elements), but his original paper in the Comptes Rendus de l'Académie des Sciences
used geological rather than chemical terms and did not include a
diagram. As a result, de Chancourtois' ideas received little attention
until after the work of Dmitri Mendeleev had been published.
John Newlands
In 1864, the English chemist John Newlands classified the sixty-two known elements into eight groups, based on their physical properties.
Newlands noted that many pairs of similar elements existed, which
differed by some multiple of eight in mass number, and was the first to
assign them an atomic number. When his 'law of octaves' was printed in Chemistry News,
likening this periodicity of eights to the musical scale, it was
ridiculed by some of his contemporaries. His lecture to the Chemistry
Society on 1 March 1866 was not published, the Society defending their
decision by saying that such 'theoretical' topics might be
controversial.
The importance of Newlands' analysis was eventually recognised by
the Chemistry Society with a Gold Medal five years after they
recognised Mendeleev's work. It was not until the following century,
with Gilbert N. Lewis's valence bond theory (1916) and Irving Langmuir's octet theory of chemical bonding (1919), that the importance of the periodicity of eight would be accepted. The Royal Chemistry Society acknowledged Newlands' contribution to science in 2008, when they put a Blue Plaque on the house where he was born, which described him as the "discoverer of the Periodic Law for the chemical elements".
He contributed the word 'periodic' in chemistry.
Julius Lothar Meyer
Meyer noted, as J. A. R. Newlands did in England, if each element is
arranged in the order of their atomic weights, they fall into groups of
similar chemical and physical properties repeated at periodic intervals.
According to him, if the atomic weights were plotted as ordinates and
the atomic volumes as abscissae—the curve obtained a series of maxima
and minima—the most electro-positive elements appearing at the peaks of
the curve in the order of their atomic weights.
His book, Die modernen Theorien der Chemie,
which he began writing in Breslau in 1862 and which was published two
years later, contained an early version of the periodic table containing
28 elements, classified elements into six families by their valence—for
the first time, elements had been grouped according to their valence.
Works on organizing the elements by atomic weight, until then had been
stymied by inaccurate measurements of the atomic weights.
He published articles about classification table of the elements
in horizontal form (1862, 1864) and vertical form (1870), in which the
series of periods are properly ended by an element of the alkaline earth
metal group.
In 1869, a few months later than Mendeleev, Meyer published a
revised and expanded version of his 1864 table independently, which was
similar to that published by Mendeleev (Meyer had been sent a copy of
Mendeleev's table earlier; Mendeleev had sent it to many well-known
chemists of his day) and a paper showing graphically the periodicity of the elements as a function of atomic weight.
In 1882, both Meyer and Mendeleev received the Davy Medal from
the Royal Society in recognition of their work on the Periodic Law.
Dmitri Mendeleev
The Russian chemist Dmitri Mendeleev arranged the elements by atomic mass, corresponding to relative molar mass.
It is sometimes said that he played 'chemical solitaire' on long train
journeys, using cards with various facts about the known elements. On March 1 [O.S. February 17] 1869, he put a date on his first table, and sent it for publication. On 18 March [O.S. 6 March] 1869, Mendeleev gave a formal presentation, The Dependence Between the Properties of the Atomic Weights of the Elements, to the Russian Chemical Society. In 1869, the table was published in an obscure Russian journal and then republished in a German journal, Zeitschrift für Chemie. In it, Mendeleev stated that:
- The elements, if arranged according to their atomic mass, exhibit an apparent periodicity of properties.
- Elements which are similar as regards to their chemical properties have atomic weights which are either of nearly the same value (e.g., Pt, Ir, Os) or which increase regularly (e.g., K, Rb, Cs).
- The arrangement of the elements, or of groups of elements in the order of their atomic masses, corresponds to their so-called valencies, as well as, to some extent, to their distinctive chemical properties; as is apparent among other series in that of Li, Be, B, C, N, O, and F.
- The elements which are the most widely diffused have small atomic weights.
- The magnitude of the atomic weight determines the character of the element, just as the magnitude of the molecule determines the character of a compound body.
- We must expect the discovery of many yet unknown elements – for example, elements analogous to aluminium and silicon – whose atomic weight would be between 65 and 75.
- The atomic weight of an element may sometimes be amended by a knowledge of those of its contiguous elements. Thus the atomic weight of tellurium must lie between 123 and 126, and cannot be 128.
- Certain characteristic properties of elements can be foretold from their atomic masses.
Scientific benefits of Mendeleev's table
- It enabled Mendeleev to predict the discovery of new elements and left spaces for them, namely eka-silicon (germanium, discovered in 1885), eka-aluminium (gallium, 1875), and eka-boron (scandium, 1879). Thus, there was no disturbance in the periodic table.
- It could be used by Mendeleev to point out that some of the atomic weights being used at the time were incorrect.
- It provided for variance from atomic weight order.
William Odling
In 1864, the English chemist William Odling also drew up a table that was remarkably similar to the table produced by Mendeleev.
Odling overcame the tellurium-iodine problem and even managed to get
thallium, lead, mercury and platinum into the right groups, which is
something that Mendeleev failed to do at his first attempt.
Odling failed to achieve recognition, however, since it is suspected
that he, as Secretary of the Chemical Society of London, was
instrumental in discrediting Newlands' earlier work on the periodic
table.
Shortcomings of early versions of the periodic table
- The table was not able to predict the existence of the noble gases, but did leave spaces for yet-to-be discovered elements. Time proved this method correct. When the entire group of noble gases was discovered, primarily by William Ramsay, he added them to the table as Group 0, without disturbing the basic concept of the periodic table.
- A single position could not be assigned to hydrogen, which could be placed either in the alkali metals group, the halogens group or separately above the table between boron and carbon.
- The lanthanides were difficult to fit into the table.
20th century
Frederick Soddy
By 1912 almost 50 different radioactive elements had been found, too many for the periodic table. Frederick Soddy
in 1913 found that although they emitted different radiation, many
elements were alike in their chemical characteristics so shared the same
place on the table. They became known as isotopes, from the Greek eisos topos ("same place").
Henry Moseley
In 1914, a year before he was killed in action at Gallipoli, the English physicist Henry Moseley found a relationship between the X-ray wavelength of an element and its atomic number. He was then able to re-sequence the periodic table by nuclear charge,
rather than by atomic weight. Before this discovery, atomic numbers
were sequential numbers based on an element's atomic weight. Moseley's
discovery showed that atomic numbers were in fact based upon
experimental measurements.
Using information about their X-ray wavelengths, Moseley placed argon (with an atomic number Z=18) before potassium
(Z=19), despite the fact that argon's atomic weight of 39.9 is greater
than the atomic weight of potassium (39.1). The new order was in
agreement with the chemical properties of these elements, since argon is
a noble gas and potassium is an alkali metal. Similarly, Moseley placed cobalt before nickel and was able to explain that tellurium occurs before iodine, without revising the experimental atomic weight of tellurium, as had been proposed by Mendeleev.
Moseley's research showed that there were gaps in the periodic
table at atomic numbers 43 and 61, which are now known to be occupied by
technetium and promethium respectively.
Glenn T. Seaborg
During his Manhattan Project research in 1943, Glenn T. Seaborg experienced unexpected difficulties in isolating the elements americium and curium. These elements, in addition to the elements from actinium to plutonium,
were believed to form a fourth series of transition metals. Seaborg
wondered if these elements belonged to a different series, which would
explain why their chemical properties, in particular the instability of
higher oxidation states, were different from predictions. In 1945, against the advice of colleagues, he proposed a significant change to Mendeleev's table: the actinide series.
Seaborg's actinide concept of heavy element electronic structure, predicting that the actinides form a transition series analogous to the rare earth series of lanthanide
elements, is now well accepted and included in the periodic table. The
actinide series is the second row of the f-block (5f series). In both
the actinide and lanthanide series, an inner electron shell is being filled. The actinide series comprises the elements from actinium to lawrencium. Seaborg's subsequent elaborations of the actinide concept theorized a series of superheavy elements in a transactinide series comprising elements from 104 to 121 and a superactinide series of elements from 122 to 153.