In 1789, a book named Elementary Treatise of Chemistry was published by Antoine-Laurent de Lavoisier and was considered to be the first modern chemical textbook. The textbook contained a list of elements, or substances that could not be broken down which included oxygen, nitrogen, hydrogen, phosphorus, mercury, zinc and sulphur. His list also included light and caloric which he believed to be material substances. Due to this absurd idea, many leading chemists of that time refused to believe his revelations. Also, Lavoisier’s description only classified elements as metals and non-metals and therefore was short of a complete analysis.
Johann Dobereiner on the other hand was one of the first that attempted to classify the elements in 1817. He found that some elements formed groups of three with related properties. His findings grouped chlorine, bromine and iodine, calcium, strontium, and barium, sulphur, selenium and tellurium as well as lithium, sodium and potassium.
In 1862, a French geologist named Alexandre-Emile Chancourtois was the first person to notice the periodicity of elements. As a result of his findings, he devised an early form of a periodic table, which he called the telluric helix. His paper was published in 1862, but his use of geological rather than chemical terms caused it to receive little attention.
John Newlands, an English chemist classified the 56 elements that had been discovered at the time into eleven groups which were based on similar physical properties. He classified them in the year of 1865.
Then in 1869, a Russian chemist known as Dmitri Mendeleev became the first scientist to make a periodic table much like the one we use today. Mendeleev arranged the elements in a table ordered by atomic mass, corresponding to relative molar mass as it is defined today. During his presentation to the Russian Chemical Society, he outlined a number of rules that his periodic table abided. That enabled him to predict many other unknown elements and their properties that would be discovered later on. As a result, he reserved room for some of those yet to be discovered elements on his print of the periodic table. At the time that Mendeleev presented his periodic table, also known as “Mendeleev’s table of periodicity”, other scientists like Lothar Meyer and William Odling were also working on a periodic table.
In the years that followed, the periodic table was modified on numerous occasions to accommodate the newly discovered elements. In 1914, Henry Moseley found a relationship between an element’s X-ray wavelength and its atomic number. As a result, he resequenced the periodic table by nuclear charge rather than atomic weight. Before this discovery, atomic numbers were just sequential numbers based on an element’s atomic weight. In 1943, Glenn Seaborg who worked on the Manhattan Project research experienced unexpected difficulty in isolating two elements. This made him wonder whether these elements belonged to a different group. Finally, in 1945 he went against the advice of his colleagues and proposed a significant change to the periodic table that was implemented soon after.
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