The modern periodic table is a table showing known
elements, their symbols, atomic numbers and relative atomic masses. The position of an
element in the table shows whether it is a metal, non metal, or metalloid. It also
indicates what properties it possesses. The table got its name from the frequent, or
periodic, repeating of the properties of similar elements.
Today the table is taken for granted, but how did
scientists first work it out? Throughout the 19th century, many scientist tried to create
charts listing elements in order of the size of their atoms. The idea was to
try to find and show a relationship between the size of an atom and its properties, and to
show a pattern of similarities between elements of a similar size.
The size of an atom really means its mass. It is possible
to calculate the mass of an atom in relation to other atoms, using the mass of Carbon-12
as a base. This is called relative atomic mass. (Relative atomic mass is sometimes
referred to as RAM.) The relative atomic mass, number of an element is the average of the
masses of its isotopes. One way to imagine this is as an average mass of a sample of atoms
in a particular element. The RAM of one particular element is always the same.

Early attempts - History
An early attempt to find a pattern in the properties of
elements was made by the German chemist Johann Wolfgang Döbereiner (1780-1849).
He noticed that some elements could be arranged in groups
of three. An element in a particular group had similar properties to the other two
elements in that group. As there were three elements to a group, Döbereiner gave them the
name of triads (which means groups of three). He also discovered
that if he put the elements of a triad in order of RAM, the RAM of the element in the
middle was very close to the average RAM of the other two elements. Later, the English
scientist John Newlands (1837-1898) arranged elements in groups of eight, but 'Newland's
octaves', as they were called, were largely ignored by scientists.
Dmitri Mendeleev
The modern periodic table owes its existence to the Russian scientist Dmitri
Mendeleev (1834-1907). He collected all the information he had about each element on
separate cards. He then sorted the cards into order of increasing atomic mass, and laid
them out in a horizontal row. When he came to an element with properties similar to one he
had already laid down, he started a new row, directly beneath the last. This meant that
elements in the same vertical column had similar properties to each other.
Mendeleev, found that there was a repetition of
properties every eight or eighteen elements. When this didn't occur, he realised that
there were probably some undiscovered elements. He solved this by leaving gaps, and by
predicting what the properties of these missing elements would be. He was also confident
enough to swap around a few elements when their mass did not match the patterns he had
discovered. Mendeleev published the table in 1869.
Scientists later discovered several new elements as a
direct result of trying to fill in the gaps that he had left. The properties of these
elements were startlingly similar to those Mendeleev had predicted. His table was accepted
as a very important guide to the properties of elements.
The modern periodic table
The major fault in Mendeleevs table was that he
believed that it was the mass of the elements that affected their properties. It is, in
fact, their atomic numbers. Although the atomic number affects the mass, it is not the
mass that is most important. It was the English physicist Henry Moseley (1887-1915) who
discovered the significance of the atomic numbers. Once the elements were arranged by
atomic number, the errors in Mendeleevs table were corrected.
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periodic table n.

a table of the chemical
elements arranged in order of atomic number, usu. in rows, so that elements with similar
atomic structure (and hence similar chemical properties) appear in vertical columns.

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Periodic
table of chemical elements |