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The periodic table of the chemical elements, also called the Mendeleev periodic table, is a tabular display of the known chemical elements. First created by Dmitri Mendeleev, the elements were originally arranged by atomic mass. Then in 1911, Henry Moseley rearranged the table more logically according to atomic number so that many chemical properties followed a regular pattern across the table. Each element is listed by its atomic number and chemical symbol. Mendeleev's and Moseley's development of the periodic table was one of the greatest achievements in modern chemistry. Chemists were able to quantitatively explain the behavior of the elements, and to predict the existence of yet undiscovered ones. There are 116 chemical elements whose discoveries have been confirmed. Ninety-four can be found naturally on Earth, and the rest have been produced in laboratories. The standard table provides the basic information on the elements. There are also other methods for displaying the chemical elements for more details or different perspectives.
GroupsA group is a vertical column in the periodic table of the elements. There are 18 groups in the standard periodic table. Elements in a group have similar configurations of their valence shell electrons, which gives them similar properties. They can also be called families. Group numbersThere are three systems of group numbers; one using Arabic numerals (1, 2, w/. 18), another using Roman numerals (I, II, w/. VIII), and one using a combination of Roman numerals and Latin letters (IA, IIA, IB, w/. VIIIA). The Roman numeral names are the original traditional names of the groups; the Arabic numeral names are a newer naming scheme recommended by the International Union of Pure and Applied Chemistry (IUPAC). The IUPAC scheme was developed to replace both older Roman numeral systems as they confusingly used the same names to mean different things. Standard periodic table
1Actinides and lanthanides are collectively known as "Rare Earth Metals". 2Alkali metals, alkaline earth metals, transition metals, actinides, lanthanides, and poor metals are all collectively known as "Metals". 3Halogens and noble gases are also non-metals. State at standard temperature and pressure
Natural occurrence
Other methods for displaying the chemical elements
And here is the periodic table for magnetic resonance. Periodicity of chemical propertiesElements adjacent to one another within a group have similar physical properties, despite their significant differences in mass. Elements adjacent to one another within a period, or energy level, have similar mass but different properties. For example, very near to nitrogen (N) in the second period of the chart are carbon (C) and oxygen (O). Despite their similarities in mass (only a few atomic mass units), they have extremely different properties, as can be seen by looking at their allotropes: diatomic oxygen is a gas that supports burning, diatomic nitrogen is a gas that does not support burning, while carbon is a solid which can be burned. Diamonds which are a form of crystallized carbon can also burn. In the group known as the halogens, the element chlorine (Cl) falls between fluorine (F) and bromine (Br). Despite their dramatic differences in mass, their allotropes have very similar properties. They are all highly corrosive. Chlorine and fluorine are gases, while bromine is a very low-boiling liquid. Chlorine and bromine are brightly colored, whereas flourine is not. Explanation of the structure of the periodic tableThe primary determinant of an element's chemical properties is its electron configuration, particularly the valence shell electrons. For instance, all atoms whose four valence electrons are found on the p shell will behave similarly, regardless of which energy level that last p shell is on. The shell in which the atom's outermost electrons reside determines the "block" to which it belongs. The number of valence shell electrons determines which family, or group, the element belongs. The total number of electron shells an atom has determines the period to which it belongs. Each shell is divided into different subshells, which as atomic number increases are filled in roughly this order:
1s
2s 2p
3s 3p
4s 3d 4p
5s 4d 5p
6s 5d 6p
7s 6d 7p
4f
5f
w/.
Hence the structure of the table. Since the outermost electrons determine chemical properties, those with the same number of valence electrons are grouped togetherw/ Progressing through a group from lightest element to heaviest element, the outer-shell electrons (those most readily accessible for participation in chemical reactions) are all in the same type of orbital, with a similar shape, but with increasingly higher energy and average distance from the nucleus. For instance, the outer-shell (or "valence") electrons of the first group, headed by hydrogen all have one electron in an s orbital. In hydrogen, that s orbital is in the lowest possible energy state of any atom, the first-shell orbital (and represented by hydrogen's position in the first period of the table). In francium, the heaviest element of the group, the outer-shell electron is in the seventh-shell orbital, significantly further out on average from the nucleus than those electrons filling all the shells below it in energy. As another example, both carbon and lead have four electrons in their outer shell orbitals. Because of the importance of the outermost shell, the different regions of the periodic table are sometimes referred to as periodic table blocks, named according to the sub-shell in which the "last" electron resides, e.g. the s-block, the p-block, the d-block, etc. HistoryMain article: History of the periodic table The original table was created without a knowledge of the inner structure of atoms: if one orders the elements by atomic mass, and then plots certain other properties against atomic mass, one sees an undulation or periodicity to these properties as a function of atomic mass. The first to recognize these regularities was the German chemist Johann Wolfgang Döbereiner who, in 1829, noticed a number of triads of similar elements:
This was followed by the English chemist John Newlands, who in 1865 noticed that the elements of similar type recurred at intervals of eight, which he likened to the octaves of music, though his law of octaves was ridiculed by his contemporaries. Finally, in 1869, the German Julius Lothar Meyer and the Russian chemist Dmitri Ivanovich Mendeleev almost simultaneously developed the first periodic table, arranging the elements by mass. However, Mendeleev plotted a few elements out of strict mass sequence in order to make a better match to the properties of their neighbours in the table, corrected mistakes in the values of several atomic masses, and predicted the existence and properties of a few new elements in the empty cells of his table. Mendeleev was later vindicated by the discovery of the electronic structure of the elements in the late 19th and early 20th century. In the 1940s Glenn T. Seaborg identified the transuranic lathanides and the actinides, which may be placed within the table, or below (as shown above). Further resources
See also
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