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A block of the periodic table is a set of elements unified by the atomic orbitals their valence electrons or vacancies lie in. [1] The term seems to have been first used by Charles Janet. [2] Each block is named after its characteristic orbital: s-block , p-block , d-block , f-block and g-block .
Periodic table of the chemical elements showing the most or more commonly named sets of elements (in periodic tables), and a traditional dividing line between metals and nonmetals. The f-block actually fits between groups 2 and 3 ; it is usually shown at the foot of the table to save horizontal space.
Many other names have been used for this set, and its borders are not agreed on. Precious metals – Variously-defined group of non-radioactive metals of high economical value. Superactinides – Hypothetical series of elements 121 to 157, which includes a predicted "g-block" of the periodic table.
A more conventional long form of periodic table is included for comparison. The advantage of the long form is that shows where the lanthanides and actinides fit into the periodic table; its disadvantage is its width. Some other notable long tables include: 1892 — Bassett's vertical arrangement: 37 columns sideways [61]
Like the periodic table, ... originally the name of 222 Rn: 18 6 p-block ... + actinium; protactinium decays into actinium. f-block groups 7 f-block 231.04: 15.37: 1841:
Element names are those accepted by IUPAC. Block indicates the periodic table block for each element: red = s-block, yellow = p-block, blue = d-block, green = f-block. Group and period refer to an element's position in the periodic table. Group numbers here show the currently accepted numbering; for older numberings, see Group (periodic table)
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Groups (columns in the periodic table; sometimes called 'family') are numbered 1–18, following modern IUPAC guidelines. So called trivial group names, like halogens, are well defined and acceptable. Each group can also be identified by its top element: group 14 = carbon group.