Earth Materials. John O'Brien

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СКАЧАТЬ Ne 2080 3963 6 130 9 361 12 180 15 240 — — Na 496 4563 6 913 9 541 13 353 16 610 20 114 26 660 Mg 737 1451 7 733 10 540 13 630 17 995 21 703 25 662 Al 578 1817 2 745 11 575 14 830 18 376 23 292 — Si 787 1577 3 231 4 356 16 091 19 784 23 783 — P 1012 1903 2 912 4 956 6 273 22 233 25 397 — S 1000 2251 3 361 4 564 7 012 8 495 27 105 — Cl 1251 2297 3 822 5 160 6 540 7 458 11 020 — Ar 1520 2665 3 931 5 570 7 238 8 781 11 995 — K 418 3052 4 220 5 877 7 975 9 590 11 343 14 944 Ca 590 1145 4 912 6 491 8 153 10 496 12 270 14 206

      2.2.3 Ionization behavior of columns (groups) on the periodic table

      The elements in every column or group on the periodic table (Table 2.3) share a similarity in their electron configuration that distinguishes them from elements in every other column. This shared property causes the elements in each group to behave in a similar manner during chemical reactions. As will be seen later in this chapter and throughout the book, knowledge of these patterns is fundamental to understanding and interpreting the formation and behavior of minerals, rocks, and other Earth materials. The tendency of atoms to form cations or anions is indicated by the location of elements in columns of the periodic СКАЧАТЬ