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Abundance of elements in Earth's crust

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67: 2554:. USGS. All production numbers are for mines, except for Al, Cd, Fe, Ge, In, N, Se (plants, refineries), S (all forms) and As, Br, Mg, Si (unspecified). Data for B, K, Ti, Y are given not for the pure element but for the most common oxide, data for Na and Cl are for NaCl. For many elements like Si, Al, data are ambiguous (many forms produced) and are taken for the pure element. U data is pure element required for consumption by current reactor fleet 44:
The Earth's crust is one "reservoir" for measurements of abundance. A reservoir is any large body to be studied as unit, like the ocean, atmosphere, mantle or crust. Different reservoirs may have different relative amounts of each element due to different chemical or mechanical processes involved in
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Estimates of elemental abundance are difficult because (a) the composition of the upper and lower crust are quite different, and (b) the composition of the continental crust can vary drastically by locality. The composition of the Earth changed after its formation due to loss of volatile compounds,
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Surendra P. Verma , E. Santoyo & Fernando Velasco-Tapia (2002) "Statistical Evaluation of Analytical Methods for the Determination of Rare-Earth Elements in Geological Materials and Implications for Detection Limits", International Geology Review, 44:4, 287–335,
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This table gives the estimated abundance in parts per million by mass of elements in the continental crust; values of the less abundant elements may vary with location by several orders of magnitude.
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is higher. Tellurium and selenium are concentrated as sulfides in the core and have also been depleted by preaccretional sorting in the nebula that caused them to form volatile
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Examines the abundance and distribution of the chemical elements in the earth's crust, as well as the figures and methods that have contributed to this knowledge.
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Abundance (atom fraction) of the chemical elements in Earth's upper continental crust as a function of atomic number; siderophiles shown in yellow
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melting and recrystalization, selective loss of some elements to the deep interior, and erosion by water. The
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of elements. These have been depleted by being relocated deeper into the Earth's core; their abundance in
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Graphs of abundance against atomic number can reveal patterns relating abundance to
3003: 2826: 2474: 2447: 2393: 25: 21: 2830: 82:. The alternation of abundance between even and odd atomic number is known as the 2991: 2561: 2397: 2356: 2478: 2992:"The abundance and distribution of the chemical elements in the earth's crust" 2938: 3103: 3015: 2459: 2451: 2345: 123: 86:. The rarest elements in the crust are not the heaviest, but are rather the 2890:"Praseodymium (Pr) - Chemical properties, Health and Environmental effects" 2359: – Naturally occurring uranium self-sustaining nuclear chain reactions 2065: 993: 79: 3082: 2491: 3033: 55: 2813:
Phoung, Sinoun; Williams, Eric; Gaustad, Gabrielle; Gupta, Ajay (2023).
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Abundance of chemical elements in Earth's (continental) crust
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ABUNDANCE OF ELEMENTS IN THE EARTH’S CRUST AND IN THE SEA,
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Anderson, Don L.; "Chemical Composition of the Mantle",
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498:350 (0.035%) 494: 491: 489: 486: 483: 482: 478: 476:370 (0.037%) 472: 469: 467: 464: 461: 460: 456: 450: 447: 445: 442: 439: 438: 434: 428: 425: 423: 420: 417: 416: 412: 410:950 (0.095%) 406: 403: 401: 398: 395: 394: 390: 384: 381: 379: 376: 373: 372: 368: 362: 359: 357: 354: 351: 350: 346: 340: 337: 335: 332: 329: 328: 324: 318: 315: 313: 310: 307: 306: 302: 296: 293: 291: 288: 285: 284: 280: 274: 271: 269: 266: 263: 262: 258: 252: 249: 247: 244: 241: 240: 236: 230: 227: 225: 222: 219: 218: 214: 208: 205: 203: 200: 197: 196: 192: 186: 183: 181: 178: 175: 174: 170: 164: 161: 159: 156: 153: 152: 148: 135: 132: 129: 127: 126: 122: 121: 115: 107: 105: 101: 97: 93: 89: 85: 81: 77: 68: 59: 57: 46: 37: 35: 31: 27: 23: 19: 3090:. 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Retrieved 2495: 2486: 2468: 2443: 2439: 2429: 2416: 2388: 2381: 2066:protactinium 1993:Siderophile 1968:Siderophile 1943:Siderophile 1918:Siderophile 1892:Chalcophile 1867:Siderophile 1841:Siderophile 1815:Siderophile 1739:Chalcophile 1713:Siderophile 1687:Chalcophile 1661:Chalcophile 1635:Chalcophile 1609:Chalcophile 1583:Chalcophile 1557:Chalcophile 1455:Chalcophile 1412:Siderophile 1369:Siderophile 1347:Chalcophile 1325:Chalcophile 1260:Chalcophile 994:praseodymium 960:10 (0.001%) 935:Chalcophile 913:Chalcophile 897:140,000,000 872:20 (0.002%) 850:20 (0.002%) 803:Siderophile 718:60 (0.006%) 715:Chalcophile 674:70 (0.007%) 671:Chalcophile 649:Siderophile 630:90 (0.009%) 520:200 (0.02%) 495:Chalcophile 391:226,000,000 281:255,000,000 231:Siderophile 124: 113: 80:geochemistry 73: 52: 43: 17: 15: 2790:"Lanthanum" 2696:www.rsc.org 1870:0.0015 (1.5 1742:0.0085 (8.5 1531:Lithophile 1506:Lithophile 1481:Lithophile 1434:Lithophile 1391:Lithophile 1304:Lithophile 1282:Lithophile 1238:Lithophile 1216:Lithophile 1194:Lithophile 1173:Lithophile 1152:Lithophile 1131:Lithophile 1088:Lithophile 1067:Lithophile 1045:Lithophile 1023:Lithophile 1001:Lithophile 979:Lithophile 957:Lithophile 869:Lithophile 847:Lithophile 825:Lithophile 781:Lithophile 759:Lithophile 737:Lithophile 721:19,400,000 693:Lithophile 677:11,900,000 627:Lithophile 611:26,000,000 605:Lithophile 583:Lithophile 567:71,250,000 561:Lithophile 539:Lithophile 501:69,300,000 473:Lithophile 451:Lithophile 429:Lithophile 413:16,000,000 407:Lithophile 385:Lithophile 369:75,000,000 341:Lithophile 325:53,200,000 319:Lithophile 303:27,700,000 297:Lithophile 275:Lithophile 253:Lithophile 215:57,600,000 209:Lithophile 187:Lithophile 171:10,335,000 165:Lithophile 136:Goldschmidt 56:lanthanides 3104:Categories 3092:2024-03-22 3074:2024-03-22 3032:BookRags, 3002:(9): 446. 2972:2024-05-23 2948:2024-05-23 2924:2024-05-23 2915:"Samarium" 2899:2024-05-23 2861:2024-05-23 2836:2024-05-23 2799:2024-05-23 2774:2024-05-23 2750:2024-05-23 2725:2024-05-23 2701:2024-05-23 2677:2024-05-23 2653:2024-05-23 2633:2024-05-23 2623:"Hydrogen" 2608:2024-05-23 2583:2024-05-23 2524:0865421234 2501:2024-03-23 2373:References 2231:promethium 2211:technetium 2044:Atmophile 2019:Atmophile 1790:Atmophile 1765:Atmophile 1716:0.015 (1.5 1664:0.075 (7.5 1638:0.085 (8.5 1405:molybdenum 1110:Atmophile 1060:dysprosium 1038:gadolinium 963:9,400,000 941:4,820,000 891:Atmophile 655:2,250,000 545:1,460,000 517:Atmophile 457:6,000,000 378:phosphorus 363:Atmophile 347:6,600,000 193:7,200,000 144:Production 96:meteoroids 40:Reservoirs 3016:0021-9584 2852:"Thorium" 2460:0034-6861 2446:: 53–74. 2311:plutonium 2291:neptunium 2022:0.0001 (1 1996:0.0007 (7 1911:ruthenium 1885:tellurium 1706:palladium 1612:0.15 (1.5 1560:0.25 (2.5 1534:0.45 (4.5 1509:0.52 (5.2 1458:0.85 (8.5 1340:germanium 1187:beryllium 1124:ytterbium 752:lanthanum 730:neodymium 532:zirconium 466:strontium 400:manganese 312:potassium 290:magnesium 202:aluminium 32:(ppm) by 2870:cite web 2741:"Cerium" 2720:Statista 2672:Statista 2558:Archived 2329:See also 2271:francium 2251:astatine 2153:polonium 2124:actinium 1971:0.001 (1 1946:0.001 (1 1921:0.001 (1 1895:0.001 (1 1844:0.004 (4 1818:0.005 (5 1808:platinum 1793:0.005 (5 1768:0.008 (8 1680:selenium 1593:130,000 1576:antimony 1474:lutetium 1448:thallium 1418:227,000 1362:tungsten 1297:europium 1275:tantalum 1266:280,000 1244:391,000 1016:samarium 884:nitrogen 818:scandium 809:123,000 620:rubidium 598:chromium 576:vanadium 554:chlorine 479:350,000 422:fluorine 356:hydrogen 334:titanium 130:Element 2080:10 (1.4 2012:krypton 1986:rhenium 1961:rhodium 1936:iridium 1749:10,200 1732:bismuth 1690:0.05 (5 1671:27,000 1628:mercury 1619:23,000 1602:cadmium 1541:31,600 1499:thulium 1427:terbium 1384:holmium 1375:86,400 1331:36,500 1318:arsenic 1231:bromine 1222:74,119 1209:uranium 1166:caesium 1145:hafnium 972:thorium 906:gallium 875:64,000 862:niobium 853:35,000 840:lithium 774:yttrium 765:12,500 699:24,000 589:76,000 435:17,000 259:18,000 246:calcium 180:silicon 133:Symbol 22:crustal 3014:  2913:MMTA. 2788:MMTA. 2739:MMTA. 2564:. WNA. 2522:  2458:  2404:  2318:trace 2298:trace 2278:trace 2258:trace 2238:trace 2218:trace 2189:trace 2160:trace 2131:trace 2102:trace 2095:radium 2073:trace 1902:2,200 1860:osmium 1851:3,100 1758:helium 1697:2,200 1654:silver 1645:4,500 1586:0.2 (2 1550:indium 1524:iodine 1484:0.8 (8 1288:1,100 1081:erbium 1007:2,500 985:5,000 796:cobalt 787:6,000 743:7,000 708:copper 686:cerium 642:nickel 510:carbon 488:sulfur 444:barium 268:sodium 158:oxygen 149:/year 147:tonnes 2578:(PDF) 2200:10%) 2196:10 (4 2182:radon 2171:10%) 2167:10 (2 2142:10%) 2138:10 (6 2113:10%) 2109:10 (9 2084:10%) 2055:10%) 2051:10 (3 2037:xenon 2026:10%) 2003:47.2 2000:10%) 1975:10%) 1950:10%) 1925:10%) 1899:10%) 1874:10%) 1848:10%) 1822:10%) 1797:10%) 1772:10%) 1746:10%) 1720:10%) 1694:10%) 1668:10%) 1642:10%) 1616:10%) 1590:10%) 1564:10%) 1538:10%) 1513:10%) 1488:10%) 1462:10%) 1103:argon 950:boron 3012:ISSN 2943:RWMM 2919:MMTA 2876:link 2794:MMTA 2745:MMTA 2520:ISBN 2456:ISSN 2402:ISBN 1834:gold 1825:172 1783:neon 1723:208 1567:655 1353:155 1200:220 1094:500 1051:400 1029:700 928:lead 919:315 664:zinc 224:iron 102:and 78:and 34:mass 16:The 3004:doi 2827:doi 2823:401 2475:doi 2448:doi 2394:doi 2315:Pu 2307:94 2295:Np 2287:93 2275:Fr 2267:87 2255:At 2247:85 2235:Pm 2227:61 2215:Tc 2207:43 2186:Rn 2178:86 2157:Po 2149:84 2134:5.5 2128:Ac 2120:89 2099:Ra 2091:88 2076:1.4 2070:Pa 2062:91 2041:Xe 2033:54 2016:Kr 2008:36 1990:Re 1982:75 1965:Rh 1957:45 1940:Ir 1932:77 1915:Ru 1907:44 1889:Te 1881:52 1864:Os 1856:76 1838:Au 1830:79 1812:Pt 1804:78 1787:Ne 1779:10 1762:He 1736:Bi 1728:83 1710:Pd 1702:46 1684:Se 1676:34 1658:Ag 1650:47 1632:Hg 1624:80 1606:Cd 1598:48 1580:Sb 1572:51 1554:In 1546:49 1520:53 1503:Tm 1495:69 1478:Lu 1470:71 1465:10 1452:Tl 1444:81 1431:Tb 1423:65 1409:Mo 1401:42 1388:Ho 1380:67 1358:74 1344:Ge 1336:32 1322:As 1314:33 1301:Eu 1293:63 1279:Ta 1271:73 1257:Sn 1253:tin 1249:50 1235:Br 1227:35 1205:92 1191:Be 1170:Cs 1162:55 1149:Hf 1141:72 1128:Yb 1120:70 1107:Ar 1099:18 1085:Er 1077:68 1064:Dy 1056:66 1042:Gd 1034:64 1020:Sm 1012:62 998:Pr 990:59 976:Th 968:90 932:Pb 924:82 910:Ga 902:31 866:Nb 858:41 844:Li 831:14 822:Sc 814:21 800:Co 792:27 770:39 756:La 748:57 734:Nd 726:60 712:Cu 704:29 690:Ce 682:58 668:Zn 660:30 646:Ni 638:28 624:Rb 616:37 602:Cr 594:24 572:23 558:Cl 550:17 536:Zr 528:40 484:16 470:Sr 462:38 448:Ba 440:56 404:Mn 396:25 374:15 338:Ti 330:22 308:19 294:Mg 286:12 272:Na 264:11 250:Ca 242:20 228:Fe 220:26 206:Al 198:13 184:Si 176:14 3106:: 3085:. 3067:. 3042:, 3018:. 3010:. 3000:31 2998:. 2994:. 2965:. 2941:. 2917:. 2892:. 2872:}} 2868:{{ 2854:. 2825:. 2821:. 2817:. 2792:. 2767:. 2743:. 2718:. 2694:. 2670:. 2625:. 2601:. 2530:^ 2494:. 2454:. 2444:28 2442:. 2438:. 2400:. 1754:2 1528:I 1366:W 1213:U 1183:4 954:B 946:5 888:N 880:7 836:3 778:Y 633:2 580:V 514:C 506:6 492:S 426:F 418:9 382:P 360:H 352:1 316:K 162:O 154:8 106:. 3095:. 3077:. 3053:. 3046:. 3036:. 3006:: 2975:. 2951:. 2927:. 2902:. 2878:) 2864:. 2839:. 2829:: 2802:. 2777:. 2753:. 2728:. 2704:. 2680:. 2656:. 2636:. 2611:. 2586:. 2504:. 2477:: 2462:. 2450:: 2410:. 2396:: 2198:× 2194:× 2192:4 2169:× 2165:× 2163:2 2140:× 2136:× 2111:× 2107:× 2105:9 2082:× 2078:× 2053:× 2049:× 2047:3 2024:× 1998:× 1973:× 1948:× 1923:× 1897:× 1872:× 1846:× 1820:× 1795:× 1770:× 1744:× 1718:× 1692:× 1666:× 1640:× 1614:× 1588:× 1562:× 1536:× 1511:× 1486:× 1460:× 125:Z

Index

crustal
chemical element
parts per million
mass
lanthanides

stellar nucleosynthesis
geochemistry
Oddo–Harkins rule
siderophile elements
Goldschmidt classification
meteoroids
hydrogen selenide
hydrogen telluride
Z
tonnes
oxygen
silicon
aluminium
iron
calcium
sodium
magnesium
potassium
titanium
hydrogen
phosphorus
manganese
fluorine
barium

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