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Nickeline

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623: 22: 80: 564:. Other localities include the eastern flank of the Widgiemooltha Dome, Western Australia, from altered pentlndite-pyrite-pyrrhotite assemblages within the Mariners, Redross and Miitel nickel mines where nickeline is produced by regional Au-As-Ag-bearing alteration and carbonate metasomatism. Other occurrences include within similarly modified nickel mines of the 698:
and milling techniques. When nickel sulfide ore deposits have been altered to produce nickeline, often the presence of arsenic renders the ore uneconomic when concentrations of As reach several hundred parts per million. However, arsenic bearing nickel ore may be treated by blending with 'clean' ore
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The primary problem for treating nickeline in conventionally constructed nickel mills is the specific gravity of nickeline versus that of pentlandite. This renders the ore difficult to treat via the froth flotation technique. Within the smelter itself, the nickeline contributes to high arsenic
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would sometimes find a red mineral, superficially resembling copper ore. Upon attempting extraction, no copper was produced, and subsequently, the miners would be afflicted with mysterious illness. They blamed a mischievous sprite of German mythology, Nickel (similar to
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was attempting to extract copper from kupfernickel mineral, and obtained instead a white metal which he named "nickel", after the sprite. In modern German, Kupfernickel and Kupfer-Nickel designates the alloy
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of nickeline is used as the prototype of a group of crystalline solids with similar crystal structures. The structure consists of two interpenetrating sublattices: a
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of sulfide-free ultramafic rocks, where metasomatic fluids introduce sulfur, carbonate, and arsenic. This typically results in mineral assemblages including
368:(NiAs). The naturally-occurring mineral contains roughly 43.9% nickel and 56.1% arsenic by mass, but composition of the mineral may vary slightly. 408:) for besetting the copper (German: Kupfer). This German equivalent of "copper-nickel" was used as early as 1694 (other old German synonyms are 479: 454: 957: 596: 1027: 997: 206:
Pale copper red with blackish tarnish. white with strong yellowish pink hue on polished section strongly anisotropic
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The main compound within nickeline, nickel arsenide (NiAs), can be prepared by direct combination of the elements:
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Inorganic Chemistry by Duward Shriver and Peter Atkins, 3rd Edition, W.H. Freeman and Company, 1999, pp.47,48.
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Nickeline is rarely used as a source of nickel due to the presence of arsenic, which is deleterious to most
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sources, to produce a blended feedstock which the mill and smelter can handle with acceptable recovery.
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Massive columnar to reniform, rarely as distorted, horizontally striated, {1011} terminated crystals
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coordinated to six nickel atoms. Compounds adopting the NiAs structure are generally the
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contents which require additional reagents and fluxes to strip from the nickel metal.
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Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (2005).
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Nickeline is formed by hydrothermal modification of ultramafic rocks and associated
934: 930: 889: 741: 616: 304: 221: 100: 832: 557: 553: 43: 482:, and may be formed by replacement of nickel-copper bearing sulfides (replacing 622: 140: 48: 872:(1932). "The discovery of the elements: III. Some eighteenth-century metals". 1006: 643: 538: 495: 400: 388: 211: 152: 534: 510: 487: 805: 546: 530: 499: 483: 425: 314: 167: 746: 721: 811: 634: 542: 526: 324: 159: 383:
are usually present, and sometimes the arsenic is largely replaced by
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via sulfidation and associated arsenopyrite-nickeline-breithauptite.
491: 145: 695: 608: 604: 384: 190: 952:(5th ed.). New York: W. H. Freeman and Company. p. 383. 612: 561: 365: 358: 112: 549:(a coating of green nickel arsenate) on exposure to moist air. 518: 514: 503: 444: 380: 372: 362: 109: 552:
Most of these minerals can be found in the areas surrounding
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recommended use of the name nickeline rather than niccolite.
79: 486:, and in association with copper arsenic sulfides), or via 376: 771: 630:
The following are the members of the nickeline group:
29:It has been suggested that this article should be 595:to six arsenic atoms, while each arsenic atom is 399:Medieval miners looking for copper in the German 1004: 443:from J. D. Dana, 1868, refer to the presence of 947: 387:. This last forms an isomorphous series with 900: 767: 765: 830: 745: 431:The names subsequently given to the ore, 800: 798: 621: 588:arsenic sublattice. Each nickel atom is 394: 950:Shriver and Atkins' Inorganic Chemistry 762: 455:International Mineralogical Association 1005: 689: 460: 868: 857:Chambers Twentieth Century Dictionary 824: 795: 722:"IMA–CNMNC approved mineral symbols" 719: 571: 15: 859:, p888, W&R Chambers Ltd, 1977. 193:, c = 5.009 Ă…; Z = 2 13: 236:{1010} Imperfect, {0001} Imperfect 14: 1039: 948:Shriver, D.; Atkins, P. (2009). 157:Dihexagonal dipyramidal (6/mmm) 78: 20: 978: 966: 941: 935:10.1180/minmag.1971.038.293.14 862: 850: 713: 1: 874:Journal of Chemical Education 706: 509:Associated minerals include: 473: 226:On {1011} producing fourlings 992:Dana's Manual of Mineralogy 7: 1028:Minerals in space group 194 10: 1044: 626:The unit cell of nickeline 975:". Retrieved 20 May 2022. 831:Barthelmy, David (2014). 783:. Mineral Data Publishing 341: 333: 323: 313: 303: 293: 283: 273: 260: 250: 240: 230: 220: 210: 202: 197: 183: 166: 151: 139: 129: 119: 99: 91: 86: 77: 72: 833:"Nickeline Mineral Data" 584:nickel sublattice and a 361:consisting primarily of 319:Strong (reflected light) 469:Ni(s) + As(s) → NiAs(s) 67:Nickel arsenide mineral 921:(293): 102–105. 1971. 915:Mineralogical Magazine 781:Handbook of Mineralogy 726:Mineralogical Magazine 627: 597:trigonal prismatically 586:hexagonal close-packed 545:. Nickeline alters to 421:Axel Fredrik Cronstedt 337:garlic odor on heating 973:The Mineral Nickeline 625: 395:Etymology and history 391:(nickel antimonide). 334:Other characteristics 131:Strunz classification 35:into articles titled 371:Small quantities of 927:1971MinM...38..102. 886:1932JChEd...9...22W 747:10.1180/mgm.2021.43 738:2021MinM...85..291W 720:Warr, L.N. (2021). 690:Economic importance 582:primitive hexagonal 461:Preparation of NiAs 1023:Hexagonal minerals 870:Weeks, Mary Elvira 628: 1018:Arsenide minerals 959:978-1-4292-1820-7 617:transition metals 572:Crystal structure 348: 347: 65: 64: 1035: 985: 982: 976: 970: 964: 963: 945: 939: 938: 912: 904: 898: 897: 894:10.1021/ed009p22 866: 860: 854: 848: 847: 845: 843: 828: 822: 821: 820: 818: 802: 793: 792: 790: 788: 778: 769: 760: 759: 749: 717: 685: 679: 673: 667: 661: 655: 649: 640: 498:and metamorphic 470: 305:Specific gravity 266: 106: 105:(repeating unit) 95:Arsenide mineral 82: 70: 69: 60: 57: 24: 23: 16: 1043: 1042: 1038: 1037: 1036: 1034: 1033: 1032: 1013:Nickel minerals 1003: 1002: 989: 988: 983: 979: 971: 967: 960: 946: 942: 910: 906: 905: 901: 867: 863: 855: 851: 841: 839: 829: 825: 816: 814: 804: 803: 796: 786: 784: 776: 770: 763: 718: 714: 709: 692: 683: 677: 671: 665: 659: 653: 647: 638: 574: 476: 468: 463: 419:In 1751, Baron 397: 264: 189:a = 3.602  178: 162:: (6/m 2/m 2/m) 158: 104: 103: 68: 61: 55: 52: 44:Nickel arsenide 25: 21: 12: 11: 5: 1041: 1031: 1030: 1025: 1020: 1015: 1001: 1000: 987: 986: 977: 965: 958: 940: 899: 861: 849: 837:Webmineral.com 823: 794: 761: 732:(3): 291–320. 711: 710: 708: 705: 691: 688: 687: 686: 680: 676:Sobolevskite: 674: 668: 662: 656: 650: 641: 573: 570: 475: 472: 462: 459: 396: 393: 346: 345: 343: 339: 338: 335: 331: 330: 327: 321: 320: 317: 311: 310: 307: 301: 300: 297: 291: 290: 289:brownish black 287: 281: 280: 277: 271: 270: 267: 258: 257: 254: 248: 247: 244: 238: 237: 234: 228: 227: 224: 218: 217: 214: 208: 207: 204: 200: 199: 198:Identification 195: 194: 187: 181: 180: 176: 170: 164: 163: 155: 149: 148: 143: 141:Crystal system 137: 136: 133: 127: 126: 123: 117: 116: 107: 97: 96: 93: 89: 88: 84: 83: 75: 74: 66: 63: 62: 28: 26: 19: 9: 6: 4: 3: 2: 1040: 1029: 1026: 1024: 1021: 1019: 1016: 1014: 1011: 1010: 1008: 999: 998:0-471-03288-3 995: 991: 990: 981: 974: 969: 961: 955: 951: 944: 936: 932: 928: 924: 920: 916: 909: 903: 895: 891: 887: 883: 879: 875: 871: 865: 858: 853: 838: 834: 827: 813: 809: 808: 801: 799: 782: 775: 768: 766: 757: 753: 748: 743: 739: 735: 731: 727: 723: 716: 712: 704: 700: 697: 681: 675: 669: 663: 657: 651: 645: 644:Breithauptite 642: 636: 633: 632: 631: 624: 620: 618: 614: 610: 606: 602: 601:chalcogenides 598: 594: 591: 587: 583: 579: 569: 567: 563: 559: 555: 550: 548: 544: 540: 539:breithauptite 536: 532: 528: 524: 520: 516: 512: 507: 505: 501: 497: 496:heazelwoodite 493: 489: 485: 481: 471: 466: 458: 456: 453:In 1971, the 451: 450: 446: 442: 438: 437:F. S. Beudant 434: 429: 427: 422: 417: 415: 411: 410:Rotnickelkies 407: 402: 401:Ore Mountains 392: 390: 389:breithauptite 386: 382: 378: 374: 369: 367: 364: 360: 356: 352: 344: 340: 336: 332: 328: 326: 322: 318: 316: 312: 308: 306: 302: 298: 296: 292: 288: 286: 282: 278: 276: 272: 268: 263: 259: 255: 253: 249: 245: 243: 239: 235: 233: 229: 225: 223: 219: 215: 213: 212:Crystal habit 209: 205: 201: 196: 192: 188: 186: 182: 174: 171: 169: 165: 161: 156: 154: 153:Crystal class 150: 147: 144: 142: 138: 134: 132: 128: 124: 122: 118: 114: 111: 108: 102: 98: 94: 90: 85: 81: 76: 71: 59: 50: 46: 45: 40: 39: 34: 33: 27: 18: 17: 980: 968: 949: 943: 918: 914: 902: 877: 873: 864: 856: 852: 840:. Retrieved 836: 826: 815:, retrieved 806: 785:. Retrieved 780: 729: 725: 715: 701: 693: 682:Sudburyite: 664:Langistite: 658:Kotulskite: 652:Freboldite: 629: 590:octahedrally 575: 551: 535:chalcopyrite 511:arsenopyrite 508: 488:metasomatism 480:ore deposits 477: 467: 464: 452: 448: 447:; in Latin, 440: 439:, 1832, and 432: 430: 418: 413: 409: 405: 398: 370: 354: 350: 349: 172: 56:January 2022 53: 42: 37: 36: 30: 774:"Nickeline" 670:Nickeline: 613:bismuthides 609:antimonides 593:coordinated 547:annabergite 531:pentlandite 500:pentlandite 484:pentlandite 426:Cupronickel 414:Arsennickel 315:Pleochroism 295:Diaphaneity 168:Space group 1007:Categories 812:Mindat.org 707:References 635:Achavalite 543:maucherite 527:pyrrhotite 474:Occurrence 441:niccolite, 342:References 325:Fusibility 262:Mohs scale 246:Conchoidal 160:H-M symbol 121:IMA symbol 880:(1): 22. 842:13 August 817:13 August 807:Nickeline 787:13 August 756:235729616 684:(Pd,Ni)Sb 678:Pd(Bi,Te) 666:(Co,Ni)As 660:Pd(Te,Bi) 605:arsenides 578:unit cell 523:cobaltite 492:millerite 449:niccolum. 433:nickeline 355:niccolite 351:Nickeline 185:Unit cell 146:Hexagonal 73:Nickeline 38:Nickeline 696:smelting 566:Kambalda 406:Old Nick 385:antimony 366:arsenide 279:metallic 265:hardness 252:Tenacity 242:Fracture 232:Cleavage 222:Twinning 113:arsenide 92:Category 923:Bibcode 882:Bibcode 734:Bibcode 562:Ontario 554:Sudbury 359:mineral 269:5 – 5.5 256:Brittle 135:2.CC.05 101:Formula 87:General 49:discuss 996:  956:  754:  568:area. 558:Cobalt 519:silver 515:barite 504:pyrite 445:nickel 381:cobalt 373:sulfur 363:nickel 299:Opaque 285:Streak 275:Luster 115:(NiAs) 110:nickel 911:(PDF) 777:(PDF) 752:S2CID 435:from 357:is a 203:Color 32:split 994:ISBN 954:ISBN 844:2022 819:2022 789:2022 672:NiAs 654:CoSe 648:NiSb 639:FeSe 611:and 576:The 556:and 541:and 412:and 379:and 377:iron 179:/mmc 41:and 931:doi 890:doi 742:doi 619:. 615:of 521:, 416:). 353:or 309:7.8 51:) 47:. ( 1009:: 929:. 919:38 917:. 913:. 888:. 876:. 835:. 810:, 797:^ 779:. 764:^ 750:. 740:. 730:85 728:. 724:. 646:: 637:: 607:, 603:, 560:, 537:, 533:, 529:, 525:, 517:, 513:, 494:, 428:. 375:, 125:Nc 962:. 937:. 933:: 925:: 896:. 892:: 884:: 878:9 846:. 791:. 758:. 744:: 736:: 502:- 329:2 191:Ă… 177:3 175:6 173:P 58:) 54:(

Index

split
Nickeline
Nickel arsenide
discuss

Formula
nickel
arsenide
IMA symbol
Strunz classification
Crystal system
Hexagonal
Crystal class
H-M symbol
Space group
Unit cell
Ă…
Crystal habit
Twinning
Cleavage
Fracture
Tenacity
Mohs scale
Luster
Streak
Diaphaneity
Specific gravity
Pleochroism
Fusibility
mineral

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