Knowledge (XXG)

Maghemite

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transport system. The presence of the particles indicated that they are suspended for long periods due to poor ventilation, particularly on platforms. The health implications presented by the particles were not investigated.
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There is experimental and theoretical evidence that Fe(III) cations and vacancies tend to be ordered in the octahedral sites, in a way that maximizes the homogeneity of the distribution and therefore minimizes the
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Litter, M. I. & Blesa, M. A. (1992). "Photodissolution of iron oxides. IV. A comparative study on the photodissolution of hematite, magnetite, and maghemite in EDTA media".
492: 626:(~950 K), which together with its low cost and chemical stability led to its wide application as a magnetic pigment in electronic recording media since the 1940s. 554:. It is known to also form in areas that have been subjected to bushfires (particularly in the Leonora area of Western Australia) magnetising iron minerals. 1148: 569:. The name alludes to somewhat intermediate character between magnetite and hematite. It can appear blue with a grey shade, white, or brown. It has 358: 884:
Grau-Crespo, Ricardo; Al-Baitai, Asmaa Y; Saadoune, Iman; De Leeuw, Nora H (2010). "Vacancy ordering and electronic structure of γ-Fe
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It was found in 2022 that high levels of maghemite particles small enough to enter the bloodstream if inhaled, some as small as five
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or titanomagnetite. Maghemite can also form through dehydration and transformation of certain iron oxyhydroxide minerals, such as
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Rarely as minute octahedral crystals, or acicular overgrowths; commonly as coatings on or replacements of magnetite; massive.
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Pankhurst, Q A; Connolly, J; Jones, S K; Dobson, J (2003). "Applications of magnetic nanoparticles in biomedicine".
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Gaines, Richard V.; Skinner, H. Catherine W.; Foord, Eugene E.; Mason, Brian and Rosenzweig, Abraham (1997)
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Greaves, C. (1983). "A powder neutron diffraction investigation of vacancy ordering and covalence in γ-Fe
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a = 8.33 Å; Z = 8 or a = 8.35 Å c = 24.99 Å; Z = 8 for tetragonal supercell
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Brown, bluish black; brown to yellow in transmitted light; white to bluish gray in reflected light.
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Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (1997).
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Dronskowski, R. (2010). "The little maghemite story: A classic functional material".
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represents a vacancy, A indicates tetrahedral and B octahedral positioning.
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of ca. 2 eV, although the precise value of the gap depends on the electron
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crystals. Maghemite is formed by the topotactic oxidation of magnetite.
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The Iron Oxides: Structure, Properties, Reactions, Occurrences and Uses
603: 587: 539: 527: 768: 467:{\displaystyle \left({\ce {Fe^{III}8}}\right)_{A}\left_{B}{\ce {O32}}} 1060:
Sheikh, H. A.; Tung, P. Y.; Ringe, E.; Harrison, R. J. (2022-12-15).
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can be considered as an Fe(II)-deficient magnetite with formula
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Maghemite was named in 1927 for an occurrence at the
480: 361: 283: 275: 267: 257: 247: 237: 227: 214: 204: 194: 184: 176: 171: 161: 137: 119: 106: 96: 86: 65: 55: 50: 36: 486: 466: 8: 534:and soils. It is associated with magnetite, 526:. It occurs as widespread brown or yellow 892:(maghemite): a theoretical investigation". 795:Cornell, R. M. and Schwertmann, Udo (2003) 349:. It is sometimes spelled as "maghaemite". 879: 877: 729: 727: 16:Iron oxide with a spinel ferrite structure 1093: 905: 696: 479: 459: 454: 449: 443: 434: 424: 414: 404: 399: 388: 377: 372: 367: 360: 779: 777: 764: 762: 341: 337: 663: 820:, John Wiley & Sons. pp. 229-230. 33: 1009:Journal of Physics D: Applied Physics 253:Opaque, transparent in thin fragments 7: 894:Journal of Physics: Condensed Matter 673:"IMA–CNMNC approved mineral symbols" 1149:Minerals in space group 212 or 213 14: 42: 311:) is a member of the family of 924:10.1088/0953-8984/22/25/255401 1: 868:10.1016/S0022-4596(83)80010-3 514:containing iron(II) such as 1021:10.1088/0022-3727/36/13/201 115:with a tetragonal supercell 1165: 1078:10.1038/s41598-022-24679-4 18: 567:Shasta County, California 41: 487:{\displaystyle \square } 19:Not to be confused with 994:10.1002/chin.200125209 743:Handbook of Mineralogy 677:Mineralogical Magazine 649:, were present in the 488: 468: 818:Dana's new mineralogy 622:ordering with a high 489: 469: 276:Other characteristics 98:Strunz classification 799:. Wiley-VCH. p. 32. 594:Electronic structure 584:electrostatic energy 550:, lepidocrocite and 478: 359: 1049:. 15 December 2022. 916:2010JPCM...22y5401G 860:1983JSSCh..49..325G 848:J. Solid State Chem 698:10.1180/mgm.2021.43 689:2021MinM...85..291W 671:Warr, L.N. (2021). 618:Maghemite exhibits 577:Cation distribution 506:or low-temperature 502:Maghemite forms by 462: 437: 419: 382: 1124:Iron(III) minerals 1066:Scientific Reports 651:London Underground 559:Iron Mountain Mine 484: 464: 450: 420: 400: 368: 315:. It has the same 268:Optical properties 263:4.860 (calculated) 1139:Magnetic minerals 453: 432: 417: 412: 403: 380: 371: 290: 289: 279:Strongly magnetic 133: 1156: 1108: 1107: 1097: 1057: 1051: 1050: 1039: 1033: 1032: 1004: 998: 997: 977: 971: 970: 950: 944: 943: 909: 881: 872: 871: 835: 829: 814: 808: 793: 787: 781: 772: 766: 757: 756: 740: 731: 722: 717: 711: 710: 700: 668: 624:Néel temperature 493: 491: 490: 485: 473: 471: 470: 465: 463: 461: 458: 451: 448: 447: 442: 438: 436: 433: 425: 418: 415: 413: 405: 401: 393: 392: 387: 383: 381: 378: 376: 369: 344: 259:Specific gravity 220: 127: 72: 71:(repeating unit) 46: 34: 1164: 1163: 1159: 1158: 1157: 1155: 1154: 1153: 1114: 1113: 1112: 1111: 1059: 1058: 1054: 1041: 1040: 1036: 1006: 1005: 1001: 979: 978: 974: 967:10.1139/v92-316 952: 951: 947: 891: 887: 883: 882: 875: 845: 841: 837: 836: 832: 815: 811: 794: 790: 782: 775: 767: 760: 753: 738: 733: 732: 725: 720:Mineralienatlas 718: 714: 670: 669: 665: 660: 643: 616: 598:Maghemite is a 596: 579: 561:, northwest of 530:in terrestrial 500: 476: 475: 395: 394: 363: 362: 357: 356: 343: 339: 335: 323:, but the same 310: 306: 302: 298: 218: 156: 148: 126: 125:Gyroidal (432) 82: 78: 70: 69: 32: 17: 12: 11: 5: 1162: 1160: 1152: 1151: 1146: 1144:Cubic minerals 1141: 1136: 1134:Ilmenite group 1131: 1129:Oxide minerals 1126: 1116: 1115: 1110: 1109: 1052: 1034: 999: 972: 945: 900:(25): 255401. 889: 885: 873: 854:(3): 325–333. 843: 839: 830: 809: 788: 773: 758: 751: 723: 712: 683:(3): 291–320. 662: 661: 659: 656: 642: 639: 615: 612: 595: 592: 578: 575: 499: 496: 483: 457: 446: 441: 431: 428: 423: 411: 408: 398: 391: 386: 375: 366: 345:) and is also 308: 304: 300: 296: 288: 287: 285: 281: 280: 277: 273: 272: 269: 265: 264: 261: 255: 254: 251: 245: 244: 241: 235: 234: 231: 225: 224: 221: 212: 211: 208: 202: 201: 198: 192: 191: 188: 182: 181: 178: 174: 173: 172:Identification 169: 168: 165: 159: 158: 154: 146: 141: 135: 134: 123: 117: 116: 110: 108:Crystal system 104: 103: 100: 94: 93: 90: 84: 83: 80: 76: 73: 63: 62: 60:Oxide minerals 57: 53: 52: 48: 47: 39: 38: 15: 13: 10: 9: 6: 4: 3: 2: 1161: 1150: 1147: 1145: 1142: 1140: 1137: 1135: 1132: 1130: 1127: 1125: 1122: 1121: 1119: 1105: 1101: 1096: 1091: 1087: 1083: 1079: 1075: 1071: 1067: 1063: 1056: 1053: 1048: 1044: 1038: 1035: 1030: 1026: 1022: 1018: 1014: 1010: 1003: 1000: 995: 991: 987: 983: 976: 973: 968: 964: 960: 956: 949: 946: 941: 937: 933: 929: 925: 921: 917: 913: 908: 903: 899: 895: 880: 878: 874: 869: 865: 861: 857: 853: 849: 834: 831: 827: 823: 819: 813: 810: 806: 802: 798: 792: 789: 785: 780: 778: 774: 770: 765: 763: 759: 754: 748: 744: 737: 730: 728: 724: 721: 716: 713: 708: 704: 699: 694: 690: 686: 682: 678: 674: 667: 664: 657: 655: 652: 648: 640: 638: 636: 632: 631:nanoparticles 627: 625: 621: 620:ferrimagnetic 613: 611: 609: 605: 601: 600:semiconductor 593: 591: 589: 585: 576: 574: 572: 568: 564: 560: 555: 553: 549: 545: 541: 537: 533: 529: 525: 521: 520:lepidocrocite 517: 513: 509: 505: 497: 495: 481: 455: 444: 439: 429: 426: 421: 409: 406: 396: 389: 384: 373: 364: 354: 350: 348: 347:ferrimagnetic 333: 330:structure as 329: 326: 322: 318: 314: 294: 286: 282: 278: 274: 270: 266: 262: 260: 256: 252: 250: 246: 242: 240: 236: 232: 230: 226: 222: 217: 213: 210:Subconchoidal 209: 207: 203: 199: 197: 193: 189: 187: 186:Crystal habit 183: 179: 175: 170: 166: 164: 160: 152: 145: 142: 140: 136: 131: 124: 122: 121:Crystal class 118: 114: 111: 109: 105: 101: 99: 95: 91: 89: 85: 74: 68: 64: 61: 58: 54: 49: 45: 40: 35: 30: 26: 22: 1072:(1): 20298. 1069: 1065: 1055: 1046: 1037: 1015:(13): R167. 1012: 1008: 1002: 985: 981: 975: 958: 955:Can. J. Chem 954: 948: 897: 893: 851: 847: 833: 817: 812: 796: 791: 786:. Webmineral 742: 715: 680: 676: 666: 644: 641:As pollutant 633:are used in 628: 617: 614:Applications 597: 580: 556: 524:ferrihydrite 501: 352: 351: 292: 291: 150: 143: 961:(9): 2502. 736:"Maghemite" 635:biomedicine 313:iron oxides 249:Diaphaneity 139:Space group 1118:Categories 988:(25): no. 982:ChemInform 826:0471193100 805:3527302743 752:0962209732 658:References 647:nanometres 629:Maghemite 504:weathering 498:Occurrence 284:References 216:Mohs scale 130:H-M symbol 88:IMA symbol 1086:2045-2322 907:1005.2370 784:Maghemite 769:Maghemite 707:235729616 571:isometric 548:marcasite 532:sediments 516:magnetite 508:oxidation 482:◻ 422:◻ 353:Maghemite 332:magnetite 293:Maghemite 271:Isotropic 163:Unit cell 37:Maghemite 29:Magnemite 25:Magnetite 21:Magnesite 1104:36522360 1047:BBC News 1029:51768859 932:21393797 771:. Mindat 552:goethite 536:ilmenite 321:hematite 219:hardness 206:Fracture 196:Cleavage 56:Category 1095:9755232 912:Bibcode 856:Bibcode 685:Bibcode 604:bandgap 602:with a 588:crystal 586:of the 563:Redding 540:anatase 528:pigment 512:spinels 328:ferrite 317:formula 102:4.BB.15 67:Formula 51:General 1102:  1092:  1084:  1027:  940:778411 938:  930:  824:  803:  749:  705:  544:pyrite 474:where 325:spinel 303:, γ-Fe 239:Streak 229:Luster 128:(same 1025:S2CID 936:S2CID 902:arXiv 739:(PDF) 703:S2CID 243:Brown 177:Color 113:Cubic 27:, or 1100:PMID 1082:ISSN 928:PMID 822:ISBN 801:ISBN 747:ISBN 608:spin 522:and 233:Dull 200:None 149:32, 75:γ-Fe 1090:PMC 1074:doi 1017:doi 990:doi 963:doi 920:doi 864:doi 846:". 693:doi 510:of 416:III 379:III 319:as 295:(Fe 92:Mgh 1120:: 1098:. 1088:. 1080:. 1070:12 1068:. 1064:. 1045:. 1023:. 1013:36 1011:. 986:32 984:. 959:70 957:. 934:. 926:. 918:. 910:. 898:22 896:. 876:^ 862:. 852:49 850:. 776:^ 761:^ 741:. 726:^ 701:. 691:. 681:85 679:. 675:. 610:. 590:. 565:, 546:, 542:, 538:, 456:32 407:40 402:Fe 370:Fe 336:Fe 157:32 144:P4 23:, 1106:. 1076:: 1031:. 1019:: 996:. 992:: 969:. 965:: 942:. 922:: 914:: 904:: 890:3 888:O 886:2 870:. 866:: 858:: 844:3 842:O 840:2 828:. 807:. 755:. 709:. 695:: 687:: 452:O 445:B 440:] 430:3 427:8 410:3 397:[ 390:A 385:) 374:8 365:( 342:4 340:O 338:3 334:( 309:3 307:O 305:2 301:3 299:O 297:2 223:5 155:3 153:4 151:P 147:1 132:) 81:3 79:O 77:2 31:.

Index

Magnesite
Magnetite
Magnemite

Oxide minerals
Formula
IMA symbol
Strunz classification
Crystal system
Cubic
Crystal class
H-M symbol
Space group
Unit cell
Crystal habit
Cleavage
Fracture
Mohs scale
Luster
Streak
Diaphaneity
Specific gravity
iron oxides
formula
hematite
spinel
ferrite
magnetite
ferrimagnetic
weathering

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