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Nitisol

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Nitisols are technically defined by a significant accumulation of clay (30 percent or more by mass and extending as much as 150 cm below the surface) and by a blocky aggregate structure. Iron oxides and high-water content are believed to play important roles in creating the soil structure. Nitisols
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are also strongly influenced by biological activity, resulting in a homogenization of the upper portion of the soil profile. These soils are related to the
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or a blocky structure, breaking into a polyhedral or a flat-edged structure. The soil aggregates show pressure faces. Nitisols correlate with the
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IUSS Working Group WRB: World Reference Base for Soil Resources, fourth edition. International Union of Soil Sciences, Vienna 2022.
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These soils are found in the tropics and subtropics; there are extensive areas of them in the tropical highlands of
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W. Zech, P. Schad, G. Hintermaier-Erhard: Soils of the World. Springer, Berlin 2022, Chapter 9.3.2.
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soil groups originating in tropical climates and also containing layers with clay accumulations are
625: 620: 583: 304: 255: 921: 897: 283: 751: 8: 320: 145: 871: 504: 297: 60: 916: 786: 261: 247: 166: 791: 220:"Nitisol | Soil Classification, Clay Content & Nutrient Retention | Britannica" 856: 841: 701: 831: 776: 40: 910: 876: 761: 219: 112: 861: 806: 83:. Nitisols form from fine-textured material weathered from intermediate to 36: 866: 846: 766: 746: 726: 716: 711: 277: 135: 55: 851: 801: 756: 741: 706: 676: 542: 449: 414: 389: 108: 96: 92: 84: 289: 836: 781: 721: 484: 479: 469: 404: 374: 354: 88: 821: 736: 691: 567: 547: 537: 522: 494: 489: 474: 444: 439: 419: 409: 394: 379: 369: 364: 359: 189:"Major Soils of the World. ISRIC Wageningen, The Netherlands, 2001" 140: 80: 68: 51: 47: 771: 731: 696: 686: 681: 671: 666: 562: 532: 527: 517: 512: 464: 459: 429: 424: 399: 384: 349: 344: 339: 124: 120: 104: 881: 816: 557: 552: 454: 796: 72: 826: 661: 656: 651: 646: 32: 167:"Mineral Soils conditioned by a Wet (Sub)Tropical Climate" 16: 811: 908: 305: 312: 298: 39:content of at least 30% and a polyhedral 164: 15: 319: 29:World Reference Base for Soil Resources 909: 606:Canadian system of soil classification 293: 284:profile photos (with classification) 278:profile photos (with classification) 31:(WRB), is a deep, red, well-drained 13: 590:Unified Soil Classification System 240: 181: 14: 933: 595:AASHTO Soil Classification System 271: 893: 892: 99:dominate their clay mineralogy. 77:Democratic Republic of the Congo 611:Australian Soil Classification 602:(French classification system) 212: 158: 1: 151: 7: 631:List of vineyard soil types 129: 10: 938: 616:Polish Soil Classification 890: 640:Non-systematic soil types 639: 576: 503: 327: 115:. Soil Taxonomy. Related 626:List of U.S. state soils 20:Distribution of nitisols 621:1938 USDA soil taxonomy 600:RĂ©fĂ©rentiel pĂ©dologique 584:FAO soil classification 165:Delvaux, B.; Brahy, V. 21: 19: 752:Calcareous grassland 329:World Reference Base 321:Soil classification 286:IUSS World of Soils 146:Soil classification 505:USDA soil taxonomy 331:for Soil Resources 224:www.britannica.com 61:USDA soil taxonomy 22: 904: 903: 266:978-3-540-30460-9 252:979-8-9862451-1-9 85:basic parent rock 929: 896: 895: 792:Hydrophobic soil 314: 307: 300: 291: 290: 234: 233: 231: 230: 216: 210: 209: 207: 206: 200: 194:. Archived from 193: 185: 179: 178: 176: 174: 162: 937: 936: 932: 931: 930: 928: 927: 926: 907: 906: 905: 900: 886: 857:Subaqueous soil 842:Serpentine soil 702:Parent material 635: 572: 499: 330: 323: 318: 274: 243: 241:Further reading 238: 237: 228: 226: 218: 217: 213: 204: 202: 198: 191: 187: 186: 182: 172: 170: 163: 159: 154: 132: 12: 11: 5: 935: 925: 924: 919: 902: 901: 891: 888: 887: 885: 884: 879: 874: 869: 864: 859: 854: 849: 844: 839: 834: 832:Prime farmland 829: 824: 819: 814: 809: 804: 799: 794: 789: 787:Fuller's earth 784: 779: 777:Expansive clay 774: 769: 764: 759: 754: 749: 744: 739: 734: 729: 724: 719: 714: 709: 704: 699: 694: 689: 684: 679: 674: 669: 664: 659: 654: 649: 643: 641: 637: 636: 634: 633: 628: 623: 618: 613: 608: 603: 597: 592: 587: 580: 578: 574: 573: 571: 570: 565: 560: 555: 550: 545: 540: 535: 530: 525: 520: 515: 509: 507: 501: 500: 498: 497: 492: 487: 482: 477: 472: 467: 462: 457: 452: 447: 442: 437: 432: 427: 422: 417: 412: 407: 402: 397: 392: 387: 382: 377: 372: 367: 362: 357: 352: 347: 342: 336: 334: 325: 324: 317: 316: 309: 302: 294: 288: 287: 281: 273: 272:External links 270: 269: 268: 258: 242: 239: 236: 235: 211: 180: 156: 155: 153: 150: 149: 148: 143: 138: 131: 128: 111:orders of the 9: 6: 4: 3: 2: 934: 923: 922:Types of soil 920: 918: 915: 914: 912: 899: 898:Types of soil 889: 883: 880: 878: 877:Tropical peat 875: 873: 870: 868: 865: 863: 860: 858: 855: 853: 850: 848: 845: 843: 840: 838: 835: 833: 830: 828: 825: 823: 820: 818: 815: 813: 810: 808: 805: 803: 800: 798: 795: 793: 790: 788: 785: 783: 780: 778: 775: 773: 770: 768: 765: 763: 762:Dry quicksand 760: 758: 755: 753: 750: 748: 745: 743: 740: 738: 735: 733: 730: 728: 725: 723: 720: 718: 715: 713: 710: 708: 705: 703: 700: 698: 695: 693: 690: 688: 685: 683: 680: 678: 675: 673: 670: 668: 665: 663: 660: 658: 655: 653: 650: 648: 645: 644: 642: 638: 632: 629: 627: 624: 622: 619: 617: 614: 612: 609: 607: 604: 601: 598: 596: 593: 591: 588: 585: 582: 581: 579: 577:Other systems 575: 569: 566: 564: 561: 559: 556: 554: 551: 549: 546: 544: 541: 539: 536: 534: 531: 529: 526: 524: 521: 519: 516: 514: 511: 510: 508: 506: 502: 496: 493: 491: 488: 486: 483: 481: 478: 476: 473: 471: 468: 466: 463: 461: 458: 456: 453: 451: 448: 446: 443: 441: 438: 436: 433: 431: 428: 426: 423: 421: 418: 416: 413: 411: 408: 406: 403: 401: 398: 396: 393: 391: 388: 386: 383: 381: 378: 376: 373: 371: 368: 366: 363: 361: 358: 356: 353: 351: 348: 346: 343: 341: 338: 337: 335: 332: 326: 322: 315: 310: 308: 303: 301: 296: 295: 292: 285: 282: 279: 276: 275: 267: 263: 259: 256: 253: 249: 245: 244: 225: 221: 215: 201:on 2016-03-04 197: 190: 184: 168: 161: 157: 147: 144: 142: 139: 137: 134: 133: 127: 126: 122: 118: 114: 110: 106: 100: 98: 94: 90: 86: 82: 78: 74: 70: 65: 64: 62: 57: 53: 49: 46: 42: 38: 34: 30: 26: 18: 807:Martian soil 434: 280:WRB homepage 227:. 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Retrieved 160: 101: 66: 59: 24: 23: 872:Terra rossa 867:Terra preta 847:Spodic soil 767:Duplex soil 747:Brown earth 727:Alkali soil 717:Rhizosphere 712:Laimosphere 586:(1974–1998) 543:Inceptisols 450:Plinthosols 415:Kastanozems 136:Pedogenesis 97:iron oxides 56:inceptisols 911:Categories 852:Stagnogley 802:Lunar soil 757:Dark earth 742:Brickearth 707:Pedosphere 677:Soil crust 485:Technosols 470:Solonchaks 390:Ferralsols 355:Anthrosols 229:2023-09-10 205:2014-06-14 152:References 109:Inceptisol 93:halloysite 837:Quicksand 782:Fill dirt 722:Bulk soil 568:Vertisols 558:Spodosols 548:Mollisols 538:Histosols 523:Aridisols 495:Vertisols 490:Umbrisols 480:Stagnosol 445:Planosols 440:Phaeozems 420:Leptosols 405:Gypsisols 395:Fluvisols 375:Chernozem 370:Cambisols 365:Calcisols 360:Arenosols 125:Lixisols. 89:kaolinite 41:structure 27:, in the 917:Pedology 822:Paleosol 737:Blue goo 692:Gypcrust 563:Ultisols 533:Gelisols 528:Entisols 518:Andisols 513:Alfisols 475:Solonetz 465:Retisols 460:Regosols 435:Nitisols 430:Luvisols 425:Lixisols 410:Histosol 400:Gleysols 385:Durisols 380:Cryosols 350:Andosols 340:Acrisols 141:Pedology 130:See also 121:Acrisols 81:Cameroon 69:Ethiopia 52:ultisols 48:alfisols 772:Eluvium 732:Bay mud 697:Caliche 687:Hardpan 682:Claypan 672:Subsoil 667:Topsoil 553:Oxisols 455:Podzols 345:Alisols 333:(1998–) 173:14 June 105:Alfisol 35:with a 25:Nitisol 882:Yedoma 817:Muskeg 264:  250:  58:of the 45:kandic 862:Takir 797:Loess 199:(PDF) 192:(PDF) 169:. FAO 73:Kenya 827:Peat 662:Loam 657:Clay 652:Silt 647:Sand 262:ISBN 248:ISBN 175:2014 123:and 107:and 95:and 87:and 79:and 54:and 37:clay 33:soil 812:Mud 117:FAO 113:U.S 913:: 257:). 222:. 91:, 75:, 71:, 50:, 313:e 306:t 299:v 254:( 232:. 208:. 177:. 63:.

Index


World Reference Base for Soil Resources
soil
clay
structure
kandic
alfisols
ultisols
inceptisols
USDA soil taxonomy
Ethiopia
Kenya
Democratic Republic of the Congo
Cameroon
basic parent rock
kaolinite
halloysite
iron oxides
Alfisol
Inceptisol
U.S
FAO
Acrisols
Lixisols.
Pedogenesis
Pedology
Soil classification
"Mineral Soils conditioned by a Wet (Sub)Tropical Climate"
"Major Soils of the World. ISRIC Wageningen, The Netherlands, 2001"
the original

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