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Kherlen River

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It has been noted that Shar Burdiin lake shows the maximum concentration in uranium (with, only a short distance away, Gurvany-2 lake not far behind in uranium concentration); and that said concentration decreases while the distance from that area increases, as seen from Tsaidam-2 lake and Gurvany-1
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Several of these lakes are exceedingly rich in uranium; in one location of the Shar Burdiin lake, uranium concentration has been measured at 62.5 μM, which may be the highest reported naturally occurring U concentration in a surface water body. Shar Burdiin is also the most highly evaporated lake.
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recharged by rainfall and snowmelt, and from precipitation in the highlands north of the lakes. But the local climate is semi-arid, with only 207 mm mean annual precipitation distributed unequally throughout the year. This means that groundwater recharge is relatively rare: only the largest
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The Kherlen River is the regional discharge point and also represents a hydrogeological divide for the shallow unconfined aquifer, as groundwater flows south along the topographic gradient. The lakes in their shallow closed basins act as evaporative discharge points.
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The Khuduu Aral, a 30 kilometre long and 20 km wide plain on the Kherlen river, is home to Genghis Khan’s Ikh Aurag (palace). Nearby it there is a small lake that is high in carbonate, soda, and chlorine. Its water has a reputation for treating nerve disorders.
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lake which are over 15 km from Shar Burdiin Lake. So another possibility for the contamination is that of wind-blown salts from Shar Burdiin lake and Gurvany-2 lake, reaching the lakes and groundwaters in other parts of the area.
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of volcanic glass is a potential source of uranium in the region’s groundwater and soda lakes. Contamination may also result from large dust storms, which are frequent during the spring when the soda lakes are driest.
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In the new tectonic division of Mongolia, the Kerulen block is the new name for what used to be called the Ereendavaa block. It extends eastward into Russia and northeast China and connects with the Erguna
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These uranium-rich mineral deposits, 100 km north of the lakes, were mined during the 1970s when Mongolia was aligned with the USSR. Several of the old mines were reopened during the years 2000.
758:"Late Triassic initial closure of the Mongol-Okhotsk Ocean in the western segment: Constraints from sedimentological, detrital zircon ages and paleomagnetic evidence" 477:; among these lakes are the Tsaidam lakes, the Gurvany lakes and the Shar Burdiin lake. The groundwater that feeds the soda lakes comes from a shallow unconfined 952: 720: 1297: 493:
No uranium deposits have been identified within their catchment area. However, approximately 100 km north of the lakes, there are several deposits of
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Orkhonselenge, Alexander; Bulgan, Odmaa (2021). "Geochemical studies and lacustrine geomorphology of Lake Yakhi basin in eastern Mongolia".
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The mean streamflow of Kherlen River has decreased by more than a half from 2000 to 2008 when compared with prior decades.
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Zhao, Pan; Jia, Zhenhua; Xu, Bei; Xu, Yan; Sukhbaatar, Turbold; Appel, Erwin; Chen, Yan (August 2023).
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In central Mongolia, a soda lake was found in 2008 to also have high amounts of uranium in its salts.
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Linhoff, Benjamin S.; Bennett, Philip C.; Puntsag, Tamir; Gerel, Ochir (March 2011).
672: 633: 442: 360: 320: 183: 961:, p. 13, "Discussion" > "Source for uranium in soda lakes and groundwaters". 1796: 1736: 1147: 772: 732: 701: 664: 619: 466: 458: 347: 278: 126: 663:. Geography of the Physical Environment. Cham: Springer International Publishing. 567:(WHO) provisional guideline value for uranium is 0.063 μM L (15 μg L). or ~15,000 1786: 1776: 1658: 1312: 705: 510: 446: 324: 179: 130: 1931: 1926: 1888: 1831: 1801: 1699: 1629: 1579: 1422: 1073: 140: 904: 736: 668: 1946: 1878: 1761: 1609: 1574: 1540: 1471: 1402: 1266: 1256: 1184: 1125: 1120: 1088: 776: 470: 385: 372: 228: 215: 971: 1883: 1806: 1756: 1668: 1496: 1432: 1427: 1324: 1317: 1283: 1271: 1261: 1226: 1083: 1078: 624: 433:
Kherlen-Ergune-Amur has a total length of 5,052 kilometres or 3,139 miles.
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after about 30 kilometres or 19 miles. The Ergune marks the border between
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precipitation events and snowmelt periods result in significant recharge.
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From there the Kherlen flows in a mostly eastern direction through the
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and China for about 944 kilometres or 587 miles, until it meets the
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may overflow at its northern shore, and the water will meet the
48: 1911: 1791: 1771: 1751: 1491: 1063: 454: 422: 286: 700:(3): 231-242 (see section 5.2. "Changes in lake area", § 33). 1036: 436: 1462: 994: 958: 946: 934: 922: 910: 898: 886: 874: 862: 850: 830: 815: 800: 718: 618:(6). London: Taylor & Francis Informa Ltd: 1221–1229. 449:(far Northeast Mongolia), the Kherlen river feeds several 343:) basins and is consequently named “Three River Basins”. 949:, p. 10, "Discussion" > "Groundwater evolution". 818:, p. 4, "Introduction" > "Uranium geochemistry". 413:
In years with high precipitation, the normally exitless
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Centre for Russian and Central EurAsian Mineral Studies
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Brutsaert, Wilfried; Sugita, Michiaki (December 2008).
335:. This area constitutes the divide between the Arctic ( 833:, p. 10, "Discussion" > "Evolution of lakes". 803:, p. 3, "Introduction" > "Regional geology". 691: 331:, about 180 kilometres or 112 miles northeast of 1944: 319:The river originates in the south slopes of the 605: 85: 925:, p. 6, "Results" > "Water chemistry". 1019: 36: 755: 601: 599: 597: 402:after another 164 kilometres or 102 miles. 1026: 1012: 843:Mironov, Y (2006). "Uranium of Mongolia". 437:Soda lakes, uranium and associated geology 62: 853:, "Introduction" > "Regional geology". 623: 594: 842: 836: 14: 1945: 656: 408: 1007: 652: 650: 329:Khan Khentii Strictly Protected Area 1917:North Jiangsu Main Irrigation Canal 24: 660:The Physical Geography of Mongolia 25: 1969: 647: 1035: 657:Yembuu, Batchuluun, ed. (2021). 47: 964: 574: 557: 473:volcanic chain during the late 749: 712: 685: 547: 291: 207: • coordinates 13: 1: 997:, p. 13, "Implications". 731:(1): 171-183 (see Abstract). 612:Hydrological Sciences Journal 587: 157:Physical characteristics 1958:International rivers of Asia 725:Environmental Earth Sciences 706:10.4000/geomorphologie.15873 7: 528: 248:1,254 km (779 mi) 175: • location 27:River in China and Mongolia 10: 1974: 535:List of rivers of Mongolia 115:People's Republic of China 1897: 1682: 1638: 1564: 1520: 1461: 1377: 1282: 1048: 865:, p. 5-6, "Results". 737:10.1007/s12665-010-0512-8 669:10.1007/978-3-030-61434-8 565:World Health Organization 314: 282: 274: 252: 244: 205: 193: 189: 173: 165: 161: 156: 146: 136: 120: 106: 101: 86: 81: 70: 61: 46: 37: 32: 777:10.1016/j.gr.2023.08.007 540: 339:) and Pacific (Kherlen, 1922:Eastern Zhejiang Canal 625:10.1623/hysj.53.6.1221 77:: kherlen, "hederated" 1042:Major rivers of China 913:, p. 7, table 4. 995:Linhoff et al. 2011 959:Linhoff et al. 2011 947:Linhoff et al. 2011 935:Linhoff et al. 2011 923:Linhoff et al. 2011 911:Linhoff et al. 2011 899:Linhoff et al. 2011 887:Linhoff et al. 2011 875:Linhoff et al. 2011 863:Linhoff et al. 2011 851:Linhoff et al. 2011 831:Linhoff et al. 2011 816:Linhoff et al. 2011 801:Linhoff et al. 2011 501:assemblages within 409:Kherlen-Ergune-Amur 382: /  225: /  1953:Rivers of Mongolia 1683:Other major rivers 398:and emptying into 386:48.050°N 115.600°E 229:48.733°N 117.083°E 147:Chinese Prefecture 1940: 1939: 765:Gondwana Research 678:978-3-030-61433-1 465:erupted from the 441:Near the city of 321:Khentii mountains 256: 255: 184:Khentii Mountains 16:(Redirected from 1965: 1104:Qingyi (Sichuan) 1040: 1039: 1028: 1021: 1014: 1005: 1004: 998: 992: 986: 985: 983: 982: 976:mongolian.travel 968: 962: 956: 950: 944: 938: 932: 926: 920: 914: 908: 902: 896: 890: 884: 878: 872: 866: 860: 854: 848: 840: 834: 828: 819: 813: 804: 798: 787: 786: 784: 783: 762: 753: 747: 746: 744: 743: 716: 710: 709: 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Retrieved 975: 966: 954: 942: 930: 918: 906: 894: 882: 870: 858: 844: 838: 780:. Retrieved 768: 764: 751: 740:. Retrieved 728: 724: 714: 697: 693: 687: 659: 637:. Retrieved 615: 611: 576: 559: 549: 524: 520: 516: 492: 488: 484: 440: 419:Ergune River 412: 404: 351: 345: 318: 309:Orkhon River 290: 266: 262: 258: 257: 41:(Kèlǔlún hé) 1907:Grand Canal 1767:Lion Spring 1477:2nd Songhua 1352:Luo (Henan) 459:pyroclastic 389: / 363:, entering 333:Ulaanbaatar 323:, near the 232: / 82:Native name 1947:Categories 1205:Qi (Hunan) 981:2024-07-25 782:2024-07-25 742:2024-07-18 639:19 January 588:References 507:sandstones 475:Cretaceous 467:Choibalsan 451:soda lakes 443:Choibalsan 427:Amur River 415:Hulun Lake 400:Hulun Nuur 361:Choibalsan 357:Ulaan Ereg 337:Tuul River 292:Kèlǔlún hé 275:Хэрлэн гол 200:Hulun Nuur 87:Хэрлэн гол 55:Ondorkhaan 1787:Subansiri 1747:Longjiang 1659:Xar Moron 1313:Huangshui 849:Cited in 847:. London. 634:128674944 499:coffinite 495:uraninite 299:river in 271:Mongolian 151:Hulunbuir 94:Mongolian 75:Mongolian 71:Etymology 1932:Zhengguo 1927:Red Flag 1889:Xiaoqing 1802:Qiantang 1742:Minjiang 1700:Karatash 1580:Yongding 1423:Hongshui 1148:Qingshui 1074:Tongtian 771:(1): 9. 529:See also 463:rhyolite 377:115°36′E 301:Mongolia 111:Mongolia 102:Location 1879:Wanquan 1762:Nujiang 1752:Lancang 1630:Jiyunhe 1610:Sanggan 1575:Chaobai 1541:Shiguan 1502:Kherlen 1472:Songhua 1403:Yujiang 1267:Huangpu 1257:Qinhuai 1185:Chishui 1155:Hanshui 1126:Bailong 1121:Jialing 1089:Baishui 1050:Yangtze 479:aquifer 445:in the 348:Khentii 295:) is a 279:Chinese 267:Kerülen 220:117°5′E 217:48°44′N 127:Khentii 107:Country 18:Kherlen 1912:Lingqu 1884:Taping 1807:Puyang 1797:Suifen 1792:Irtysh 1757:Beilun 1664:Xinkai 1642:system 1615:Fuyang 1595:Daqing 1568:system 1524:system 1492:Ussuri 1465:system 1433:Beipan 1428:Nanpan 1381:system 1325:Wuding 1318:Datong 1293:Kariqu 1286:system 1284:Yellow 1262:Xitiao 1227:Lishui 1084:Yalong 1079:Jinsha 1069:Chumar 1064:Dangqu 1059:Tuotuo 1052:system 675:  632:  554:Block. 455:basalt 431:system 429:. The 423:Russia 374:48°3′N 315:Course 289:: 287:pinyin 281:: 245:Length 169:  166:Source 131:Dornod 90:  1874:Nandu 1847:Mulan 1832:Cao'e 1782:Nyang 1722:Tumen 1710:Shule 1690:Tarim 1654:Taizi 1600:Wenyu 1585:Hutuo 1512:Huifa 1507:Woken 1497:Argun 1487:Mudan 1388:North 1379:Pearl 1367:Dawen 1362:Muwen 1303:Daxia 1232:Miluo 1190:Xiang 761:(PDF) 630:S2CID 541:Notes 365:China 352:aimag 305:China 195:Mouth 53:Near 1867:Ting 1732:Luan 1727:Yalu 1715:Dang 1695:Ejin 1640:Liao 1605:Juma 1590:Ziya 1556:Hong 1546:Quan 1536:Ying 1522:Huai 1438:Rong 1418:Qian 1408:Yong 1398:West 1393:East 1340:Jing 1222:Yuan 1195:Xiao 1180:Qing 1160:Muma 1099:Dadu 673:ISBN 641:2015 563:The 505:and 471:Onon 359:and 341:Onon 303:and 283:克鲁伦河 263:Kern 38:克鲁伦河 1862:Mei 1827:Shu 1817:Dai 1737:Red 1705:Ili 1649:Hun 1620:Wei 1566:Hai 1551:Hui 1531:Guo 1482:Nen 1453:Liu 1448:Gui 1413:Xun 1357:Qin 1335:Wei 1330:Fen 1308:Tao 1247:Xin 1237:Gan 1200:Lei 1175:Bao 1165:Chi 1111:Tuo 1094:Min 773:doi 769:125 733:doi 702:doi 665:doi 620:doi 569:ppb 367:at 265:or 1949:: 1842:Ou 1822:Si 1625:Ju 1217:Zi 1210:Mi 1170:Du 1143:Wu 1136:Qu 974:. 823:^ 808:^ 791:^ 767:. 763:. 729:62 727:. 723:. 698:27 696:. 671:. 649:^ 628:. 616:53 614:. 610:. 596:^ 509:. 457:, 311:. 285:; 277:; 273:: 269:; 182:, 129:, 113:, 1027:e 1020:t 1013:v 984:. 785:. 775:: 745:. 735:: 708:. 704:: 681:. 667:: 643:. 622:: 571:U 469:– 96:) 92:( 20:)

Index

Kherlen

Ondorkhaan

Mongolian
Mongolian
Mongolia
People's Republic of China
Mongolian Aimags
Khentii
Dornod
Inner Mongolia
Hulunbuir
Burkhan Khaldun
Khentii Mountains
Mouth
Hulun Nuur
48°44′N 117°5′E / 48.733°N 117.083°E / 48.733; 117.083
Mongolian
Chinese
pinyin
1,254 km
Mongolia
China
Orkhon River
Khentii mountains
Burkhan Khaldun
Khan Khentii Strictly Protected Area
Ulaanbaatar
Tuul River

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