Knowledge (XXG)

Baiyang River

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metre (3 ft) deep; by the 1990s, it had virtually dried up. Since the opening of the Irtysh–Karamay Canal in August 2000, the Ailik lake, which had been almost dry, has been able to recover as a deep lake with plenty of fish; now it occupies 50 square kilometres (19 sq mi) and is up to 7 metres (23 ft) deep.
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Due to the construction of the Baiyang River Reservoir and the Huangyangquan Reservoir (see below) and the concomitant diversion of the Baiyang River waters, the Ailik Lake started shrinking in the 1980s; by the mid 1980s, it was just 15 square kilometres (5.8 sq mi) in size and hardly 1
516:
Meng, Jiangli (孟江丽) (2013), "西北干旱区水资源利用与生态环境响应研究———以新疆白杨河流域为例 (A study of the use of water resources of the arid regions of the Northwest and its effect on the environment -- on the example of the Baiyang River basin in Xinjiang)",
338:
For over 20 kilometres (12 mi) downstream from the Baiyang River Reservoir to the Ailik Lake, the natural river bed of the Baiyang River is paralleled by an artificial, concrete-lined canal, which leaves the reservoir at
326:), whose water surface is (as of 1999) at about 270 metres (890 ft) above sea level. Potentially, water can seep through the same fault even farther to the southwest, to the dry Alan Nur lake (the former terminus of the 230:), thus improving the water supply situation in Urho District and a revitalizing the riverside wetlands. The Baiyang River canyon in the western part of Urho District is considered a scenic site. 199:, upstream of Urho District's main urban area. A provision has been made for letting about 1/3 of the water flow from the canal into the Baiyang River, ( 85:. The river's total length is estimated at 170 kilometres (110 mi), and the average annual flow at 109 million cubic metres (88,000  439: 404: 373: 298: 248: 129: 342: 202: 171: 287:
While there is no further surface water flow out of the Ailik Lake, some water from this lake is believed to seasonally seep through
112: 70: 52: 24: 604: 234: 157:; the dam creates the Baiyang River Reservoir (白杨河水库) with an area of 5.8 square kilometres (2.2 sq mi). 567: 161: 483:) carry names meaning "Poplar River" in Chinese or in a Turkic language. This includes the Baiyang River of 165: 433: 93: 276:). As of 1999, the lake's water surface elevation was 273 to 276 metres (896 to 906 ft) above 123:
Counties in the west. It crosses Urho District of Karamay City, and then re-enters Hoboksar County.
543:艾里克湖消失10年后复活] (Ten years after its disappearance, the vanished Ailik Lake has come back to life 288: 74: 579: 108: 47:'White Poplar River'), also known under a Mongolian name transcribed in Chinese as 292: 492: 97: 541: 598: 496: 484: 78: 327: 82: 584: 242: 120: 116: 89:). The river's basin occupies 16,400 square kilometres (6,300 sq mi), 476: 238: 101: 454: 441: 419: 406: 388: 375: 357: 344: 313: 300: 263: 250: 217: 204: 186: 173: 144: 131: 488: 277: 105: 86: 568:"Tectonic geomorphological characteristics for evolution of the Manas Lake" 480: 60: 32: 92:
The Baiyang River starts in a massif near the junction of the
401:, passes through the Huangyangquan Reservoir (黄羊泉水库, dam at 104:. It flows in a general southeastern direction, toward the 499:
in Kazakhstan or Kazakh-speaking sections of Xinjiang.
111:. Along much of its length it forms the border between 16:
River in Xinjiang Uighur Autonomous Region of China
475:Numerous watercourses in Central Asia (including 100:mountain ranges, near Xinjiang's border with 8: 42: 583: 295:into the nearby Small Ailik Lake (小艾里克湖, 73:of China. It flows through the region's 536: 534: 532: 508: 561: 559: 557: 555: 553: 370:, crosses the Irtysh–Karamay Canal at 432:), and ends in what appears to be an 7: 519:水资源保护 - Water resources protection 14: 566:Yao, Yonghui; Li, Huiguo (2010), 113:Hoboksar Mongol Autonomous County 71:Xinjiang Uighur Autonomous Region 164:crosses the Baiyang River on an 126:The Baiyang River is dammed at 65: 56: 37: 28: 1: 585:10.3724/SP.J.1227.2010.00167 487:, which flows from the main 621: 241:. The river forms a small 237:and ends in the endorheic 245:as it enters the lake ( 495:, as well as several 455:46.03333°N 85.60000°E 420:46.06472°N 85.58028°E 389:46.11944°N 85.41667°E 358:46.13833°N 85.37222°E 314:45.75972°N 85.57028°E 264:45.96667°N 85.78333°E 233:The river enters the 218:46.12917°N 85.42778°E 187:46.12917°N 85.42639°E 145:46.14306°N 85.37639°E 572:Journal of Arid Land 334:A distributary canal 235:Gurbantünggüt Desert 162:Irtysh–Karamay Canal 451: /  416: /  385: /  354: /  310: /  260: /  214: /  183: /  141: /  605:Rivers of Xinjiang 460:46.03333; 85.60000 425:46.06472; 85.58028 394:46.11944; 85.41667 363:46.13833; 85.37222 319:45.75972; 85.57028 269:45.96667; 85.78333 223:46.12917; 85.42778 192:46.12917; 85.42639 150:46.14306; 85.37639 75:Tacheng Prefecture 69:), is a river in 45: 612: 589: 588: 587: 563: 548: 547: 538: 527: 526: 513: 466: 465: 463: 462: 461: 456: 452: 449: 448: 447: 444: 431: 430: 428: 427: 426: 421: 417: 414: 413: 412: 409: 400: 399: 397: 396: 395: 390: 386: 383: 382: 381: 378: 369: 368: 366: 365: 364: 359: 355: 352: 351: 350: 347: 325: 324: 322: 321: 320: 315: 311: 308: 307: 306: 303: 289:ground fractures 275: 274: 272: 271: 270: 265: 261: 258: 257: 256: 253: 229: 228: 226: 225: 224: 219: 215: 212: 211: 210: 207: 198: 197: 195: 194: 193: 188: 184: 181: 180: 179: 176: 156: 155: 153: 152: 151: 146: 142: 139: 138: 137: 134: 115:in the east and 109:Dzungarian Basin 67: 58: 46: 43: 39: 30: 620: 619: 615: 614: 613: 611: 610: 609: 595: 594: 593: 592: 565: 564: 551: 540: 539: 530: 515: 514: 510: 505: 473: 459: 457: 453: 450: 445: 442: 440: 438: 437: 424: 422: 418: 415: 410: 407: 405: 403: 402: 393: 391: 387: 384: 379: 376: 374: 372: 371: 362: 360: 356: 353: 348: 345: 343: 341: 340: 336: 318: 316: 312: 309: 304: 301: 299: 297: 296: 268: 266: 262: 259: 254: 251: 249: 247: 246: 222: 220: 216: 213: 208: 205: 203: 201: 200: 191: 189: 185: 182: 177: 174: 172: 170: 169: 149: 147: 143: 140: 135: 132: 130: 128: 127: 17: 12: 11: 5: 618: 616: 608: 607: 597: 596: 591: 590: 578:(3): 167−173, 549: 528: 507: 506: 504: 501: 497:Terekty Rivers 493:Lake Aydingkol 472: 469: 335: 332: 15: 13: 10: 9: 6: 4: 3: 2: 617: 606: 603: 602: 600: 586: 581: 577: 573: 569: 562: 560: 558: 556: 554: 550: 545: 544: 537: 535: 533: 529: 524: 520: 512: 509: 502: 500: 498: 494: 491:range toward 490: 486: 485:Toksun County 482: 478: 470: 468: 464: 435: 429: 398: 367: 333: 331: 329: 323: 294: 290: 285: 281: 279: 273: 244: 240: 236: 231: 227: 196: 167: 163: 158: 154: 124: 122: 118: 114: 110: 107: 103: 99: 95: 90: 88: 84: 80: 79:Urho District 76: 72: 68: 66:Nàmùguōlēi hé 62: 54: 50: 40: 34: 26: 22: 21:Baiyang River 575: 571: 546:, 2003-06-02 542: 522: 518: 511: 474: 436:facility at 337: 291:of the Kewu 286: 282: 232: 159: 125: 91: 83:Karamay City 64: 48: 36: 20: 18: 458: / 434:aquaculture 423: / 392: / 361: / 328:Manas River 317: / 267: / 221: / 190: / 148: / 525:(2): 38–42 477:Kazakhstan 471:Other uses 446:85°36′00″E 443:46°02′00″N 411:85°34′49″E 408:46°03′53″N 380:85°25′00″E 377:46°07′10″N 349:85°22′20″E 305:85°34′13″E 302:45°45′35″N 255:85°47′00″E 252:45°58′00″N 239:Ailik Lake 209:85°25′40″E 178:85°25′35″E 136:85°22′35″E 133:46°08′35″N 102:Kazakhstan 94:Tarbagatai 49:Namuguolei 38:Báiyáng hé 489:Tian Shan 346:46°8′18″N 278:sea level 206:46°7′45″N 175:46°7′45″N 106:endorheic 599:Category 481:Xinjiang 166:aqueduct 77:and the 87:acre⋅ft 53:Chinese 25:Chinese 63:: 61:pinyin 55:: 35:: 33:pinyin 27:: 503:Notes 293:Fault 243:delta 57:纳木郭勒河 479:and 160:The 121:Toli 119:and 117:Emin 98:Saur 96:and 44:lit. 19:The 580:doi 330:). 280:. 168:at 81:of 29:白杨河 601:: 574:, 570:, 552:^ 531:^ 523:29 521:, 467:. 59:; 41:; 31:; 582:: 576:2 51:( 23:(

Index

Chinese
pinyin
Chinese
pinyin
Xinjiang Uighur Autonomous Region
Tacheng Prefecture
Urho District
Karamay City
acre⋅ft
Tarbagatai
Saur
Kazakhstan
endorheic
Dzungarian Basin
Hoboksar Mongol Autonomous County
Emin
Toli
46°08′35″N 85°22′35″E / 46.14306°N 85.37639°E / 46.14306; 85.37639
Irtysh–Karamay Canal
aqueduct
46°7′45″N 85°25′35″E / 46.12917°N 85.42639°E / 46.12917; 85.42639
46°7′45″N 85°25′40″E / 46.12917°N 85.42778°E / 46.12917; 85.42778
Gurbantünggüt Desert
Ailik Lake
delta
45°58′00″N 85°47′00″E / 45.96667°N 85.78333°E / 45.96667; 85.78333
sea level
ground fractures
Fault
45°45′35″N 85°34′13″E / 45.75972°N 85.57028°E / 45.75972; 85.57028

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