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Huai River

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to the north repeatedly changed its course southwards to run into the Huai River. The resulting silting was so heavy that after the Yellow River changed back to its northerly course for the most recent time in 1897, the geography of the Huai River basin was changed significantly by the creation of
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new high lands, lakes, and the built-up silt of the Yellow River's historical southern course. As a result, water from the midsection of the river could not easily flow into the lower section, while water in the lower section could not find an outlet to the sea. The problem worsened in the
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There are many tributaries of the Huai River. There are 15 main tributaries cover an area of more than 2,000 square kilometers (770 sq mi) each, and 21 main tributaries have a catchment area larger than 1,000 square kilometers (390 sq mi).
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and empties into the sea at Biandan Port. A separate course runs north by way of the Huaimu River and Huai Shu River and connects the Huai River system with the Xinyi River (part of the Yishusi River system) which exits into the sea at
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Attempts to solve the Huai River's problems have focused on building outlets for the Huai River into the Yangtze River and the sea. Currently, the major part of the river's flow enters the Yangtze River via Lake Hongze. The
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invasion, flooded the lower Huai basin by opening the Yellow River's southern levee. The main stem of the Yellow River flowed through the levee breach for the next nine years, further disrupting the Huai river system.
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also diverts some of its water along its old historical course to the sea, and is planned to be upgraded with a new parallel channel. Several former tributaries also carry some water to the sea.
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1,616 m/s (57,100 cu ft/s) Note, this is the main discharge into the Yangtze, 82.0% of the total water flow of all Huai waters.
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such that it now primarily discharges into the Yangtze. The Huai River is, to this day, notoriously vulnerable to flooding.
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Evaluation of the Implementation of Water Pollution Prevention and Control Plans in China - The Case of Huai River Basin
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province the Huai River system is interconnected with different waterways and thereby forms part of the
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Pictorial map showing the Huai Basin between the Yangtze (top) and Yellow (bottom) rivers, 1736.
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The main tributaries on the Huai River (listed from upstream to downstream) are as follows:
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of 174,000 km (67,000 sq mi). It is located about midway between the
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The result of these changes was that water from the Huai River pooled up into
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The Retreat of the Elephants: An Environmental History of China
42: 556:, emptying into the Yangtze River at Sanjiangying (三江营) near 516:. This line approximates the 0 °C (32 °F) January 755: 741: 727: 713: 699: 30:"Huai" redirects here. For the Xia Dynasty king, see 2022: 1807: 1763: 1689: 1645: 1586: 1502: 1407: 1173: 789:government, in an attempt to check the pace of the 749: 735: 721: 707: 693: 686: 681: 667: 653: 633: 624: 434: 429: 415: 407: 395: 387: 377: 338: 328: 316: 302: 263: 250: 242: 233: 195: 175: 165: 160: 144: 107: 532:The Huai River originates in Tongbai Mountain in 477:, about 1,110 km (690 mi) long with a 139:Map of the Huai River and its major tributaries. 615:(modern day Yunti Village, in Huangwei Town of 1144: 639: 150: 8: 977: 975: 973: 971: 536:. It flows through southern Henan, northern 1151: 1137: 1129: 678: 1008: 1006: 1004: 607:Historically, the Huai River entered the 93:Learn how and when to remove this message 831: 816: 399:174,000 km (67,000 sq mi) 56:This article includes a list of general 937: 567:and Subei Irrigation Canal that passes 1042: 1032: 757: 621: 104: 520:and the 800 millimeters (30 in) 7: 2042:North Jiangsu Main Irrigation Canal 956:from the original on March 13, 2012 807:North Jiangsu Main Irrigation Canal 583:In part to circumvent flooding, in 563:There is also a passage called the 508:, formed by the Huai River and the 62:it lacks sufficient corresponding 25: 2098:Tributaries of the Yangtze River 1160: 776:Beginning in 1194, however, the 133: 117: 47: 499:changed the course of the river 756: 742: 728: 714: 700: 640: 340: • coordinates 265: • coordinates 1: 234:Physical characteristics 379: • elevation 308:1,029 m (3,376 ft) 304: • elevation 514:northern and southern China 391:1,110 km (690 mi) 330: • location 252: • location 2114: 417: • average 123:Huai River in the city of 36: 29: 1067:. Yale University Press. 821:The Bengbu Railway Bridge 770: 715:ㄏㄨㄞˊ   ㄏㄜˊ 677: 663: 649: 629: 448: 425: 403: 312: 238: 151: 132: 116: 987:Encyclopædia Britannica 77:more precise citations. 2047:Eastern Zhejiang Canal 822: 604: 27:River in Central China 1167:Major rivers of China 918:Dong Fei River (东淝河) 820: 602: 1061:Elvin, Mark (2004). 883:Xin Bian River (新汴河) 868:Zhu Gan River (竹竿河) 544:where it pools into 383:0 m (0 ft) 362:32.3078°N 119.7035°E 287:32.3810°N 113.2763°E 950:National Conditions 894:Bai Lu River (白露河) 891:Kui Sui River (奎濉河) 833: 565:Huaihe Sea Entryway 506:Qinling–Huaihe Line 430:Basin features 358: /  283: /  1808:Other major rivers 865:Xi Fei River (西淝河) 832: 823: 605: 2083:Rivers of Jiangsu 2065: 2064: 929: 928: 886:Huang River (潢河) 774: 773: 766: 765: 688:Standard Mandarin 452: 451: 367:32.3078; 119.7035 334:Yangzhou, Jiangsu 292:32.3810; 113.2763 103: 102: 95: 39:2016 China floods 16:(Redirected from 2105: 1229:Qingyi (Sichuan) 1165: 1164: 1153: 1146: 1139: 1130: 1111: 1110: 1108: 1106: 1092: 1086: 1085: 1083: 1081: 1058: 1052: 1050: 1044: 1040: 1038: 1030: 1028: 1026: 1021: 1010: 999: 998: 996: 994: 979: 966: 965: 963: 961: 952:. 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Index

Huaihe River
Huai of Xia
2016 China floods
references
inline citations
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introducing
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Bengbu

China
Provinces
Henan
Anhui
Jiangsu
Xinyang
Fuyang
Lu'an
Huainan
Bengbu
Tianchang
Huai'an
Yangzhou
Nanyang
32°22′52″N 113°16′35″E / 32.3810°N 113.2763°E / 32.3810; 113.2763
Mouth
Yangtze
32°18′28″N 119°42′13″E / 32.3078°N 119.7035°E / 32.3078; 119.7035
Yangtze

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