Huai River

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Huai River
Huai He
Huaihe Xingying Ferry.jpg
Huai River at Xingying Ferry, Funan County, Fuyang, Anhui.
Huairivermap.jpg
Map of the Huai River and its major tributaries.
Native name淮河
Location
Country China
Provinces Henan, Anhui, Jiangsu
Cities Xinyang, Fuyang, Lu'an, Huainan, Bengbu, Tianchang, Huai'an, Yangzhou
Physical characteristics
Length1,110 km (690 mi)
Basin size174,000 km2 (67,000 sq mi)
Discharge 
  average1,616 m3/s (57,100 cu ft/s) [1] Note, this is the main discharge into the Yangtze, 82.0% of the total water flow of all Huai waters.
Huai River
Chinese 淮河
Hanyu Pinyin Huái Hé
Postal Hwai Ho

The Huai River (Chinese : 淮河 ; pinyin :Huái Hé), formerly romanized as the Hwai, is a major river in China. It is located about midway between the Yellow River and Yangtze, [2] the two largest rivers in China, and like them runs from west to east. Historically draining directly into the Yellow Sea, floods have changed the course of the river such that it is now a major tributary of the Yangtze. The Huai is notoriously vulnerable to flooding.

Contents

The Huai River Qin Mountains line is sometimes regarded as the geographical dividing line between Northern and southern China. This line approximates the 0 °C January isotherm and the 800 mm isohyet in China.

The Huai River is 1,110 kilometres (690 mi) long with a drainage area of 174,000 square kilometres (67,000 sq mi). [2]

Course

The Wanfu Floodgate (Mo Fu Zha 
) near Yangzhou, Jiangsu, one of the major flood control projects in the area Wanfu Zha - CIMG3326.JPG
The Wanfu Floodgate (万福闸) near Yangzhou, Jiangsu, one of the major flood control projects in the area

The Huai River originates in Tongbai Mountain in Henan province. It flows through southern Henan, northern Anhui, and northern Jiangsu where it pools into Lake Hongze. Nowadays the Huai River then runs southwards as the Sanhe River by way of the Gaoyou Lake and Shaobo Lake emptying into Yangtze River at Sanjiangying (三江营) near Yangzhou. [3]

There is also a passage called the Huaihe Sea Entryway and Subei Irrigation Canal that passes Huai'an 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 GuanYun. [3]

In part to circumvent flooding, in Jiangsu province the Huai river system is interconnected with different waterways and thereby forms part of the Grand Canal. [2]

History

Historically, both the Huai River and Yellow River entered the Yellow Sea at Yunti Pass (modern day Yunti Village, in Huangwei Town of Xiangshui County) through a broad and level lower course. It was long used to irrigate the surrounding farmlands, and was the centre of an extensive network of canals and tributaries. [4]

A map of the Warring States around 350 BC, showing the former coastline and mouth of the Huai River Streitende-Reiche2.jpg
A map of the Warring States around 350 BC, showing the former coastline and mouth of the Huai River

Beginning in 1194, however, the Yellow River 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 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 Second World War, when the Nationalist government, in an attempt to check the pace of the Japanese 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. [2]

The result of these changes was that water from the Huai River pooled up into Lake Hongze, and then ran southwards towards the Yangtze River. Major and minor floods occurred frequently, with the area suffering droughts in between floods. In the 450 years to 1950, the Huai River saw, on average, 94 major floods per century.

Attempts to solve the Huai River's problems have focussed 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 North Jiangsu Main Irrigation Canal 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.

Tributaries

There are many tributaries of the Huai River. There are 15 main tributaries cover an area of more than 2000 km2 each, and 21 main tributaries have a catchment area larger than 1000 km2. [3]

The main tributaries on the Huai river (listed from upstream to downstream) are as follows: [5] [ circular reference ]

North bankSouth bank
Hong River (洪河) You River (游河)
Ying River (潁河) Shi River (浉河 [河流])
Xi Fei River (西淝河)Zhu Gan River (竹竿河)
Guo River (涡河) Zhai River (寨河)
Xin Bian River (新汴河)Huang River (潢河)
Kui Sui River (奎濉河)Bai Lu River (白露河)
Shi Guan River (白露河)
Pi He River (东淝河)
Dong Fei River (东淝河)
Chi River (池河 [淮河])

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1931 China floods

The 1931 China floods, or the 1931 Yangtze–Huai River floods, were a series of floods that occurred from June to August 1931 in the Republic of China, hitting major cities such as Wuhan, Nanjing and beyond, which eventually culminated into a dike breach along Lake Gaoyou on August 25, 1931.

Hongze Lake

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Ming Ancestors Mausoleum

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The North Jiangsu Main Irrigation Canal is located in the lower reaches of the Huai River, one of the major rivers in the north of Jiangsu Province, China. It originates at Gaoliangjian on Hongze Lake and runs through Hongze, Qingpu, Huai'an, Funing, Sheyang and Binghai county(or district) and joins the artificial estuary of Biandan Harbour. The canal is 168 km in length and can irrigate 1,720,000 hectares of farmland. The construction program was organized and directed by the headquarters of the Jiangsu Huai River management program between October 1951 and May 1952.

Hui River

Hui River, traditionally known as Huan River or Baohui River, was a major tributary of Huai River in northern China. Currently, it flows into the Huai-Hong New Canal , a constructed flood-control waterway connecting Huaiyuan and Hongze Lake. The starting point of Hui River is the ancient Honggou Canal (鸿沟), which has a great historical significance because it was the border between territories controlled by Liu Bang and Xiang Yu during the Chu-Han Contention. The river is mainly recharged by rainwater and groundwater. The river is heavily polluted by wastewater from nearby towns.

Qingjiangpu District District in Jiangsu, Peoples Republic of China

Qingjiangpu District is one of four districts of the prefecture-level city of Huai'an, Jiangsu Province, China. It was approved to establish on June 8, 2016. The district has an area of 420 km2 (160 sq mi) with a population of 735,900. The district of Qingjiangpu has 12 subdistricts and seven towns or townships under its jurisdiction, its seat is Chengnan Subdistrict.

1935 Yangtze flood

The 1935 Yangtze flood struck China during a decade of flooding, famine and social turmoil. It is considered to be the 5th deadliest flood in recorded history with a death toll of 145,000 and displacement of millions. As a result of the flood, millions of survivors were faced with many hardships. These problems ranged from displacement, injury, loss of property as well as food shortages and famine.

References

  1. "Main Rivers". National Conditions. China.org.cn. Archived from the original on March 13, 2012. Retrieved July 27, 2010.
  2. 1 2 3 4 "Huai River". Encyclopædia Britannica. 2014. Retrieved 31 October 2014.
  3. 1 2 3 Ma, Zhong. Evaluation of the Implementation of Water Pollution Prevention and Control Plans in China - The Case of Huai River Basin (PDF). School of Environment and Natural Resources Renmin University of China. Retrieved 10 October 2020./
  4. Elvin, Mark (2004). The Retreat of the Elephants: An Environmental History of China. Yale University Press. ISBN   9780300133530 . Retrieved 11 October 2020.
  5. "淮河". Wikipedia. Retrieved 10 October 2020.

Coordinates: 32°24′37″N115°24′14″E / 32.4103°N 115.404°E / 32.4103; 115.404