Ji Canal River

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The Ji Canal River or Jiyunhe (Chinese :蓟运河; literally: "Ji Canal") is a semi-artificial river in North China Plain near the major city of Tianjin. It is an important part of Hai River watershed system. The total length of Jiyunhe as of today is about 145 km and it drains into the Bohai Sea near Tanggu. Jiyunhe was originally a natural river (named Baoqiu River before Sui and Tang dynasties and Chao River before Ming dynasty) derived from a mountain called Baoqiu north of the Great Wall near Zunhua. The original length of this river was over 310 km. The section south of the Great Wall was artificially widened by Cao Cao during the Han dynasty so that it became navigable and thus it could be used to supply the frontline in the northeast. The upstream section of the river was gradually abandoned. In Ming dynasty, the channel was artificially broadened again to make it navigable to bigger ships. Since then, it became a supply line of Tianjin. Grains were shipped to Tianjin and nearby towns on this river, so it got a nickname of Grain River and was finally renamed as Jiyunhe which literally means Canal of Ji. [1]

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North China Plain plain

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Tianjin Municipality in Peoples Republic of China

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Du Ji, courtesy name Bohou, was an official who lived in the late Eastern Han dynasty of China. He later served as a high-ranking official in the state of Cao Wei during the Three Kingdoms period. He had the reputation of being a model governor, valiant, loyal and wise. He was the grandfather of Du Yu, the author of the most influential Zuo Zhuan commentary, who gave the work its modern form.

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The Ming Great Wall, built by the Ming dynasty (1368–1644), forms the most visible parts of the Great Wall of China today. A comprehensive archaeological survey, using advanced technologies, has concluded that the Ming walls measure 8,850 km (5,500 mi) from Jiayu Pass in the west to the sea in Shanhai Pass, then looping over to terminate in Manchuria at the Hushan Great Wall. This is made up of 6,259 km (3,889 mi) sections of actual wall, 359 km (223 mi) of trenches and 2,232 km (1,387 mi) of natural defensive barriers such as hills and rivers.

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The Ju River in North China Plain is a major river in the Beijing and Tianjin vicinities. It is a part of Hai River's watershed system. In 354 BCE, State of Yan defeated State of Qi in a battle by this river. In Han dynasty, the original channel of Ju River was widened by Emperor Xian so that it became a navigable river and a major military supply line to the northeast frontier. The total length of Ju River is 206 km, 66 of them are in the Pinggu District of Beijing. Before paved roads were constructed in 1930s, this river was the only transportation route to and from the remote Pinggu region. The river was polluted by industrial wastewater in 1990s. The water quality has been improved in recent years and it has become a water resource for the Pinggu region.

Ziya River river in the Peoples Republic of China

The Ziya River is one of the five major tributaries of Hai River system in northern China. The total length of Ziya River is 730 km (450 mi) and the size of its drainage basin is 78,700 square kilometers (30,400 sq mi). The discharge rate of Ziya River is about 1 m3/s.

References

  1. Zhang, Zhidong. Historical record of Shuntian Fu in Reign of Guanxu Emperor (in Chinese).