Huang He: Ancient Floods and Recent Water Scarcity
Ancient Floods and Recent Water Scarcity
During the winter dry season the Huang He is slow-moving and silt-laden, and occupies only part of its huge bed; with the summer rains, it can become a raging torrent. Since the 2d cent.
The Chinese have long sought to control the Huang He by building dikes and overflow channels. Silt deposition, the principal cause of flooding, has elevated the riverbed; in places the river flows 60 to 70 ft (18–21 m) above the surrounding plains. During the summer high-water period, water pressure against the dikes can break through the retaining walls to cause devastating floods, which have led the Huang He to be called “China's Sorrow.” In 1955 the Chinese initiated a 50-year construction plan for control of the river. Dikes have been repaired
In recent years, however, extensive use of the river's waters has severely reduced the flow of the Huang He in its lower reaches, and its flow often fails to reach the sea. In 2000 the Chinese government embarked on the South-to-North Water Diversion Project to replenish the oversubscribed waters of the Huang He with those of the Chang (Yangtze); three sets of canals would divert water from the upper, middle, and lower Chang. The eastern route brings water from the lower Chang to the Huang He utilizing in part sections of the Grand Canal, and a central route connects the Han (a tributary of the Chang) to the Huang He. A third, western route, linking the headwaters of the Chang to those of the Huang He, is planned.
Sections in this article:
- Introduction
- Ancient Floods and Recent Water Scarcity
- Course
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