Research on the River Branch Scheme of Qingshui Gully Flow Path of the Yellow River
Since 1976, the flow path of Qingshui Gully at the estuary of the Yellow River (YR) has been performing for 30 years, while it has already diverted to Qingbacha River for 10 years. It considers that the useful life for flow path of Qingshui Gully will continue for another 50-year, and suggests that the performing sequence for flow path of Qingshui Gully is as follows: Qingbacha River will divert to Beicha while flowing to the site, about 65km below Xihekou, and Beicha will then divert to the former channel while the corresponding flow level of 10,000m3/s discharge at Xihekou reaches 12m (Dagu Elevation, and the same as follows) during its flowing, and the former channel will again divert to Qingbacha River while the corresponding flow level of 10,000m3/s discharge at Xihekou reaches 12m during its flowing, and Qingbacha River will finally divert to the spare ocean flow path while the corresponding flow level of 10,000m3/s discharge at Xihekou reaches 12m during its flowing, all through making researches on such aspects as the feedback influence induced by deposition within lower channels, performance cost, effects of flood control and influence on the coastal dike safety of Gudong Oil Field, etc..
the Yellow River estuary flow path of Qingshui Gully Qingbacha Beicha, formal channel
Tang Meiying Chen Xiongbo Cui Meng Qian Yu
The Yellow River Engineering Consulting Company, Ltd. Zhengzhou, 450003, China
国际会议
山东东营
英文
348-354
2007-10-16（万方平台首次上网日期，不代表论文的发表时间）