Suspended sediment load in the turbidity maximum zone at the Yangtze River Estuary: The trends and causes

Author:

Yang Yunping,Li Yitian,Sun Zhaohua,Fan Yongyang

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous)

Reference32 articles.

1. Blake A C, Kineke G C, Milligan T G et al., 2001. Sediment trapping and transport in the ACE Basin, South Carolina. Estuaries, 24(5): 721–733.

2. Chen Xiqing, Lv Xixi, Yan Yixin et al., 2008. Long-term changes and causes of the grain size bottom sediment at landward limit of the Yangtze Estuary. Resources and Environment in the Yangtze Basin, 17(4): 598–605.

3. Dai Shibao, Liu X X, Yang Shilun et al., 2008. A preliminary estimate of human and natural contributions to the decline in sediment flux from the Yangtze River to the China Sea. Quaternary International, 186: 43–54.

4. Dai Shibao, Yang Shilun, Li Ming, 2009. The sharp decrease in suspended sediment supply from China’s rivers to the sea: Anthropogenic and natural causes. Hydrological Sciences Journal, 54(1): 134–146.

5. Dai Zhijun, Han Zhen, Yun Caixing, 2005. Grainsized characteristics and transport trends of the sediment in the south channel of the Yangtze River. Transaction of Oceanology and Limnology, (2): 72–77. (in Chinese)

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