ACTUAL FLUX OF THE HUANGHE (YELLOW-RIVER) SEDIMENT TO THE WESTERN PACIFIC-OCEAN

被引：141

作者：

MARTIN, JM

ZHANG, J

SHI, MC

ZHOU, Q

机构：

[1] OCEAN UNIV QINGDAO,DEPT MARINE CHEM,QINGDAO 266003,PEOPLES R CHINA

[2] OCEAN UNIV QINGDAO,DEPT PHYS OCEANOG,QINGDAO 266003,PEOPLES R CHINA

[3] SOC,N CHINA SEA MONITORING CTR,QINGDAO 266033,PEOPLES R CHINA

来源：

NETHERLANDS JOURNAL OF SEA RESEARCH | 1993年 / 31卷 / 03期

关键词：

D O I：

10.1016/0077-7579(93)90025-N

中图分类号：

Q17 [水生生物学];

学科分类号：

071004 ;

摘要：

More than 90% of the Huanghe sediment load is deposited in the lower reaches of the river and within the shallow estuarine area. Additional sedimentation occurs in the southern part of Bohai so that the actual flux of sediment to the Yellow Sea (Huanghai) is very limited. We show that this flux takes place via a nepheloid layer across the Bohai Sea strait, transporting similar to 6.10(9) kg.y(-1), i.e, less than 1% of the Huanghe sediment discharge.

引用

页码：243 / 254

页数：12

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