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浑水推移质分组输沙研究

孙志林 邵凯 许丹 梁旭

水利学报2012,Vol.43Issue(1):99-105,7.
水利学报2012,Vol.43Issue(1):99-105,7.

浑水推移质分组输沙研究

Fractional bedload transport in turbid waters

孙志林 1邵凯 1许丹 1梁旭2

作者信息

  • 1. 浙江大学水利与海洋工程系,浙江杭州310058
  • 2. 杭州市市区河道监管中心,浙江杭州310008
  • 折叠

摘要

Abstract

The mechanism of sediment transport in turbid water is different from that in clear water. According to the concept of three states exchange mode of non-uniform sediment at riverbed surface, an analytical formula for calculating the fractional bedload transport rate in turbid was established. In the formula the parameter expressing the drawn up possibility was introduced and the net exchange of bedload towards water flow was considered. The reliability of the proposed formula was verified by experimental and field observation data. It is found that the bedload particles may become coarser than that of original in turbid water. Furthermore, for exactly estimating the sandy bedload transport rate the content of suspended load which comes from bedload should be neglected.

关键词

非均匀沙/分组/推移质/输沙率/浑水

Key words

non-uniform sediment/fractional bedload/transport rate/turbid waters

分类

建筑与水利

引用本文复制引用

孙志林,邵凯,许丹,梁旭..浑水推移质分组输沙研究[J].水利学报,2012,43(1):99-105,7.

基金项目

国家自然科学基金项目 ()

国家科技重大专项课题 ()

水利学报

OA北大核心CSCDCSTPCD

0559-9350

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