摘要
利用文献中的泥沙起动流速公式,推导出非均匀细颗粒泥沙起动流速近似估算公式。采用长江口南槽定点测量涨落潮过程中水深、水面以下1m的流速与近底床悬沙粒径d95资料,拟合该近似估算公式。估算结果表明:近底床悬沙粒径d95小于0 06mm的细颗粒泥沙起动流速值大于已有水槽实验值。
Referring to the existing literatures, an approximate equation to estimate threshold velocity for nonuniform fine sediments is derived. This equation is fitted by the mean water depth, the flow velocity at 1 m below the water surface and the nearbottom suspended sediment particles sizes d95, which are collected from one monitoring station during flood/ebb tides at the South Passage of the Changjiang Estuary. Results suggest that the threshold velocities for nonuniform fine sediments (d95<006 mm) are larger than the laboratory experimental data in the literatures.
出处
《泥沙研究》
CSCD
北大核心
2003年第5期37-40,共4页
Journal of Sediment Research
基金
国家杰出青年科学基金(海口海岸学40225014)
国家自然科学基金(49571007)联合资助
关键词
长江口
细颗粒泥沙
起动流速
近似估算
非均匀
non-uniform fine sediments
threshold velocities
the Changjiang Estuary