期刊
APPLIED OCEAN RESEARCH
卷 69, 期 -, 页码 116-125出版社
ELSEVIER SCI LTD
DOI: 10.1016/j.apor.2017.10.005
关键词
Threshold of sediment motion; Silt; Cohesive force; Additional static water pressure; Shields curve
资金
- Joint Research Project of National Natural Science Foundation of China (NSFC) - The Netherlands Organization for Scientific Research (NWO) [51061130546]
- NSFC [51509160, 51520105014, 51379127]
Sediment incipient motion is a fundamental issue in sediment transport theory and engineering practice. Silt has transitional behavior between cohesive and non-cohesive sediment and its incipient motion is still poorly understood. This study aims to find an expression for incipient motion from silt to sand from a unified perspective and analysis. From the analysis of forces, using the derivation method for the Shields curve, an expression for sediment incipient motion is proposed for both silt and sand under conditions of combined waves and currents. The differences and similarities in the sediment motion threshold were analyzed under the effects of waves and currents, and fine and coarse sediment. The Shields number was revised by introducing the cohesive force and additional static water pressure, which indicates that this study could be seen as an extension of the Shields curve method for silt. A number of experimental datasets as well as field data were used to verify the formula. The effect of bulk density on fine sediment was discussed and tested using experimental data. (C) 2017 Elsevier Ltd. All rights reserved.
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