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Shear Strength Study of Cohesive Sediment in The Lower Yellow River

机译:黄河下游粘性沉积物的抗剪强度研究

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It is a complex problem for the cementation strength between cohesive fine sediment. In this study, the cementation strength of cohesive fine sand is studied, and the cementation strength index is expressed by shear strength in soil mechanics. Through the shear strength test of remolded cohesive fine sediment, the shear strength parameters of cohesive fine sediment were obtained, and the effects of water content and particle size distribution on the shear strength of cohesive fine sediment were analyzed. The results show that the cohesion of cohesive fine sediment decreases with the increase of water content, the internal friction angle varies with the change of water content due to different particle size distribution, and the shear strength decreases with the change of water content. For cohesive fine sediment with median size less than 0.03mm, the shear strength with water content ranging from 5% to 30% ranges from 100 kPa to 600 kPa. For fine sediment with median size less than 0.01mm, the shear strength with water content ranging from 30% to 52% decreases significantly, mostly within 100 kPa. It can be seen that the water content has a great influence on the shear strength of cohesive fine sand. This study provides a basis for understanding the cementation strength of cohesive fine sediment grains and lays a foundation for further study on the scour resistance of cohesive fine sediment.
机译:这是一个复杂的粘合强度在内聚力细沉积物之间的问题。在这项研究中,研究了粘性细砂的胶结强度,并通过土壤力学剪切强度表示胶结强度指数。通过重形粘性细细沉积物的剪切强度试验,获得了内聚细沉积物的剪切强度参数,分析了含水含量和粒度分布对粘性细沉积物的剪切强度的影响。结果表明,随着水含量的增加,内聚细粒沉积物的内聚力降低,内部摩擦角随由于不同粒度分布而导致的含水量的变化,并且剪切强度随着水含量的变化而降低。对于中间尺寸小于0.03mm的粘性细沉积物,水含量的剪切强度为5%至30%范围为100kPa至600kPa。对于低于0.01mm的中间沉积物,水含量范围为30%至52%的剪切强度显着降低,主要在100kPa内。可以看出,水含量对内聚细砂的剪切强度有很大影响。本研究为了解粘性细沉积物谷物的胶结强度,为进一步研究粘性细细沉积物进行进一步研究的基础。

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