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Rheological Characteristics and Run-out Simulation of Fine-Grained Soils with Sand Content and Liquidity Index

机译:含砂量和流动性指数的细粒土的流变特性和跳动模拟

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To evaluate effects of sand content and liquidity index(water content)on the rheological properties of fine-grained soils, several series oflaboratory tests were performed on specimens with various sandcontents of 0, 5, 10, and 15% or with various liquidity indices rangingfrom 5 to 12.3. The flow behavior was strongly influenced by liquidityindex(water content) and sand content. The overall shape of the flowcurves of specimens had characteristics of a shear thinning fluid, with adecrease in viscosity as shear rate increased. The yield stress andviscosity gradually decreased as the liquidity index increased. At agiven liquidity index, yield stress and viscosity of soil increased with anincrease in sand content. A two-dimensional flow model (FLO-2D) wasused to simulate a debris flow including flow depth, velocity andvolumetric sediment using rheological data collected in this study. Itwas found that velocity and run-out distance decreased as viscosity andyield stress increased. Numerical results indicated that flowcharacteristics of debris flow depended on viscosity and yield stress ofsoil.
机译:评估含砂量和流动性指数(水含量)的影响 细颗粒土壤的流变特性 实验室测试是用各种沙子对标本进行的 含量为0%,5%,10%和15%或各种流动性指数 从5到12.3。流动性受到流动性的强烈影响 指数(水含量)和含沙量。流的整体形状 试样的曲线具有剪切稀化流体的特征,具有 粘度随剪切速率的增加而降低。屈服应力和 随着流动性指数的增加,粘度逐渐降低。在 在给定流动性指数的情况下,土壤的屈服应力和黏度随 增加砂含量。二维流动模型(FLO-2D)为 用于模拟泥石流,包括泥流深度,流速和 使用本研究收集的流变数据收集体积沉积物。它 发现速度和跳动距离随粘度和 屈服应力增加。数值结果表明流量 泥石流的特征取决于黏度和屈服应力 泥。

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