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Mechanical Properties of Riverbank Soil in the Jingjiang Reach and the Characteristics of Flow in Pocket Collapse Area

机译:京江河岸土壤的力学性能与口袋坍塌区流动的特点

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摘要

Based on analyzing the field data and the experimental results, Mechanical properties of riverbank soil in the Jingjiang Reach and the characteristics of flow in the region of pocket collapse are discussed. It is calculated that riverbank of the Jingjiang Reach is characterized by a typical composite structure, covering the low liquid limit cohesive upper layer and the sandy lower layer. The cohesion of the cohesive soil increases first and then decreases with the increase of water content. The internal friction angle generally decreases with the increase of water content. The flow structure in pocket collapse area shows the intensive three-dimensional characteristics. The surface and vertical average velocity, the range and strength of the reflux increase with the increase of upstream flow discharge. Under different conditions of flow discharge, the vertical average velocity in pocket collapse area has a distributed feature of nearly linear or tiny oscillation along the relative direction of water depth. The research can provide the technical support for prevention measures of bank collapse.
机译:基于分析现场数据和实验结果,讨论了荆江河岸土壤的力学性能和口袋塌陷区域的流动特征。计算荆江河的河岸的特点是典型的复合结构,覆盖低液体限制粘结的上层和砂质下层。粘性土壤的内聚力首先增加,然后随着水含量的增加而降低。随着水含量的增加,内部摩擦角通常会降低。口袋塌陷区的流动结构显示了密集的三维特性。表面和垂直平均速度,回流的范围和强度随着上游流量排出的增加而增加。在流动放电的不同条件下,袋塌陷区域中的垂直平均速度具有沿着水深的相对方向的几乎线性或微小振荡的分布特征。该研究可以为防止银行崩溃措施提供技术支持。

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