课题基金 / 基金详情

黄土细观界面形成演化机制试验研究

批准号:
42107198
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
马鹏辉
依托单位:
学科分类:
工程地质环境与灾害
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
马鹏辉

项目摘要

结项摘要

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中文摘要
黄土界面是黄土形成演化过程中形成的产物,是黄土发生灾变的根源。同时平山造城、治沟造地和固沟保塬等重大工程建设过程中,也形成了众多堆填土与黄土之间的人工界面,在黄土界面控灾这一全新认识中,这些界面均是黄土细观界面发展演化的综合外在体现。本项目拟通过野外调研、室内土工试验、计算机图像处理技术、三轴加载协同实时CT扫描试验等研究手段开展以下三个方面的研究:(1)大量获取黄土细观界面数据,总结其成因与发育规律;(2)获取土样图像切片并构建三维数字模型,提取黄土细观界面的关键要素,分析其在加载过程中的变化趋势;(3)基于黄土细观界面动态发展过程和土体力学行为变化过程,分析土体损伤过程与土体强度的折减关系。从而搭建细观界面的基础数据库,重现细观界面形成演化过程,建立黄土细观结构损伤数学评价模型,初步揭示黄土细观界面形成演化机制。研究成果将为黄土界面控灾机制和黄土灾害预测预报研究提供数据支撑和理论依据。
英文摘要
Loess interface is formed during the formation and evolution of loess. It is the root cause of loess disasters. At the same time, many artificial interfaces between landfills and loess have also been formed during the construction of major projects such as Mountain Excavation and City Construction, Gully Stabilization and Land Reclamation, Gully Control and Highland Protection, etc. “Loess disasters was controlled by the loess interface” was a new understanding, in which these loess interfaces are the comprehensive external manifestations of the loess meso interface. This project intends to carry out the following three aspects of research through the methods such as field investigations, soil tests, computer image processing technology, real-time CT scanning tests in the condition of triaxial loading: (1) Collecting a large amount of data of loess meso interface, and summarize the inducing factors and development characteristics of the loess meso interface; (2) Collecting image slices of the soil sample and construct the 3D digital core models. Extracting the key elements of the loess meso interface, and analyze its changing trend during the loading process; (3) Based on the dynamic development process of the loess meso interface and the change process of the mechanical behavior of soil, the relationship between the damage process of the soil and the reduction of soil strength was analyzed. We aimed to build a basic database of the loess meso interface, reproduce the formation and evolution process of the loess meso interface, establish a mathematical evaluation model for the damage of the meso structure of loess, and initially reveal the formation and evolution mechanism of the loess meso interface. The results will provide data support and theoretical basis for the mechanism of “loess disasters was controlled by the loess interface” and the prediction of loess disaster.
黄土界面是是黄土发生灾变的根源。同时挖山造城、治沟造地等重大工程建设过程中,也形成了众多堆填土与黄土之间的人工界面,在黄土界面控灾这一全新认识中,这些界面均是黄土细观界面发展演化的综合外在体现。本项目围绕“黄土细观界面的类型及其灾变效应”开展相关研究,取得的成果如下:(1)对黄土细观界面进行了定义与类型划分。细观界面其本质为地质缺陷,具有圆形状、对钩状、尖灭状及V形状的几何形态特征,组合特征表现为发散型的爪状、阶梯状、羽列状以及闭合型网格状。按成因分类为物理力学成因、生物活动成因、水土耦合成因、风化成因以及异相成因;(2)发现了黄土与其他地层界面的滞水效应是由于渗透差引起的。骨架颗粒是黄土结构中的主体部分,其形状决定了黄土的宏观特征,渗流前的土样粗颗粒表面覆盖着少量粘土集合体,在增湿作用下,通过细颗粒的运移,维持原黄土稳定性的结构可能发生破坏,导致快速坍塌,从而降低了渗透性,最终引发滑坡;(3)发现了连续固体→变形体→破裂体是黄土边坡的变形破裂阶段,黄土界面扩张效应与松动效应明显,黄土通过控制地貌、坡体、土体、颗粒,扩张和松动着土体与坡体,促使灾害链连续固体→变形体→破裂体转化。连续固体向变形体转化过程中,可以概述为以下四个过程:1.水沿结构面入渗阶段;2.水-结构面作用阶段;3.结构面松动阶段;4.湿陷沉降阶段。变形体→破碎体转化过程中,水土互馈作用主要表现在五个方面:冲蚀作用、静动水压力、崩解作用、溶滤潜蚀作用、湿陷作用;(4)发现了黄土灾害链从破裂体→散体是黄土边坡的滑移阶段,黄土界面分离效应与放大效应明显,黄土界面分离着坡体、放大着崩滑体,促使灾害链破裂体→散体转化。整体来说,黄土界面控制作用表现为:黄土坡体是由黄土界面和结构体组成,黄土界面和结构体的联合作用影响着黄土坡体的整体性。黄土界面是坡体中强度最薄弱的部位,也是水流入渗的主要通道。
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