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岩溶土洞演化及其数值模拟分析

贾龙 蒙彦 管振德

中国岩溶Issue(3):294-298,5.
中国岩溶Issue(3):294-298,5.

岩溶土洞演化及其数值模拟分析

Evolution and numerical simulation of a karst soil cave

贾龙 1蒙彦 2管振德1

作者信息

  • 1. 中国地质科学院岩溶地质研究所/国土资料部、广西壮族自治区岩溶动力学重点实验室,广西 桂林 541004
  • 2. 中国地质科学院岩溶塌陷防治重点实验室,广西 桂林 541004
  • 折叠

摘要

Abstract

Soil caves in karst areasarea concealed and adverse geological phenomena.The evolution of a soil cave can cause uneven displacement and stress redistribution on the overlying soil layer,conversely changes in displacement and stress can be used to study soil cave evolution using three-dimensional finite-difference software FLAC3D.The vertical displacement field of the soil layer shows that,the maximum vertical dis-placement taking place on the arch roof of the soil cave may cause tensile failure of the arch roof.Based on the level of soil layer displacement on the arch roof,an"equal settlement plane" can be drawn to determine the depth of the soil cave.The shear stress field of the soil layer indicates that,the maximum shear stress in the arch toes can cause arch toe shear failure,and the "low shear stress area" can be used to determine the impact of the arching effect on the overlying soil layer.Through analysis of the plastic zone of the soil layer, it is concluded that,in rigid clay areas,soil caves with barrel bottle-shaped pit collapse were mainly caused by arch roof collapse and tensile failure;while in areas of loose soil,caves with taper or plate-shaped pit col-lapse resulted from shear failure of the arch toe.The low shear stress area,equal settlement plane and plas-tic zone can be adopted to evaluate the stability of soil caves and the limits on hole size in the overlying layer. Evolution and numerical simulation of karst soil caves in this study provide important theoretical and engi-neering results for monitoring and evaluation of early stage karst collapse.

关键词

岩溶塌陷/土洞/FLAC3D/数值模拟

Key words

karat collapse/soil cave/FLAC3D/numerical simulation

分类

天文与地球科学

引用本文复制引用

贾龙,蒙彦,管振德..岩溶土洞演化及其数值模拟分析[J].中国岩溶,2014,(3):294-298,5.

基金项目

国家自然科学基金项目(41302255) (41302255)

国家自然科学基金项目(41302288) (41302288)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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