摘要
压实度是影响填方边坡稳定性的重要因素,为了分析不同压实度下填方边坡的稳定性,设计了不同压实度下填方边坡工况,分析并建立了压实土体本构关系模型,基于有限元强度折减理论,分析了变形破坏趋势,确定极限抗剪强度。采用Bishop方法计算土条两侧的作用力,在不考虑土体侧向变形的情况下,计算得出边坡稳定性系数和填土外加应力作用下导致的沉降变形值,根据计算结果提出了填方边坡稳定性防护对策。结果表明:所提出的分析方法能够准确分析出填方边坡变形情况,有效降低了稳定性分析误差,并且将其应用于实际填方边坡稳定性分析中,具有实际应用意义。
Compaction degree is an important factor affecting the stability of the fill slope.In order to analyze the stability of the fill slope under different compaction degree,the working conditions of the fill slope under different compaction degree were designed,and the constitutive relationship model of the compacted soil was analyzed and established.Based on the finite element strength reduction theory,the deformation and failure trend were analyzed and the ultimate shear strength was determined.Using the Bishop method to calculate the forces on both sides of the soil strip,without considering the lateral deformation of the soil,the stability coeffi-cient of the slope and the settlement deformation value caused by the external stress of the fill soil were calculat-ed.Based on the calculation results,stability protection measures for the fill slope were proposed.The results show that the proposed analysis method can accurately analyze the deformation of fill slopes,effectively reduce stability analysis errors,and apply it to the stability analysis of actual fill slopes,which has practical application significance.
作者
王振华
邓辉
张永军
WANG Zhenhua;DENG Hui;ZHANG Yongjun(Gansu Institute of Natural Resources Planning and Research,Lanzhou 730000,Gansu,China;State Key Laboratory of Geological Disaster Prevention and Geological Environmental Protection,Chengdu University of Technology,Chengdu 610059,Sichuan,China;Key Laboratory of Groundwater Engineering and Geothermal Resources in Gansu Province,Lanzhou 730050,Gansu,China)
出处
《西北地质》
CAS
CSCD
北大核心
2024年第4期262-270,共9页
Northwestern Geology
基金
2020年度中央财政自然灾害防治体系建设项目“兰州市黄土斜坡变形破坏机理及风险管控措施研究”(甘资财发〔2020〕16号)资助成果。
关键词
压实度
填方边坡
稳定性
防护对策
抗剪强度
沉降变形
compaction
fill slope
stability
protection countermeasures
shear strength
settlement defor-mation