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渐进式滑坡锚索抗滑桩预应力张拉值计算 被引量:3
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作者 侯小强 王新飞 +3 位作者 贾洪璐 安玉科 周重任 侯云龙 《工程科学与技术》 EI CAS CSCD 北大核心 2024年第1期138-147,共10页
依据渐进式滑坡蠕变特点,现有锚索抗滑桩计算模型针对渐进式滑坡桩–锚–土三者相互作用过程考虑较少。针对这一问题,将渐进式滑坡缓慢失稳的变形特征和预应力锚索抗滑桩从空载到满载动态工作过程相结合,利用Winkler弹性地基梁理论,优... 依据渐进式滑坡蠕变特点,现有锚索抗滑桩计算模型针对渐进式滑坡桩–锚–土三者相互作用过程考虑较少。针对这一问题,将渐进式滑坡缓慢失稳的变形特征和预应力锚索抗滑桩从空载到满载动态工作过程相结合,利用Winkler弹性地基梁理论,优化了锚索抗滑桩桩–锚变形协调条件,考虑桩后土压力渐进变化过程,构建不同工况桩–锚–土协同工作的计算模型,推导了预应力锚索抗滑桩施工阶段初张拉值的计算方法。结合工程算例和有限元软件数值模拟结果,为获取较高精度的计算数值,采用MATLAB软件编译程序进行计算分析。结果表明:1)渐进式滑坡“稳定–蠕动–失稳”阶段性变形特点决定了预应力锚索抗滑桩“空载–加载–满载”三阶段桩–锚动态内力变形过程,明确了各阶段桩后可能存在的土压力模型,单纯进行满载阶段锚索拉力设计不符合渐进式滑坡实际作用机理,进一步证明施工阶段锚索预应力张拉值设计的重要性;2)渐进式滑坡推力由尚未产生的初始空载阶段至完全作用的满载阶段,两阶段并非互相独立存在,二者通过桩–锚变形协调条件相互作用,表明了施工阶段抗滑桩预应力张拉力值大小受满载阶段桩锚内力及变形大小的影响;3)依据渐进式滑坡锚索抗滑桩动态内力变形过程,保证抗滑桩受荷段和锚固段内力大小均衡相等,优化了满载阶段全桩弯矩平衡设计原则,确立了以静止土压力作为施工阶段预应力张拉值设计标准,对比表明,此计算方法优于其余4种现有算法,同时有限元数值模拟结果与本文算法贴合度较高,进一步验证了此计算方法的合理性和可靠性。研究成果可为渐进式滑坡中预应力锚索抗滑桩的设计计算和施工提供技术指导。 展开更多
关键词 渐进式滑坡 锚索预应力 桩锚协调变形 土压力状态 锚索设计拉力
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Three-dimensional consolidation deformation analysis of porous layered soft soils considering asymmetric effects 被引量:1
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作者 张治国 黄茂松 王卫东 《Journal of Central South University》 SCIE EI CAS 2014年第9期3639-3647,共9页
Long-term settlements for underground structures, such as tunnels and pipelines, are generally observed after the completion of construction in soft clay. The soil consolidation characteristic has great influences on ... Long-term settlements for underground structures, such as tunnels and pipelines, are generally observed after the completion of construction in soft clay. The soil consolidation characteristic has great influences on the long-term deformation for underground structures. A three-dimensional consolidation analysis method under the asymmetric loads is developed for porous layered soil based on Biot's classical theory. Time-displacement effects can be fully considered in this work and the analytical solutions are obtained by the state space approach in the Cartesian coordinate. The Laplace and double Fourier integral transform are applied to the state variables in order to reduce the partial differential equations into algebraic differential equations and easily obtain the state space solution. Starting from the governing equations of saturated porous soil, the basic relationship of state space variables is established between the ground surface and the arbitrary depth in the integral transform domain. Based on the continuity conditions and boundary conditions of the multi-layered pore soil model, the multi-layered pore half-space solutions are obtained by means of the transfer matrix method and the inverse integral transforms. The accuracy of proposed method is demonstrated with existing classical solutions. The results indicate that the porous homogenous soils as well as the porous non-homogenous layered soils can be considered in this proposed method. When the consolidation time factor is 0.01, the value of immediate consolidation settlement coefficient calculated by the weighted homogenous solution is 27.4% bigger than the one calculated by the non-homogeneity solution. When the consolidation time factor is 0.05, the value of excess pore water pressure for the weighted homogenous solution is 27.2% bigger than the one for the non-homogeneity solution. It is shown that the material non-homogeneity has a great influence on the long-term settlements and the dissipation process of excess pore water pressure. 展开更多
关键词 three-dimensional consolidation deformation porous layered soils asymmetric loads long-term deformation prediction transfer matrix method
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Calculation of earth pressure based on disturbed state concept theory 被引量:4
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作者 朱剑锋 徐日庆 +1 位作者 李昕睿 陈页开 《Journal of Central South University》 SCIE EI CAS 2011年第4期1240-1247,共8页
The theoretical formulations of Coulomb and Rankine still remain as the fundamental approaches to the analysis of most gravity-type retaining wall,with the assumption that sufficient lateral yield will occur to mobili... The theoretical formulations of Coulomb and Rankine still remain as the fundamental approaches to the analysis of most gravity-type retaining wall,with the assumption that sufficient lateral yield will occur to mobilize fully limited conditions behind the wall.The effects of the magnitude of wall movements and different wall-movement modes are not taken into consideration.The disturbance of backfill is considered to be related to the wall movement under translation mode.On the basis of disturbed state concept(DSC),a general disturbance function was proposed which ranged from-1 to 1.The disturbance variables could be determined from the measured wall movements.A novel approach that related to disturbed degree and the mobilized internal frictional angle of the backfill was also derived.A calculation method benefited from Rankine's theory and the proposed approach was established to predict the magnitude and distribution of earth pressure from the cohesionless backfill under translation mode.The predicted results,including the magnitude and distribution of earth pressure,show good agreement with those of the model test and the finite element method.In addition,the disturbance parameter b was also discussed. 展开更多
关键词 disturbed state concept disturbance function translation mode earth pressure cohesionless soil
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Earth pressure coefficient at rest during secondary compression 被引量:2
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作者 赵晓东 周国庆 +1 位作者 商翔宇 陈国舟 《Journal of Central South University》 SCIE EI CAS 2011年第6期2115-2121,共7页
In order to obtain the earth pressure coefficient at rest (K0) at higher consolidation pressures during secondary compression, a series of K0 tests for saturated reconstituted clay were conducted. The results indicate... In order to obtain the earth pressure coefficient at rest (K0) at higher consolidation pressures during secondary compression, a series of K0 tests for saturated reconstituted clay were conducted. The results indicate that the measured K0 in secondary compression can be described by equations related to internal friction angle, secondary compression coefficient, compression index, recompression index, and sediment time. Effects of consolidation pressures and sediment time on K0 during secondary compression can be attributed to cementation (part of cohesion) increase and internal friction angle decrease. Cementation increase leads to nonlinear variation for K0 and internal friction angle decrease results in increase of K0. K0 computed by equations associated with internal friction angle is overestimated at apparent lower consolidation pressures with different sediment time, which agrees with the measured values well at apparent higher consolidation pressures. 展开更多
关键词 earth pressure coefficient at rest secondary compression internal friction angle CEMENTATION
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