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首页> 外文期刊>Fresenius environmental bulletin >INVESTIGATING THE STRENGTH PARAMETERS OF UNSATURATED SOIL IN SEASONAL FROZENAREAS UNDER LOW MATRIC SUCTION AND THEIR EFFECT ON OVERWINTERING DEEP FOUNDATION PITS
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INVESTIGATING THE STRENGTH PARAMETERS OF UNSATURATED SOIL IN SEASONAL FROZENAREAS UNDER LOW MATRIC SUCTION AND THEIR EFFECT ON OVERWINTERING DEEP FOUNDATION PITS

机译:低迷型吸力下季节性氧化酶中不饱和土的强度参数及其对越冬遍的深层坑的影响

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In the current paper, we explore the effect of temperature changes in seasonal frozen areas on the strength parameters of unsaturated soil under low matric suction, as well as the impact of the parame-ters under different temperatures on an overwinter-ing deep foundation pit in unsaturated soil under low matric suction. In particular, we take unsaturated silty clay in its original state as the research object and Global Digital Systems Ltd.(GDS)unsaturated silty soil as the triaxial tester to perform triaxial shear tests on unsaturated silty clay under several temper-atures. The strength parameters obtained from the la-boratory tests are then combined with Abaqus nu-merical simulations to analyze the stress and defor-mation of the overwintering deep foundation pit sup-porting structure in unsaturated soil within seasonal frozen areas. Experimental results under low matric suction demonstrate that temperature variations have a greater effect on the total cohesive force ofunsatu-rated silty clay, yet their impact on the effective in-ternal friction angle is relatively small. The influence of the frost heaving force produced by the freezing of the unsaturated soil on supporting structures is ob-served to be greater than the earth pressure during the freeze-thaw process. When the unsaturated soil is frozen, the horizontal frost heaving force of the re-taining structure at the top and bottom of the founda-tion pit is relatively large. Furthermore, the selection of strength parameters for unsaturated soil during the freeze-thaw process has a great influence on the sur-rounding environment of the deep foundation pit, as well as the stress and the deformation of the support-ing structure. Numerical simulations using strength parameters under different temperatures(20°C°C,-15°CC.20°CC--15°CC-20°C) resulted in the following general trend for the horizontal displacement of the retaining structure, the horizontal force of the pile side and the displacement of the topof the deep foun-dation: simulation results of frozen soil parameters>simulation results ofdynamic changes of parameters with temperature>simulation results of normal tem-perature soil parameters.
机译:在目前的论文中,我们探讨了在低迷型吸力下不饱和土的强度参数对季节性冷冻区域的温度变化的影响,以及在溢出深基坑坑中不同温度下的析谱间的影响低原味吸力下的不饱和土壤。特别是,我们在原始状态下作为研究对象和全球数字系统有限公司(GDS)不饱和粉状土壤作为三轴测试仪,在不饱和粉质下在几个脾气下进行三轴剪切试验。然后将从La-Boratory测试获得的强度参数与ABAQUS NU-的模拟结合,以分析季节性冷冻区域内不饱和土的越来越深基坑Sup-Porting结构的应力和差异。低原型抽吸下的实验结果表明,温度变化对Ofunsatu级粉冻粘土的总粘性力产生了更大的影响,但它们对有效内摩擦角的影响是相对较小的。通过在支撑结构上冻结的冷冻产生的霜起伏力的影响是大于冷冻 - 解冻过程中的接地压力。当不饱和的土壤被冷冻时,铸造坑顶部和底部的重新染色结构的水平霜冻力相对较大。此外,冻融过程中不饱和土的强度参数的选择对深基坑的圆形环境以及应力和支撑结构的变形具有很大影响。使用不同温度下的强度参数(20°C°C,-15°CC.20°CC - 15°CC-20°C)的数值模拟导致静止结构水平位移的以下一般趋势,水平桩侧的力量和深层Foun dation的前置位移:冷冻土壤参数的仿真结果>仿真结果与温度变化的仿真变化,温度>仿真结果正常温度土壤参数。

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