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Impact of temperature variation on pressuremeter test parameters in compacted soils

机译:温度变化对压实土壤中压力计测试参数的影响

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摘要

In geotechnical engineering, the proper design of thermo-active geostructures (piles, foundations,rnetc.) and deep waste storage disposals requires a better understanding of the thermo-hydro-mechanical behaviourrnof natural and compacted soils. For design purposes, important mechanical parameters of the soils such as thernpressuremeter modulus (E_P), limit pressure (P_l ) and creep pressure (P_f ) are usually obtained by pressuremeterrnin-situ tests. In the present study, pressuremeter tests were conducted in laboratory, using a mini-pressuremeter,rnto characterise compacted soils. The objective was to examine and quantify the influence of temperature changesrnon pressuremeter parameters of two different compacted soils: a clay and a loam. These soils were compactedrnat their optimal water content and 90% of their maximal dry density (standard Proctor) in a thermo-regulatedrnmetric scale container of 800mm in height and 600mm in diameter. The compacted soils were then subjectedrnto a range of temperatures from 20 to 50◦C.rnOnly six tests were performed in each container to prevent edge effects and interaction between the tests.rnThe thermal cycles were applied to the soil massif as following: A heating-cooling cycle (20–40–20◦C) for thernclay; three heating-cooling cycles (20–50◦C) for the loam. Pressuremeter tests were conducted at the end ofrnseveral temperature steps. The obtained results showed a decrease in P_l and P_f with increasing temperaturernfor both tested soils, while the variation of E_P was less significant. Through the temperature range tested, arnquasi-reversibility of the effect of a heating cycle is obtained.
机译:在岩土工程中,对热活性地质结构(桩,地基等)和深层废物存储处置的正确设计需要对天然和压实土壤的热-水-机械行为表现有更好的了解。为了设计目的,通常通过压力计原位测试获得土壤的重要机械参数,例如压力计模量(E_P),极限压力(P_1)和蠕变压力(P_f)。在本研究中,压力计测试是在实验室中使用微型压力计进行的,以表征压实土壤。目的是检查和量化温度变化对两种不同压实土壤:粘土和壤土的影响。这些土壤在高度为800mm,直径为600mm的温度调节容器中以最佳含水量和最大干密度的90%(标准Proctor)压实。然后将压实的土壤置于20至50°C的温度范围内。为防止边缘效应和各测试之间的相互作用,每个容器仅进行了六个测试。对土壤的热循环如下:粘土的冷却循环(20–40–20℃);壤土的三个加热-冷却循环(20–50°C)。在数个温度步骤的最后进行压力计测试。所获得的结果表明,对于两种测试土壤,P_l和P_f均随温度rn的升高而降低,而E_P的变化不那么显着。在测试的温度范围内,获得加热循环效果的近似可逆性。

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  • 来源
    《Energy geotechnics》|2016年|699-705|共7页
  • 会议地点 Kiel(DE)
  • 作者单位

    LEMTA (CNRS, UMR 7563), Université de Lorraine, Vandoeuvre-lès-Nancy-FranceESITC de Metz, Metz-France;

    LEMTA (CNRS, UMR 7563), Université de Lorraine, Vandoeuvre-lès-Nancy-FranceESITC de Metz, Metz-France;

    LEMTA (CNRS, UMR 7563), Université de Lorraine, Vandoeuvre-lès-Nancy-France;

    LEMTA (CNRS, UMR 7563), Université de Lorraine, Vandoeuvre-lès-Nancy-France;

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  • 正文语种 eng
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