首页> 外文会议>International conference on Chinese transportation professionals;ICCTP 2009 >CT Scan on Frozen Roadbed Soil under Dynamic Triaxial Test Condition ofBeilu River Section, Qinghai-Tibet Railway of China
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CT Scan on Frozen Roadbed Soil under Dynamic Triaxial Test Condition ofBeilu River Section, Qinghai-Tibet Railway of China

机译:青藏铁路北麓河段动态三轴试验条件下冻土路基CT扫描

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As an effective scanning method with no damage, the CT scanning techniqueis used more widely in studying the dynamic deformation of frozen soil. Aiming atstability and dynamic deformation of frozen soil, the structural change before andafter a dynamic tri-axial test, failure type and their main affecting factors of frozensoil taken from roadbed of Qinghai-Tibet Railway are discussed from microstructureaccording to CT scanning results. It indicates that water content, temperature andconfining pressure are the main affecting factors. Change of density, strength andmodulus during dynamical deformation decreases with an increase of water contentand confining pressure, similarly the changes of the microstructure and structure.When temperature decreases, density, strength and modulus decrease rapidly, but themicrostructure and structural changes decreases. When axial dynamic strengthdecreases, degradation of density, strength, modulus changes from large to small atthe beginning and then from small to large, but structure change and demagnificationare the reverse of that. The dynamic failure type of the frozen soil depends on thecomposite in condition of higher water content and lower temperature, but belongs toloose expand and border cracking when water content is lower, belongs to equallyexpand type when confining pressure or temperature is higher, belongs to compositeand uniform expand type when confining pressure is lower and water content ishigher, and belongs to loose failure type when confining pressure is higher and watercontent is lower. To frozen soil, these CT scanning results and recognition not onlybenefit the study pf stability and dynamic deformation, but also provide importantdata for further dynamic characteristics studies and establishing dynamicdeformation models.
机译:作为一种无损伤的有效扫描方法,CT扫描技术被广泛用于研究冻土的动态变形。针对冻土的稳定性和动态变形,根据CT扫描结果,从微观结构出发,对青藏铁路路基动态三轴试验前后的结构变化,破坏类型及其主要影响因素进行了探讨。表明含水量,温度和围压是主要影响因素。动态变形过程中密度,强度和模量的变化随含水量和围压的增加而减小,微观组织和结构的变化也相似。当温度降低时,密度,强度和模量迅速下降,但微观结构和结构的变化却减小。当轴向动强度降低时,密度,强度,模量的降低从一开始就从大到小,然后从小到大,但是结构的改变和缩小是相反的。冻土的动态破坏类型取决于含水量较高和温度较低的复合材料,但含水量较低时属于松散膨胀和边界开裂,围压或温度较高时属于均匀膨胀型,属于复合均匀围压较低,含水量较高时为膨胀型,围压较高,含水量较低时为松散破坏型。对于冻土,这些CT扫描结果和识别结果不仅有利于稳定性和动态变形的研究,而且为进一步的动力特性研究和建立动态变形模型提供了重要的数据。

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  • 会议地点 Harbin(CN);Harbin(CN)
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    Jilin Institute of Architecture and Civil Engineering P.O. Box 130021 City Changchun P.R. China PH (86) 431-85935001 email:wanglixiaql@163.com;

    Institute of Subgrade and Protection Engineering Harbin Institute of Technology P.O. Box 150090 City Harbin P.R. China PH (86) 451-86282576 email: Xianzhang_ling@263.net;

    Institute of Subgrade and Protection Engineering Harbin Institute of Technology P.O. Box 150090 City Harbin P.R. China PH (86) 451-86282576;

    State Key Laboratory of Frozen Soil Engineering CAS P.O. Box 150090 City Lanzhou P.R. China email: wanglixiaql@163.com;

    School of Civil Engineering and Architecture Zhejiang University of Science andTechnology P.O. Box 310023 City Hangzhou P.R. China PH (86) 571-850;

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