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TEST RESEARCH ON DEFORMATION OF COARSE-GRAINDE SOIL WITH WEAK ROCK DUE TO WETTING-DRYING CYCLE

机译:湿润干燥循环由于弱岩石粗麦芽土壤变形试验研究

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The wetting-drying cyclic tests are tried for coarse-grained soil with weak rocks using iron wire mesh as outer boundary, wetting by steaming and drying by hot-dry wind. Main tests organized as wetting-drying tests under different constant stress state, wetting-drying tests with various moistened water content under certain stress state and second time wetting-drying test under changed stress state. The test results indicate that there are three existent states of water in coarse-grained soil and their action and affection on humidification deformation are different; the deformation in first cycle is notable, after several wetting and drying cycles, the deformation in a wetting and drying cycle becomes stable and the deformation in drying is more outstanding than that in wetting; in second time wetting-drying test, increased stress induces considerable deformation and decreased stress induces negligible deformation. The test results are important for realizing the microscopic mechanism of the humidification and dehumidification of coarsegrained soil and the long time behavior of high earth-rock dams. The test results supply a reference for the design and construction of high earth-rock dams.
机译:使用铁丝网作为外边界,通过蒸汽滤网,通过热风风蒸汽润湿,润湿干燥的循环试验。主要试验组织为在不同恒定应力状态下的润湿干燥试验,在改变应力状态下在某些应力状态下具有各种润湿的水含量的润湿干燥试验。测试结果表明,粗粒土壤中存在三种存在的水状态,它们对加湿变形的作用和感情是不同的;在润湿和干燥循环几次润湿和干燥循环之后,第一循环中的变形是值得注意的,在润湿和干燥循环中变形变得稳定,干燥的变形比润湿更加出色;在第二次润湿干燥试验中,增加应力诱导相当大的变形和降低的应力引起可忽略不计的变形。试验结果对于实现加湿和粗晶土壤的湿润和除湿性的微观机制以及高地岩石坝的长时间行为。测试结果为高地岩石坝设计和施工提供了参考。

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