Experimental study on liquefaction fluidity of saturated loess
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摘要: 在室内动液化试验的基础上,对液化后的试样进行三轴剪切试验,并利用流体力学方法对黄土液化流动性进行了研究。研究表明:液化后的试样在受三轴剪切作用时,其表观黏度呈现先增大后减小的现象,即其流动特性会出现从“剪切稠化”到“剪切稀化”的转变。这种现象的出现可能与黄土特殊的结构性以及试验所采取的液化标准趋于保守有关。石碑塬地区特殊的地质环境和黄土的“剪切稀化”性质导致了低角度、长距离液化滑移灾害的发生。Abstract: Based on the laboratory dynamic liquefaction tests, the triaxial shear tests are carried out on the liquefied samples, and the liquefaction fluidity of loess is studied by using the fluid mechanics method.The results show that the apparent viscosity of liquefied samples increases first and then decreases when subjected to triaxial shear, that is, the flow characteristics will change from "shear thickening" to "shear thinning" .This phenomenon may be related to the special structure of loess and the conservative liquefaction standard adopted in the tests.The special geological environment and the "shear thinning" property of loess in Shibeiyuan area lead to the occurrence of low-angle and long-distance liquefaction slip disasters.
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Keywords:
- loess /
- apparent viscosity /
- shear thinning /
- liquefaction slip
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图 6 石碑塬地区地层剖面[10]
Figure 6. Stratigraphic section of Shibeiyuan area
表 1 试样物性指标
Table 1 Basic physical parameters of loess samples
参数 取样深度/m 颗粒组成/% 孔隙比 含水率/% 塑性指数 黏粒 粉粒 砂粒 数值 15 12.4 33.8 53.8 7.0 9.1 7.6 -
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