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Soil Water Characteristic Curve of an Unsaturated Soil under Low Matric Suction Ranges and Different Stress Conditions

机译:低吸力和不同应力条件下非饱和土的土壤水分特征曲线

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Accurate evaluation of unsaturated soil properties is critical for the design of geotechnical and geo-environmental structures such as road pavements, foundations, and earth dams. Water retention activity in soils which is used to predict the stability or seepage problems in the ground is one of the key features in unsaturated soil mechanics. Thus, many experimental works have reported on the unsaturated soil properties, and the soil-water characteristic curve (SWCC) test has contributed significantly to the interpretation of matric suction. Since traditional instruments cannot apply stress in SWCC tests, some researchers have developed suction controlled triaxial apparatus, by which SWCC tests are performed under different stress states. Determination of SWCCs under stress conditions similar to those in the field is key for interpretation of the hydro-mechanical behavior of unsaturated soils. This study conducted SWCC tests of unsaturated silt soil in low matric suction ranges under both drying and wetting conditions. The SWCCs were measured under one-dimensional and isotropic confining stresses ranging from 50 to 450 kPa. The micro porous membrane method was used instead of high air entry ceramic disk for controlling relatively low matric suction. The range of matric suction controlled was from 0 to 20 kPa. The study revealed that the measured SWCC in low matric suction ranges seems to be affected by the influence of stress conditions. Isotropic confining stress caused the void structure of the specimen to become dense and consequently, soil moisture flow movement also decreased. The water retention activity was obviously high, and the point regard to air entry value was larger. The study further suggests that the current methods adopted for estimating unsaturated soil properties require further development to take into account the effect of different stress conditions.
机译:对非饱和土壤特性的准确评估对于诸如道路路面,地基和土坝等岩土和地球环境结构的设计至关重要。土壤中的保水活性用来预测地下的稳定性或渗水问题,是非饱和土壤力学的关键特征之一。因此,许多实验工作报道了非饱和土壤的性质,而土壤水特征曲线(SWCC)试验对基质吸力的解释做出了重要贡献。由于传统仪器无法在SWCC测试中施加应力,因此一些研究人员开发了吸力控制三轴设备,通过该设备可以在不同的应力状态下进行SWCC测试。在与现场类似的应力条件下确定SWCC是解释非饱和土壤水力力学行为的关键。这项研究在干燥和湿润条件下在低基质吸力范围内进行了非饱和粉土的SWCC测试。 SWCC在50至450 kPa的一维和各向同性限制应力下测量。使用微孔膜方法代替高进气陶瓷盘来控制相对较低的基质吸力。基质吸力的控制范围为0至20 kPa。研究表明,在低基质吸力范围内测得的SWCC似乎受应力条件的影响。各向同性的封闭应力使试样的孔隙结构变得致密,因此,土壤水分流动也减少了。保水活性明显较高,并且与空气进入值有关的点较大。研究进一步表明,目前用于估算非饱和土壤特性的方法需要进一步发展,以考虑到不同应力条件的影响。

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