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DETERMINATION OF THE SOIL-WATER CHARACTERISTIC CURVE USING THE EVAPORATION TECHNIQUE

机译:蒸发技术测定土壤 - 水特性曲线

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The measurement of the Soil-Water Characteristic Curve (SWCC) is an important initial step in applications that require knowledge of the partially saturated soil behavior. The relationship between the pore-water suction and the soil water content is known as the SWCC. This relationship is fundamental to the description of the behavior of unsaturated soils. SWCCs are hysteretic, with the drying limb plotting above the wetting limb. Hysteresis is generally occurring due to entrapped air inside the pores. In this study, only the drying limb of the SWCC was measured. The standard method in determining the SWCC relies on the pressure plate (PP) apparatus (D3152-72, 1994). The PP apparatus is generally used to determine the equilibrium water content for various pore-water suctions allowing the construction of SWCC. The PP methodology is time consuming, expensive and elaborate. Thermocouple psychrometer (TCP) provides an alternative device to the PP for the SWCC measurement. TCPs are a simple and reliablemethod in the measurement of the soil total suction in the field and in the laboratory (Tsai and Petry, 1995). Previous studies (Daniel et al., 1981, Meerdink et al., 1996, Chiu and Shackelford, 1998, Yaldo, 1999, and Merayyan and Miller 2000) showed that the use of TCPs in the measurement of total suction in order to construct the SWCC of compacted finegrained soils is acceptable. In the current investigation, an evaporation scheme that utilizes TCPs was used in the determination of SWCC. This schemeis referred to as the "Evaporation Technique." This study will attempt to use the Evaporation Technique in the SWCC determination. In order to construct the SWCC using the Evaporation Technique, samples were prepared using three soil types (Plasticity index (PI) 7-60) compacted at or near wet of optimum water content. The findings of this investigation are in good agreement with the data reported in the literature using the PP. Samples were arranged in the order of their PI. Higher PI samples at the same suction resulted in less water content. The Evaporation Technique created as part of this study is proven to be efficient, and reliable.
机译:土壤 - 水特性曲线(SWCC)的测量是需要了解部分饱和的土壤行为的应用中的重要初始步骤。孔隙水抽吸与土壤含水量之间的关系称为SWCC。这种关系是对不饱和土壤行为的描述的基础。 SWCC是滞后的,干燥肢体在润湿肢体上方绘制。通常由于孔内夹带的空气而导致滞后。在该研究中,仅测量SWCC的干燥肢体。确定SWCC的标准方法依赖于压板(PP)装置(D3152-72,1994)。 PP装置通常用于确定允许SWCC的构建的各种孔隙水吸液的平衡含水量。 PP方法是耗时,昂贵和精心制作。热电偶手法计(TCP)为PP提供了一种替代设备,用于SWCC测量。 TCPS是一种简单而重新构建在田间和实验室的土壤总吸气量(Tsai和Petry,1995)中的一种简单和重新构建。以前的研究(Daniel等,1981年,Meerdink等,1996,Chiu和Shackelford,1998,Yaldo,1999和Merayyan和Miller 2000)表明,使用TCP在衡量总吸力时为了构建紧凑的Finegratmina的SWCC是可接受的。在目前的研究中,利用TCP的蒸发方案用于SWCC的测定。该方案称为“蒸发技术”。本研究将尝试在SWCC确定中使用蒸发技术。为了使用蒸发技术构建SWCC,使用三种土壤类型(可塑性指数(PI)7-60)在最佳含水量或湿湿含量附近进行样品来制备样品。本调查的调查结果与使用PP在文献中报告的数据一致。样品按照它们的pi的顺序排列。相同抽吸的较高的PI样品导致含水量较少。被证明是作为本研究的一部分产生的蒸发技术是有效和可靠的。

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