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The Physical State of Finely Dispersed Soil-Like Systems with Drilling Sludge as an Example

机译:以钻井液为代表的精细分散的土壤样系统的物理状态

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The physical state and its dynamics were studied at the quantitative level for drilling sludge (finely dispersed waste of the oil industry). Using original methodological approaches, the main hydrophysical and technological properties of sludge samples were assessed for the first time, including the water retention curve, the specific surface, the water conductivity, the electrical conductivity, the porosity dynamics during shrinkage, the water yield, etc., which are used in the current models of water transfer and the behavior of these soil-like objects under real thermodynamic conditions. The technologically unfavorable phenomenon of the spontaneous swelling of sludge during the storage of drilling waste was theoretically explained. The water regime of the homogeneous 0.5-m thick drilling sludge layer under the free gravity outflow and permanent evaporation of water from the surface was analyzed using the HYDRUS-1D model. The high water retention capacity and the low water conductivity and water yield of sludge do not allow their drying to the three-phase state (with the entry of air) acceptable for terrestrial plants under humid climatic conditions, which explains the spontaneous transformation of sludge pits to only hydromorphic ecosystems. DOI: 10.1134/S1064229311020128
机译:在定量水平上研究了钻井污泥(石油工业中细分散的废物)的物理状态及其动力学。使用原始的方法学方法,首次评估了污泥样品的主要水物理和技术特性,包括保水曲线,比表面积,水电导率,电导率,收缩过程中的孔隙率动态,水的产量等。 ,它们被用于当前的水传递模型以及这些在真实热力学条件下的类土壤物体的行为。从理论上解释了在钻井废物存储过程中污泥自发膨胀的技术不利现象。使用HYDRUS-1D模型分析了在自由重力流出和水从地表永久蒸发下均匀的0.5 m厚的钻井污泥层的水状态。污泥的高保水能力,低水电导率和水产率不能使其在潮湿的气候条件下干燥到陆地植物可接受的三相状态(随着空气的进入),这解释了污泥坑的自发转变仅限于水形生态系统。 DOI:10.1134 / S1064229311020128

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