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首页> 外文期刊>Soils and foundations >EXPERIMENTAL STUDY OF LNAPL MIGRATION IN THE VICINITY OF A STEEP GROUNDWATER TABLE
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EXPERIMENTAL STUDY OF LNAPL MIGRATION IN THE VICINITY OF A STEEP GROUNDWATER TABLE

机译:陡峭地下水位附近的LNAPL迁移的实验研究

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Migration of Light Non-Aqueous Phase Liquids (LNAPLs) in porous soils was studied experimentally, using one-dimensional and two-dimensional laboratory tests. The movement of crude oil under constant pressure was observed in vertical and horizontal transparent columns filled with sand. It was found that in both cases the average oil saturation does not change during the oil propagation. Its value depends on the initial water saturation in sand and the mobility of air in front of the oil front. The hydraulic conductivity to oil was found to be constant along the vertical column, while it decreased exponentially when oil was spreading along the horizontal column. Two-dimensional experiments were carried out in a sand tank with simultaneous water flow and the oil migration. Oil leaked into the sand from a thin feeder above the water table with constant oil level. The experiments were conducted with three types of LNAPL: crude oil, vegetable oil, and engine oil. Evolution of the oil mound was recorded through the transparent front wall of the sand tank, while the water table was monitored using a series of piezometers. Presence of the water table had a major effect on the oil mound shape and size. Downwards movement of the oil front slowed down around the top of the capillary fringe and completely stopped near the water table. The depth of penetration into the capillary fringe depended on the oil viscosity and the pressure at the oil source. Lateral spreading was more pronounced in the direction of the water movement.
机译:使用一维和二维实验室测试,对轻质非水相液体(LNAPL)在多孔土壤中的迁移进行了实验研究。在充满沙子的垂直和水平透明柱中观察到了原油在恒定压力下的运动。已经发现,在两种情况下,平均油饱和度在油扩散期间均不改变。它的值取决于沙中的初始水饱和度和油层前方的空气流动性。发现对油的水力传导率沿垂直柱是恒定的,而当油沿水平柱散布时,它的渗透率呈指数下降。在沙箱中进行了二维实验,同时进行了水流和油的运移。油从恒定水位下的地下水位上方的细进料口漏入沙子。实验使用三种LNAPL类型进行:原油,植物油和发动机油。通过沙罐的透明前壁记录了油丘的演变,同时使用一系列的压力计监测了地下水位。地下水位的存在对油丘的形状和大小有重大影响。油前沿的向下运动在毛细管边缘顶部附近变慢,并在水位附近完全停止。渗透到毛细边缘的深度取决于油的粘度和油源的压力。横向扩散在水运动的方向上更为明显。

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