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Removal of Carbon Tetrachloride from a Layered Porous Medium by Means of Soil Vapor Extraction Enhanced by Desiccation and Water Table Reduction

机译:通过脱水和减少地下水位促进土壤蒸汽萃取从层状多孔介质中去除四氯化碳

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A two-dimensional flow cell experiment was conducted to study the removal of the carbon tetrachloride component of a DNAPL mixture from a layered porous medium through soil vapor extraction (SVE) with moist and dry air. A dual-energy radiation system was used at various times to non-intrusively determine fluid saturations. The mixture, which contained the volatile organic carbon tetrachloride, mimics the DNAPL disposed at the Hanford Site in Washington State. The flow cell, which is 100 cm long, 75 cm high and 5.5 cm wide, was packed with two sloped coarse sand and two sloped silt layers in an otherwise uniform matrix of medium-grained sand. A V-shaped fine sand layer was placed at the bottom of the flow cell to prevent DNAPL from exiting the flow cell. The water table was located 2 cm from the bottom, creating variably saturated conditions. A 500-mL spill was introduced at the top of the flow cell from a small source area. It was observed that the DNAPL largely by-passed the silt layers but easily moved into the coarse sand layers. Residual DNAPL was formed in the medium-grained sand matrix. The DNAPL caused a distinct reduction of the capillary fringe. Most of the DNAPL ended up in a pool on top of the V-shaped fine sand. Through four treatments with moist air soil vapor extraction, most residual carbon tetrachloride was removed from the medium-grained matrix and the coarse sand layers. However, soil vapor extraction with moist air was not able to remove the carbon tetrachloride from the silt layers and the pool. Through a water table reduction and subsequent soil vapor extraction with dry air, the carbon tetrachloride in the silt layers and the pool was effectively removed. Based on measurements and carbon tetrachloride vapor concentration data, it was estimated that after the final remediation treatment, almost 90% of the total mass was removed.
机译:进行了二维流动池实验,研究了 通过土壤蒸汽萃取从层状多孔介质中去除DNAPL 混合物中四氯化碳成分的方法 (SVE)潮湿干燥的空气中。在不同时间使用双能量辐射系统 来非侵入性地确定流体 的饱和度。该混合物包含挥发性有机四氯化碳,模仿了位于华盛顿州汉福德 站点的DNAPL。流通池长100厘米,高 75厘米,宽5.5厘米,在原本均匀的基质中装有两个倾斜的粗 沙和两个倾斜的淤泥层。 sup> 中等粒度的沙子。在流动池的底部放置了一个V型细砂层,以防止DNAPL离开流动池。地下水位位于距底部2 cm处, 产生了各种饱和条件。在流动池顶部从较小的源头区域引入了500 mL溢出物 观察到DNAPL在很大程度上绕过了淤泥层,但是 很容易移入了粗沙层。残留的DNAPL是在中粒砂基质中形成的。 DNAPL导致毛细条纹的 明显减少。大多数DNAPL 都终止在V型细砂顶部的水池中。通过 湿空气土壤蒸气抽提的四种处理,从中粒基质 和粗砂层中去除了大多数残留的 四氯化碳。但是,用 潮湿空气进行土壤蒸汽抽提不能从 淤泥层和水池中去除四氯化碳。通过减少地下水位 并随后用干燥空气提取土壤蒸汽,有效去除了淤泥层和水池中的四氯化碳 。根据测量结果和四氯化碳蒸气 的浓度数据,估计在最终的修复 处理后,将近90%的总质量被去除。 >

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  • 来源
    《Vadose Zone Journal》 |2005年第4期|1170-1182|共13页
  • 作者单位

    Environmental Technology Division, Pacific Northwest National Lab., P.O. Box 999, MS K9-33, Richland, WA 99354;

    Dep. of Agronomy and Soils, Auburn Univ., Auburn, AL 36849-5412;

    Environmental Molecular Sciences Lab., Pacific Northwest National Lab., P.O. Box 999, MS K8-96, Richland, WA 99354;

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