首页> 外文期刊>Water, Air, and Soil Pollution >Evaluation of VOC fluxes at the soil-air interface using different flux chambers and a quasi-analytical approach
【24h】

Evaluation of VOC fluxes at the soil-air interface using different flux chambers and a quasi-analytical approach

机译:使用不同的通量室和拟分析方法评估土壤-空气界面的VOC通量

获取原文
获取原文并翻译 | 示例
       

摘要

Dense nonaqueous-phase liquids (DNAPLs) spilled on the soil migrate vertically depending upon gravity and capillary forces through the unsaturated zone of the porous aquifer, forming a vapour plume. These volatile organic compounds (VOCs) can be transferred by advection-diffusion to the groundwater or to the atmosphere. Evaluating DNAPL vapour fluxes at the soil-air interface is one of the key challenges in the remediation of contaminated sites. This work discusses the results of a large-scale vapour plume experiment with a well-defined trichloroethylene (TCE) spill, including a sequential raising and lowering of the water table, where the TCE vapour fluxes at the soil surface were experimentally quantified in two ways: (i) directly, with measurements at the soil-air interface using different flux chambers at various operational modes under both transient and steady-state conditions of the vapour plume, and (ii) indirectly, using a quasi-analytical approach based on soil gas measurements. It was shown that upward displacement of the water-air front during the controlled raising of the water table (approximately 10 cm h(-1)) increased the TCE vapour flux measured at the soil surface by factors of 4 to 10. Under steady-state transport conditions, TCE vapour fluxes measured using five types of flux chambers and three operational modes were similar. The effects of the flux chamber geometry, the accumulation of TCE vapours in the chamber head-space or the air recirculation at a low flow rate on the measured TCE vapour fluxes were low. At steady-state transport conditions, TCE vapour fluxes measured with the flux chambers and estimated using the quasi-analytical approach were of the same order of magnitude. However, under transient conditions of the vapour plume, the TCE vapour flux predicted by the quasi-analytical approach greatly underestimated or overestimated the real TCE vapour flux at the soil-air interface.
机译:洒在土壤上的稠密非水相液体(DNAPLs)根据重力和毛细作用力垂直迁移通过多孔含水层的不饱和区,从而形成蒸气羽流。这些挥发性有机化合物(VOC)可以通过对流扩散转移到地下水或大气中。评估土壤-空气界面处的DNAPL蒸气通量是修复污染场地的关键挑战之一。这项工作讨论了使用明确的三氯乙烯(TCE)溢漏进行的大规模蒸气羽流实验的结果,包括逐步升高和降低地下水位,其中以两种方式对土壤表面的TCE蒸气通量进行了实验量化:(i)直接进行,在蒸汽羽流的瞬态和稳态条件下,在各种操作模式下使用不同的通量室在土壤-空气界面处进行测量,以及(ii)使用基于土壤的准分析方法进行间接测量气体测量。结果表明,在受控升高地下水位(约10 cm h(-1))期间,水-空气前沿的向上位移使土壤表面测得的TCE蒸气通量增加了4到10倍。在运输条件下,使用五种类型的助焊剂室和三种操作模式测得的三氯乙烯(TCE)蒸气通量相似。助焊剂室几何形状,TCE蒸汽在室顶部空间的积聚或低流速的空气再循环对测量的TCE蒸汽通量的影响很小。在稳态运输条件下,用通量室测量并使用准分析方法估算的TCE蒸气通量处于相同数量级。但是,在蒸汽羽流的瞬态条件下,通过准分析方法预测的TCE蒸汽通量大大低估或高估了土壤-空气界面的实际TCE蒸汽通量。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号