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建立模型量化土壤湿度对基底蒸气浓度的影响。

Modeling quantification of the influence of soil moisture on subslab vapor concentration.

机构信息

School of Engineering, Brown University, Providence, RI 02912, USA.

出版信息

Environ Sci Process Impacts. 2013 Jul;15(7):1444-51. doi: 10.1039/c3em00225j.

DOI:10.1039/c3em00225j
PMID:23752876
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3756691/
Abstract

The U.S. EPA has developed a database of field data obtained from vapor intrusion sites throughout the United States. Large variations in reported subsurface contaminant vapor concentration ratios (e.g. building subslab to groundwater source) present challenges for the analysis of subsurface vapor transport processes. Meanwhile, numerical models have been used by the U.S. EPA and others to describe the transport processes governing vapor intrusion. The influence of the capillary fringe has often been ignored in these models. In this manuscript, the influence of soil moisture content on the subslab vapor concentration is analyzed in the context of mathematical models. Results are compared to those from other modeling methods that do not account for the soil moisture content. The slab capping effect is observed to interact with the effect of soil moisture in determining the subslab contaminant vapor concentration. The slab capping effect is observed to be significant when the building-source separation distance is less than half of the slab size.

摘要

美国环保署(EPA)开发了一个数据库,其中包含了全美各地蒸气入侵地点的现场数据。报告的地下污染物蒸气浓度比(例如,建筑物地下室与地下水源)存在很大差异,这给地下蒸气运移过程的分析带来了挑战。同时,美国环保署和其他机构也使用数值模型来描述控制蒸气入侵的传输过程。这些模型往往忽略了毛细边界层的影响。在本文中,从数学模型的角度分析了土壤湿度对地下室蒸气浓度的影响。将结果与不考虑土壤湿度的其他建模方法进行了比较。观察到板盖效应与土壤湿度的相互作用,从而确定了地下室污染物蒸气浓度。当建筑物与源之间的距离小于板尺寸的一半时,板盖效应明显。

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本文引用的文献

1
Estimation of Contaminant Subslab Concentration in Vapor Intrusion Including Lateral Source-Building Separation.考虑侧向源与建筑物间距的蒸汽入侵中污染物地下浓度估算
Vadose Zone J. 2013 Aug;12(3). doi: 10.2136/vzj2012.0157.
2
Influence of Soil Moisture on Soil Gas Vapor Concentration for Vapor Intrusion.土壤湿度对土壤气体蒸汽浓度的影响及蒸汽侵入
Environ Eng Sci. 2013 Oct;30(10):628-637. doi: 10.1089/ees.2013.0133.
3
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