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针对地下汽油源的室内氧气受限生物降解的蒸汽侵入

Indoor vapor intrusion with oxygen-limited biodegradation for a subsurface gasoline source.

作者信息

DeVaull George E

机构信息

Shell Global Solution US Inc., Westhollow Technology Center, 3333 Highway Six South, Houston, Texas 77082, USA.

出版信息

Environ Sci Technol. 2007 May 1;41(9):3241-8. doi: 10.1021/es060672a.

Abstract

Development and results are presented for a subsurface soil to indoor air chemical vapor intrusion model that includes oxygen-limited biodegradation. The algebraic model incorporates a steady-state subsurface gasoline vapor source, diffusion-dominated soil vapor transport in a homogeneous subsurface soil layer, and mixing within a building enclosure. The soil is divided into a shallow aerobic layer including biodegradation and a deeper anaerobic layer in which biodegradation is neglected. Biodegradation of multiple chemicals is included, with aerobic first-order reaction kinetics estimated from measured data. Oxygen is supplied at the soil surface below the building foundation. Oxygen demand is attributed to a sum of multiple biodegrading chemicals and to baseline respiration of native soil organic matter. The model is solved by iteratively varying the aerobic depth to match oxygen demand to oxygen supply. Model results are calculated for ranges of source concentrations, unsaturated soil characteristics, and building parameters. Results indicate vapor intrusion of petroleum hydrocarbons can be significantly less than indicated by estimates that neglect biodegradation.

摘要

本文介绍了一个包含缺氧生物降解的地下土壤到室内空气化学物质侵入模型的开发及结果。该代数模型纳入了稳态地下汽油蒸汽源、均质地下土壤层中以扩散为主的土壤蒸汽传输以及建筑物围护结构内的混合过程。土壤被分为浅层好氧层(包括生物降解)和深层厌氧层(其中忽略生物降解)。模型考虑了多种化学物质的生物降解,好氧一级反应动力学由实测数据估算得出。氧气在建筑物基础下方的土壤表面供应。需氧量归因于多种生物降解化学物质的总和以及原生土壤有机质的基线呼吸作用。通过迭代改变好氧深度以使需氧量与供氧量相匹配来求解该模型。针对源浓度范围、非饱和土壤特性和建筑物参数计算了模型结果。结果表明,与忽略生物降解的估算相比,石油烃的蒸汽侵入量可能显著更低。

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