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评估土壤质地对非饱和带中石油烃迁移和衰减影响的数值模拟。

Numerical modeling to assess the effect of soil texture on transport and attenuation of petroleum hydrocarbons in unsaturated zone.

作者信息

Srivastava Akanksha, Valsala Renu

机构信息

Department of Civil Engineering, IIT (ISM) Dhanbad, Dhanbad, Jharkhand, 826004, India.

出版信息

Environ Sci Pollut Res Int. 2023 Apr;30(16):46132-46146. doi: 10.1007/s11356-023-25557-w. Epub 2023 Jan 30.

DOI:10.1007/s11356-023-25557-w
PMID:36710315
Abstract

Soil texture in the unsaturated zone is a critical factor affecting the transport, accumulation, and attenuation rate of petroleum hydrocarbons (PHCs) in unsaturated conditions. The scope of this study is to investigate the soil texture impact on the fate of PHCs in unsaturated zones. The main objective is to formulate a coupled flow and multicomponent transport model for simulating the PHC plumes in various soil textures. Zeroth spatial moment (ZSM) of simulated PHC plumes is estimated to quantify the transient effect of soil textures on the dissolved PHC mass in the system. A BTEX (benzene, toluene, ethylbenzene, and xylene) spill is considered at the source zone for modeling. Simulations are carried out for clay, sand, and loam textures. The outcome of the study suggests that the infiltration rate in the unsaturated zone is minimal in clay texture. Wetting front depths and BTEX source depletion rates are found to be in the following order: clay < loam < sand. The migration depth of BTEX components in the sand texture is approximately twice the depth for clay and loam after 50 days. An increment in the BTEX source zone length by twofold enhances the dissolved BTEX mass in the unsaturated system by approximately 33% in all soil textures. Overall, the modeling and sensitivity studies conclude that the soil texture, vertical dispersivity, source zone length and composition, sorption characteristics, and volatility critically affect the depth and extent of BTEX migration in unsaturated zones.

摘要

非饱和带的土壤质地是影响石油烃(PHCs)在非饱和条件下运移、积累和衰减速率的关键因素。本研究的范围是调查土壤质地对非饱和带中PHCs归宿的影响。主要目标是建立一个耦合流和多组分传输模型,以模拟不同土壤质地中的PHC羽流。通过估计模拟的PHC羽流的零阶空间矩(ZSM)来量化土壤质地对系统中溶解的PHC质量的瞬态影响。在源区考虑了一次BTEX(苯、甲苯、乙苯和二甲苯)泄漏进行建模。对粘土、砂土和壤土质地进行了模拟。研究结果表明,粘土质地的非饱和带渗透速率最小。湿润锋深度和BTEX源消耗速率的顺序如下:粘土<壤土<砂土。50天后,砂土质地中BTEX组分的迁移深度约为粘土和壤土的两倍。在所有土壤质地中,将BTEX源区长度增加一倍可使非饱和系统中溶解的BTEX质量增加约33%。总体而言,建模和敏感性研究得出结论,土壤质地、垂直弥散度、源区长度和组成、吸附特性以及挥发性对非饱和带中BTEX迁移的深度和范围有至关重要的影响。

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