航空煤油污染含水层反应运输模拟

E. Teramoto, H. K. Chang, Marcus Paulus Martins Bressa, Adriano Soriano
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引用次数: 0

摘要

自20世纪70年代以来,一直在研究天然细菌生物降解地下碳氢化合物的能力,因为这类污染物可能对人类健康构成严重威胁。了解控制碳氢化合物生物降解的机制是污染地区管理的关键问题。因此,研究人员对反应性输运进行了数值模拟,以评估概念地球化学模型,并帮助了解受大型航空燃料污染的红土含水层中BTEX生物降解的机制。利用反应输运模型评价了地球化学分带与BTEX矿化及次生反应联系的概念模型的可行性。当pco2固定且溶解氧(由于被困空气的传质而可能存在)在模型中被考虑时,所研究的烃类污染含水层的模拟化学形态的表示得到了最好的支持。这些发现表明,在涉及碳氢化合物生物降解的反应输运模型中,需要考虑这两个限制。
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Simulações de transporte reativo em um aquífero contaminado por querosene de aviação
The ability of native bacteria to biodegrade subsurface hydrocarbons has been studied consistently since the 1970s, since this class of contaminants may pose severe human health risks. Understanding the mechanisms that govern hydrocarbons biodegradation represents a crucial issue for the management of contaminated areas. For this reason, numerical simulations of reactive transport were performed to evaluate the conceptual geochemical model and to helpunderstand the mechanisms that govern BTEX biodegradation in a lateritic aquifer contaminated by large aviation fuel. The feasibility of previously proposed conceptual model linking geochemical zonation with BTEX mineralization and secondary reactions was evaluated by means of reactive transport models. The representation of the simulated chemical speciation of the studied hydrocarbon-contaminated aquifer is best supported when PCO 2 is fixed and dissolved oxygen, potentially present due to mass transfer from entrapped air, is considered in the model. These findings suggest the need for both constraints to be considered in the reactive transport models involving hydrocarbon biodegradation.
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16 weeks
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