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具有复杂污染历史场地中控制底土非均质性的孔隙水污染物质量和微生物多样性。

Subsoil heterogeneities controlling porewater contaminant mass and microbial diversity at a site with a complex pollution history.

机构信息

Departamento de Gequímica, Petrologia i Prospecció Geològica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.

出版信息

J Contam Hydrol. 2013 Jan;144(1):1-19. doi: 10.1016/j.jconhyd.2012.10.009. Epub 2012 Oct 23.

Abstract

This study seeks to improve our understanding of the conceptual model of pollutant transport and fate in cases of DNAPL contamination at sites with a complex contamination history. The study was carried out in an unconfined aquifer of alluvial fans in the Tarragona Petrochemical Complex (Spain). Two boreholes were drilled and continuous cores were recovered in order to carry out a detailed core description at centimeter scale and a comprehensive sampling of borehole cores. The biogeochemical heterogeneity at these sites is controlled by the conjunction of lithological, hydrochemical and microbiological heterogeneities. Biodegradation processes of contaminant compounds take place not only at the level of the dissolved fraction in the aquifer but also at the level of the fraction retained in the fine, less conductive materials as shown by the biodegradation haloes of parent and metabolite compounds. Sampling the low-conductivity levels also allowed us to identify compounds, e.g. BTEX, that are the remaining traces of the passage of old contaminant plumes whose sources no longer exist. This enabled us to describe past biogeochemical processes and to partially account for the processes occurring today. Transition zones, characterized by numerous textural changes, constitute ecotones whose biostimulation could be effective in promoting the acceleration of the remediation of the multiple pollution at these sites.

摘要

本研究旨在增进我们对具有复杂污染历史的场址中,DNAPL 污染情况下污染物迁移和归宿概念模型的理解。该研究在西班牙塔拉戈纳石化综合体(Tarragona Petrochemical Complex)的冲积扇非承压含水层中进行。钻取了两口井,并回收了连续岩心,以便在厘米尺度上进行详细的岩心描述,并对井中岩心进行全面采样。这些地点的生物地球化学非均质性受岩性、水文化学和微生物异质性的共同控制。污染物化合物的生物降解过程不仅发生在含水层中溶解部分的水平,也发生在保留在细粒、低导性物质中的部分,这一点可从母体和代谢物化合物的生物降解晕圈中看出。对低电导率水平的采样还使我们能够识别出一些化合物,如 BTEX,它们是旧污染物羽流残留的痕迹,而这些羽流的源头已经不存在了。这使我们能够描述过去的生物地球化学过程,并部分解释今天正在发生的过程。以众多纹理变化为特征的过渡带构成了生态过渡带,其生物刺激作用可能有助于加速这些地点的多种污染的修复。

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