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多孔介质中乙醇生物降解的复电阻率特征。

Complex resistivity signatures of ethanol biodegradation in porous media.

机构信息

Department of Earth and Environmental Sciences, Rutgers University, 101 Warren Street, Newark, NJ, 07102 USA.

出版信息

J Contam Hydrol. 2013 Oct;153:37-50. doi: 10.1016/j.jconhyd.2013.07.005. Epub 2013 Aug 1.

Abstract

Numerous adverse effects are associated with the accidental release of ethanol (EtOH) and its persistence in the subsurface. Geophysical techniques may permit non-invasive, real time monitoring of microbial degradation of hydrocarbon. We performed complex resistivity (CR) measurements in conjunction with geochemical data analysis on three microbial-stimulated and two control columns to investigate changes in electrical properties during EtOH biodegradation processes in porous media. A Debye Decomposition approach was applied to determine the chargeability (m), normalized chargeability (m(n)) and time constant (τ) of the polarization magnitude and relaxation length scale as a function of time. The CR responses showed a clear distinction between the bioaugmented and control columns in terms of real (σ') and imaginary (σ″) conductivity, phase (ϕ) and apparent formation factor (F(app)). Unlike the control columns, a substantial decrease in σ' and increase in F(app) occurred at an early time (within 4 days) of the experiment for all three bioaugmented columns. The observed decrease in σ' is opposite to previous studies on hydrocarbon biodegradation. These columns also exhibited increases in ϕ (up to ~9 mrad) and σ″ (up to two order of magnitude higher) 5 weeks after microbial inoculation. Variations in m and m(n) were consistent with temporal changes in ϕ and σ″ responses, respectively. Temporal geochemical changes and high resolution scanning electron microscopy imaging corroborated the CR findings, thus indicating the sensitivity of CR measurements to EtOH biodegradation processes. Our results offer insight into the potential application of CR measurements for long-term monitoring of biogeochemical and mineralogical changes during intrinsic and induced EtOH biodegradation in the subsurface.

摘要

大量的不良反应与乙醇(EtOH)的意外释放及其在地下环境中的持续存在有关。地球物理技术可能允许非侵入性、实时监测微生物对碳氢化合物的降解。我们在三个微生物刺激和两个对照柱上进行了复电阻率(CR)测量,并结合地球化学数据分析,以研究在多孔介质中 EtOH 生物降解过程中电特性的变化。采用 Debye 分解方法来确定极化幅度和弛豫长度尺度的荷质比(m)、归一化荷质比(m(n))和时间常数(τ)随时间的变化。CR 响应在生物增强柱和对照柱之间在实部(σ')和虚部(σ″)电导率、相位(ϕ)和表观形成因子(F(app))方面表现出明显的区别。与对照柱不同,所有三个生物增强柱在实验开始后的早期(4 天内),σ'显著降低,F(app)显著增加。与之前关于碳氢化合物生物降解的研究相反,观察到的σ'降低。这些柱在微生物接种后 5 周内还表现出ϕ(高达约 9 mrad)和σ″(高达两个数量级)的增加。m 和 m(n)的变化分别与ϕ和σ″响应的时间变化一致。时间地球化学变化和高分辨率扫描电子显微镜成像证实了 CR 结果,从而表明 CR 测量对 EtOH 生物降解过程的敏感性。我们的结果为 CR 测量在地下环境中内在和诱导 EtOH 生物降解过程中生物地球化学和矿物学变化的长期监测提供了新的见解。

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