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在 CO2 胁迫下希瓦氏菌 MR-1 的生存能力和金属还原作用:对地质 CO2 封存中 CO2 泄漏的生态影响的启示。

Viability and metal reduction of Shewanella oneidensis MR-1 under CO2 stress: implications for ecological effects of CO2 leakage from geologic CO2 sequestration.

机构信息

Department of Energy, Environmental and Chemical Engineering, Washington University, St. Louis, Missouri 63130, United States.

出版信息

Environ Sci Technol. 2010 Dec 1;44(23):9213-8. doi: 10.1021/es102299j. Epub 2010 Nov 8.

DOI:10.1021/es102299j
PMID:21058700
Abstract

To study potential ecological impacts of CO(2) leakage to shallow groundwater and soil/sediments from geologic CO(2) sequestration (GCS) sites, this work investigated the viability and metal reduction of Shewanella oneidensis MR-1 under CO(2) stress. While MR-1 could grow under high-pressure nitrogen gas (500 psi), the mix of 1% CO(2) with N(2) at total pressures of 15 or 150 psi significantly suppressed the growth of MR-1, compared to the N(2) control. When CO(2) partial pressures were over 15 psi, the growth of MR-1 stopped. The reduced bacterial viability was consistent with the pH decrease and cellular membrane damage under high pressure CO(2). After exposure to 150 psi CO(2) for 5 h, no viable cells survived, the cellular contents were released, and microscopy images confirmed significant cell structure deformation. However, after a relatively short exposure (25 min) to 150 psi CO(2), MR-1 could fully recover their growth within 24 h after the stress was removed, and the reduction of MnO(2) by MR-1 was observed right after the stress was removed. Furthermore, MR-1 survived better if the cells were aggregated rather than suspended, or if pH buffering minerals, such as calcite, were present. To predict the cell viability under different CO(2) pressures and exposure times, a two-parameter mathematical model was developed.

摘要

为了研究地质封存(GCS)场地 CO2 泄漏对浅层地下水和土壤/沉积物的潜在生态影响,本研究调查了 Shewanella oneidensis MR-1 在 CO2 胁迫下的生存能力和金属还原能力。虽然 MR-1 可以在高压氮气(500 psi)下生长,但在总压力为 15 或 150 psi 的 1% CO2 与 N2 的混合物中,与 N2 对照相比,MR-1 的生长受到显著抑制。当 CO2 分压超过 15 psi 时,MR-1 的生长停止。减少的细菌活力与高压 CO2 下的 pH 值下降和细胞膜损伤一致。暴露于 150 psi CO2 5 小时后,没有存活的细胞,细胞内容物被释放,显微镜图像证实了细胞结构的显著变形。然而,在暴露于 150 psi CO2 25 分钟后,MR-1 可以在去除压力后 24 小时内完全恢复生长,并且在去除压力后立即观察到 MR-1 对 MnO2 的还原。此外,如果细胞聚集而不是悬浮,或者存在碳酸钙等 pH 缓冲矿物质,MR-1 的存活率更高。为了预测不同 CO2 压力和暴露时间下的细胞活力,开发了一个双参数数学模型。

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