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微生物加速碳酸盐矿物沉淀作为原位碳封存和石棉矿山场地修复的策略。

Microbially Accelerated Carbonate Mineral Precipitation as a Strategy for in Situ Carbon Sequestration and Rehabilitation of Asbestos Mine Sites.

机构信息

School of Earth Sciences, The University of Queensland , Saint Lucia, Queensland 4072, Australia.

School of Earth, Atmosphere and Environment, Monash University , Clayton, Melbourne, Victoria 3800, Australia.

出版信息

Environ Sci Technol. 2016 Feb 2;50(3):1419-27. doi: 10.1021/acs.est.5b04293. Epub 2016 Jan 19.

Abstract

A microbially accelerated process for the precipitation of carbonate minerals was implemented in a sample of serpentinite mine tailings collected from the abandoned Woodsreef Asbestos Mine in New South Wales, Australia as a strategy to sequester atmospheric CO2 while also stabilizing the tailings. Tailings were leached using sulfuric acid in reaction columns and subsequently inoculated with an alkalinity-generating cyanobacteria-dominated microbial consortium that was enriched from pit waters at the Woodsreef Mine. Leaching conditions that dissolved 14% of the magnesium from the serpentinite tailings while maintaining circumneutral pH (1800 ppm, pH 6.3) were employed in the experiment. The mineralogy, water chemistry, and microbial colonization of the columns were characterized following the experiment. Micro-X-ray diffraction was used to identify carbonate precipitates as dypingite [Mg5(CO3)4(OH)2·5H2O] and hydromagnesite [Mg5(CO3)4(OH)2·4H2O] with minor nesquehonite (MgCO3·3H2O). Scanning electron microscopy revealed that carbonate mineral precipitates form directly on the filamentous cyanobacteria. These findings demonstrate the ability of these organisms to generate localized supersaturating microenvironments of high concentrations of adsorbed magnesium and photosynthetically generated carbonate ions while also acting as nucleation sites for carbonate precipitation. This study is the first step toward implementing in situ carbon sequestration in serpentinite mine tailings via microbial carbonate precipitation reactions.

摘要

采用微生物加速碳酸盐水矿沉淀的方法对从澳大利亚新南威尔士州废弃的伍兹克里夫石棉矿采集的蛇纹岩尾矿样本进行了实验,该方法既可以封存大气 CO2,又可以稳定尾矿。在反应柱中用硫酸浸取尾矿,然后用从伍兹克里夫矿坑水中富集的产碱蓝细菌占优势的微生物共生体进行接种。实验中采用的浸取条件是在维持近中性 pH 值(1800 ppm,pH 值 6.3)的情况下,从蛇纹岩尾矿中溶解 14%的镁。实验结束后,对柱体的矿物学、水化学和微生物定殖情况进行了表征。微 X 射线衍射用于鉴定碳酸盐沉淀物为纤铁矿[Mg5(CO3)4(OH)2·5H2O]和水羟镁石[Mg5(CO3)4(OH)2·4H2O],并有少量水菱镁矿(MgCO3·3H2O)。扫描电子显微镜显示,碳酸盐矿物沉淀直接在丝状蓝细菌上形成。这些发现表明,这些生物能够在局部形成高浓度吸附镁和光合作用生成的碳酸根离子的过饱和微环境,同时也可以作为碳酸盐沉淀的成核点。本研究是通过微生物碳酸盐沉淀反应实现蛇纹岩尾矿原位碳封存的第一步。

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