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微生物对scCO2-咸水-砂岩体系中矿物反应的影响
引用本文:张凤君,宋云鹏,钟爽,樊凯,李晨阳,张志勇.微生物对scCO2-咸水-砂岩体系中矿物反应的影响[J].中国环境科学,2019,39(1):281-289.
作者姓名:张凤君  宋云鹏  钟爽  樊凯  李晨阳  张志勇
作者单位:1. 吉林大学地下水资源与环境教育部重点实验室, 吉林 长春 130021; 2. 吉林建筑大学松辽流域水环境教育部重点实验室, 吉林 长春 130118; 3. 陕西省榆林市环境保护局, 陕西 榆林 719000; 4. 吉林省松原市前郭县环境保护局, 吉林 松原 138000
基金项目:国家自然科学基金资助项目(41472214)
摘    要:利用Illumina MiSeq对scCO2-咸水-砂岩体系中微生物16S rRNA基因V3-V4区进行分析,探究高压反应釜体系中微生物对scCO2的响应及微生物对矿物反应的作用.结果显示,生物量受pH值影响较大,初始pH值为7.02,生物量11.02×106gene/mL,30d时pH值降至5.65,生物量降至0.26×106gene/mL;随着矿物溶蚀,90d时pH值增至5.87,生物量增至4.61×106gene/mL.群落结构中,phylum Proteobacteria(52.60%(30d),55.34%(90d))与phylum Firmicutes(46.89%(30d),43.89%(90d))为优势菌门.在属水平,30,90d时Exiguobacterium,Citrobacter,Acinetobacter与Pseudomonas为优势菌属.产酸菌(Exiguobacterium,Acinetobacter与Pseudomonas)促进了长石与粘土溶蚀,咸水中K+,Na+,Ca2+,Mg2+,T-Fe浓度高于空白组;铁还原菌(Citrobacter)提高了Fe(Ⅱ)/Fe(Ⅲ)比值;微生物膜对Ca2+、Mg2+、Fe2+具有吸附作用.SEM结果显示,微生物介导下先于空白组出现菱铁矿沉淀.scCO2-咸水-砂岩体系中适应菌能促进矿物溶蚀与碳酸盐矿物捕获.

关 键 词:超临界CO2  土著微生物  矿物溶蚀  矿物捕获  
收稿时间:2018-05-21

Impact of microorganisms on the mineral interaction in scCO2-saline-sandstone system
ZHANG Feng-jun,SONG Yun-peng,ZHONG Shuang,FAN Kai,LI Chen-yang,ZHANG Zhi-yong.Impact of microorganisms on the mineral interaction in scCO2-saline-sandstone system[J].China Environmental Science,2019,39(1):281-289.
Authors:ZHANG Feng-jun  SONG Yun-peng  ZHONG Shuang  FAN Kai  LI Chen-yang  ZHANG Zhi-yong
Institution:1. Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China; 2. Key Laboratory of Songliao Aquatic Environment, Ministry of Education, Jilin Jianzhu University, Changchun 130118, China; 3. Yulin Environmental Protection Bureau, Shanxi Province, Yulin 719000, China; 4. Qianguo County Environmental Protection Bureau, Songyuan City, Jilin Province, Songyuan 138000, China
Abstract:Through the Illumina MiSeq analysis within V3-V4region of 16S rRNA gene, the response of microorganisms to scCO2 and its feedback on the mineral interaction in scCO2-saline-sandstone system was investigated. The results showed that biomass was affected by pH value. The initial pH was 7.02 and biomass was 11.02×106 gene/mL. And the pH dropped to 5.65 and biomass decreased to 0.26×106 gene/mL at 30th-day. However with the dissolution of minerals, the pH increased to 5.87 and biomass increased to 4.61×106 gene/mL at 90th-day. In the community structure, phylum Proteobacteria (52.60% (30d), 55.34% (90d)) and phylum Firmicutes (46.89% (30d), 43.89% (90d)) were dominant phylum. At the genus level, Exiguobacterium, Citrobacter, Acinetobacter and Pseudomonas were dominant genus at 30th and 90th-day. Acid-producing bacteria (Exiguobacterium, Acinetobactera and Pseudomonas) promoted the dissolution of feldspar and clay, and the concentrations of K+, Na+, Ca2+, Mg2+ and T-Fe were higher than those in blank group. Iron-reducing bacteria (Citrobacter) increased the ratio of Fe(Ⅱ)/Fe(Ⅲ). Biofilm showed an adsorption function of Ca2+, Mg2+ and Fe2+. At last, the SEM results showed that the micron-mediated precipitation of siderite appeared before the blank group. Therefore, the adaptable bacteria in the scCO2-salt-sandstone system could promote the mineral dissolution and carbonates capture.
Keywords:supercritical CO2  indigenous microorganisms  mineral corrosion  mineral trapping  
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