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微生物诱导碳酸盐岩沉淀过程及作用机理

高旭波 潘振东 龚培俐 江玉 李成城 李鸿煜

高旭波,潘振东,龚培俐,等. 微生物诱导碳酸盐岩沉淀过程及作用机理[J]. 中国岩溶,2022,41(3):441-452 doi: 10.11932/karst20220311
引用本文: 高旭波,潘振东,龚培俐,等. 微生物诱导碳酸盐岩沉淀过程及作用机理[J]. 中国岩溶,2022,41(3):441-452 doi: 10.11932/karst20220311
GAO Xubo, PAN Zhendong, GONG Peili, JIANG Yu, LI Chengcheng, LI Hongyu. Process and mechanism of microbial induced carbonate precipitation[J]. CARSOLOGICA SINICA, 2022, 41(3): 441-452. doi: 10.11932/karst20220311
Citation: GAO Xubo, PAN Zhendong, GONG Peili, JIANG Yu, LI Chengcheng, LI Hongyu. Process and mechanism of microbial induced carbonate precipitation[J]. CARSOLOGICA SINICA, 2022, 41(3): 441-452. doi: 10.11932/karst20220311

微生物诱导碳酸盐岩沉淀过程及作用机理

doi: 10.11932/karst20220311
基金项目: 国家自然科学基金项目:地下水系统中碳酸盐岩体系—砷相互作用研究(41877204);国家自然科学基金青年基金项目:人类活动影响下富钙高氟地下水中氟—钙拮抗的环境生物地球化学过程研究(41902265)
详细信息
    作者简介:

    高旭波(1975—),男,研究员,长期从事岩溶及地下水水资源与水环境污染防治工作。Email: xubo.gao.cug@gmail.com; xubo.gao.cug@gmail.com

  • 中图分类号: X141;P593

Process and mechanism of microbial induced carbonate precipitation

  • 摘要: 微生物诱导碳酸钙沉淀(microbially induced calcium carbonate precipitation, MICP)是一种在自然界中广泛存在的生物矿化过程。由于MICP具有反应速度快、环境条件要求低、应用范围广、温室气体减排效应显著等特点,在地质、土木、水利、环境多个领域中广泛推广应用。文章在分析国内外相关研究成果的基础上,归纳整理出反硝化过程、硫酸盐还原作用、尿素分解作用等多种微生物诱导下碳酸钙矿化途径和作用机制。以尿素分解菌为代表,重点讨论微生物诱导碳酸盐沉淀过程中pH、温度、离子浓度等环境因素对生成矿物晶型晶貌等方面的影响,总结了MICP的环境应用机制,即环境中的重金属元素通过替换作用替换矿化矿物中的Ca2+或CO32−从而被固定。MICP作为一种简单高效的地质环境过程,在生态环境修复领域具有广阔的应用前景。

     

  • 图  1  反硝化诱导碳酸钙沉淀

    Figure  1.  Calcium carbonate precipitation induced by denitrification

    图  2  硫酸盐还原诱导碳酸钙沉淀

    Figure  2.  Calcium carbonate precipitation induced by sulfate reduction

    图  3  光合作用概念模型图

    Figure  3.  Conceptual model diagram of photosynthesis

    图  4  甲烷氧化概念模型图 [13]

    Figure  4.  Conceptual model diagram of methane oxidation [13]

    图  5  尿素分解菌诱导生成碳酸钙概念模型图

    Figure  5.  Conceptual model diagram of calcium carbonate induced by urea decomposing bacteria

    图  6  阳离子型矿化过程示意图

    Figure  6.  Schematic diagram of cationic mineralization process

    图  7  重金属置换矿化过程示意图

    Figure  7.  Schematic diagram of heavy metal replacement mineralization process

    表  1  尿素分解菌MICP固定阳离子型重金属表

    Table  1.   Cationic heavy metals fixed by urea decomposing bacteria MICP

    重金属类型细菌名称固定率/%文献
    Cd 贪铜菌属
    芽孢杆菌属
    芽孢杆菌属
    芽孢杆菌属
    贪铜菌属
    芽孢杆菌属
    芽孢杆菌属
    芽孢杆菌属
    80.10
    72.64
    76.70
    73.40
    53.30(土壤)
    35.33(土壤)
    42.54(土壤)
    53.80(土壤)
    [44]
    嗜根寡养单胞菌
    孟氏假单胞菌
    八叠球菌
    71.30
    71.30
    97.15
    [45]
    蜡样芽胞杆菌 60.72 [46]
    绿芽胞杆菌
    沙棘绿杆菌
    阴沟肠杆菌
    85.40 [45]
    Ni 蜡样芽胞杆菌 95.78(土壤) [47]
    球孢子孢菌
    巴氏芽孢八叠球菌UR53
    巴氏芽孢八叠球菌UR31
    蜡样芽胞杆菌UR41
    88~99
    88~99
    88~99
    88~99
    [48]
    Pb 芽孢杆菌 26 [49]
    嗜根寡养单胞菌(A323)
    孟氏假单胞菌(C113)
    96.25
    95.93
    [45]
    阴沟肠杆菌 60 [50]
    蜡样芽孢杆菌 85 [51]
    Pb 产黄青霉(真菌) 98.80 [52]
    镰刀菌(真菌)
    曲霉菌(真菌)
    48
    34
    [53]
    Zn 嗜根寡养单胞菌
    孟氏假单胞菌
    八叠球菌
    63.91
    73.81
    94.83
    [45]
    Cu 考克氏菌
    考克氏菌
    97
    95(土壤)
    [54]
    巴氏芽孢杆菌 10 [55]
    贪铜菌 97.7 [56]
    下载: 导出CSV

    表  2  MICP固定阴离子型重金属表

    Table  2.   Table of anionic heavy metals fixed by MICP

    (类)重金属类型细菌名称固定率文献
    As地衣芽孢杆菌100%(As5+)初始浓度3 mmol·L−1
    60%(As5+)初始浓度5 mmol·L−1
    35%(As5+)初始浓度7 mmol·L−1
    100%(As3+)初始浓度1 mmol·L−1
    95%(As3+)初始浓度3 mmol·L−1
    58%(As3+)初始浓度5 mmol·L−1
    [57]
    芽孢八叠球菌96.6%(土壤)[58]
    地衣芽孢杆菌生成1 053 mg/kg的固相(不加Mg)
    生成1 381 mg/kg的固相(加Mg)
    [59]
    Cr产黄青霉菌(真菌)95.30%[52]
    芽孢杆菌98%[60]
    表皮葡萄球菌76.80%[61]
    下载: 导出CSV
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  • 收稿日期:  2022-01-30
  • 刊出日期:  2022-06-25

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