地学前缘 ›› 2024, Vol. 31 ›› Issue (1): 467-485.DOI: 10.13745/j.esf.sf.2024.1.19
董海良1,2(), 曾强1,2, 刘邓3, 盛益之1, 刘晓磊1,4, 刘源1,2, 胡景龙1,2, 李扬1,2, 夏庆银5, 李润洁1,6, 胡大福1,2, 张冬磊1,6, 张文慧1,6, 郭东毅1,2, 张晓文1,2
收稿日期:
2023-12-05
修回日期:
2024-01-14
出版日期:
2024-01-25
发布日期:
2024-01-25
作者简介:
董海良(1965—),男,教授,博士生导师,主要从事矿物学、地质微生物学研究。E-mail: dongh@cugb.edu.cn
基金资助:
DONG Hailiang1,2(), ZENG Qiang1,2, LIU Deng3, SHENG Yizhi1, LIU Xiaolei1,4, LIU Yuan1,2, HU Jinglong1,2, LI Yang1,2, XIA Qingyin5, LI Runjie1,6, HU Dafu1,2, ZHANG Donglei1,6, ZHANG Wenhui1,6, GUO Dongyi1,2, ZHANG Xiaowen1,2
Received:
2023-12-05
Revised:
2024-01-14
Online:
2024-01-25
Published:
2024-01-25
摘要:
黏土矿物与微生物在自然环境中广泛共存。二者之间的相互作用影响着环境中的能量流动与元素循环。黏土矿物能够给微生物提供物理或化学保护,提高微生物对外界胁迫和干扰的抵抗能力。黏土矿物同时还能给微生物提供营养元素,促进其新陈代谢过程。黏土矿物中的结构铁是微生物铁氧化还原循环的重要电子供/受体。在氧化还原的环境中,多种铁还原/铁氧化细菌可以通过还原氧化黏土矿物中的结构Fe(III)/Fe(II),进而获得能量进行生长。在氧化还原过程中,微生物也可以通过溶解、转化、沉淀等作用改变黏土矿物的晶格结构及物相,或是产生新的次生矿物。黏土矿物-微生物相互作用在碳、氮、硅、磷等重要生命元素的地球化学循环中扮演着重要角色。黏土矿物可以通过吸附有机碳,降低有机碳的生物可利用性,减缓其矿化速率。在氧化还原波动的环境中,黏土矿物还可以通过活化分子氧,产生强氧化性自由基氧化降解有机质,提高其生物可利用性。黏土矿物还会吸附生物胞外酶,影响胞外酶降解有机质的效率。微生物通过耦合黏土矿物中铁氧化与硝酸盐还原,铁还原与氨氧化等过程影响氮循环。黏土矿物对磷的吸附以及风化过程中硅的释放影响着微生物的代谢活性。黏土矿物-微生物相互作用在重金属固化稳定、有机污染物降解、杀死病原菌等方面也有广泛的应用。
中图分类号:
董海良, 曾强, 刘邓, 盛益之, 刘晓磊, 刘源, 胡景龙, 李扬, 夏庆银, 李润洁, 胡大福, 张冬磊, 张文慧, 郭东毅, 张晓文. 黏土矿物-微生物相互作用机理以及在环境领域中的应用[J]. 地学前缘, 2024, 31(1): 467-485.
DONG Hailiang, ZENG Qiang, LIU Deng, SHENG Yizhi, LIU Xiaolei, LIU Yuan, HU Jinglong, LI Yang, XIA Qingyin, LI Runjie, HU Dafu, ZHANG Donglei, ZHANG Wenhui, GUO Dongyi, ZHANG Xiaowen. Interactions between clay minerals and microbes: Mechanisms and applications in environmental remediation[J]. Earth Science Frontiers, 2024, 31(1): 467-485.
图2 有(B)或无(A)电子穿梭体条件下微生物还原含铁黏土矿物的电子传递方向模式图(注:T,四面体;O,八面体)
Fig.2 Electron transfer directions during microbial reduction of structural iron in clay minerals with (B) or without (A) electron shuttle. T, tetrahedron; O, octahedron.
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