Mechanism of bacteria controlling gradient mineralization at surface layer of cement-based materials

C. Qian, Z. Hao, Xiaomeng Wang, Bin Xue
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Abstract

Microbial mineralization refers to the formation of inorganic minerals by action of microorganisms.1,2 The earliest study in this field could be traced back to the 19th century, where early aquatic and soil microbiologists carried out pioneering studies of non-medical microbial processes in soils, sediments and waters, opening the door to the empire of environmental microbiology, microbial ecology, geological microbiology and microbial geochemistry.3,4 In 1838, for the first time Ehrenberg5 explored the close relationship between ochre iron deposits in swamps and Gallionella ferruginea, investigating the important role of these bacteria in the formation of such sediments. In 1890, Muentz6 started to probe into the action process of bacteria in rock weathering and soil formation, which initiated the study of microbial weathering. Afterwards, Beijerinck7 discovered that microbes were involved in the oxidation and deposition of Mn in nature in 1931, who didn’t come singly but in pairs when Woksman8 reported that the microbial metabolites participated in geological processes, such as nitrifying bacteria, lichens, fungi and other acid-producing microorganisms in 1932. In many studies so far,9–11 it is believed that there are two main forms of microbial mineralization: one is BIM (bacteria-induced mineralization), generally nucleate and grow out of cells. The metabolites secreted by organisms are transported to the extracellular and react with ions and compounds in the environment, causing changes in pH-Eh in the solution or environment, leading to mineral deposition. The second is BCM (bacteria-controlled mineralization). Microorganism cells determine the form of mineral formation.12,13 In BCM, minerals are usually deposited inside the organic matrix or vesicles of biological cells, allowing organisms to control the nucleation and growth of minerals significantly, thus influencing the composition and size of mineralization. In cementbased materials, microbial mineralization is mainly used to repair cracks.14 In this study, the mechanism of microbial mineralization in the pores of cement-based materials and its effects on the pore structure were identified by the help of a numerical simulation of gradient mineralization.
细菌控制水泥基材料表层梯度矿化的机理
微生物矿化是指微生物作用下无机矿物的形成。1,2这一领域最早的研究可以追溯到19世纪,早期的水生和土壤微生物学家对土壤、沉积物和水中的非医用微生物过程进行了开创性的研究,打开了通往环境微生物学、微生物生态学、地质微生物学和微生物地球化学帝国的大门。3,4 1838年,Ehrenberg5首次探索了沼泽中赭石铁矿与铁Gallionella ferruginea之间的密切关系,研究了这些细菌在形成这种沉积物中的重要作用。1890年,Muentz6开始探索细菌在岩石风化和土壤形成中的作用过程,开创了微生物风化的研究。之后,beijerinck(7)在1931年发现微生物参与了自然界中Mn的氧化和沉积,当沃克斯曼(8)在1932年报道微生物代谢物参与地质过程时,它们不是单独出现的,而是成对出现的,如硝化细菌、地衣、真菌和其他产酸微生物。在目前的许多研究中,9-11认为微生物矿化主要有两种形式:一种是BIM(细菌诱导矿化),一般为成核并从细胞中生长出来。生物体分泌的代谢物被运输到细胞外,与环境中的离子和化合物发生反应,引起溶液或环境中pH-Eh的变化,导致矿物质沉积。二是细菌控制矿化(BCM)。微生物细胞决定矿物形成的形式。12,13在BCM中,矿物通常沉积在生物细胞的有机基质或囊泡内,使生物能够显著控制矿物的成核和生长,从而影响矿化的组成和大小。在水泥基材料中,微生物矿化主要用于修补裂缝本研究通过梯度矿化数值模拟,研究了水泥基材料孔隙中微生物矿化的机理及其对孔隙结构的影响。
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