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Remediation of Historic Buildings and Patrimony by Bacterially Induced Mineralization

机译:细菌诱导矿化对历史建筑和遗产的修复

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Laboratory experiments were conducted to protect and consolidate historic architectural heritages by bacterially induced carbonate mineralization on the surface of samples of marble and concrete. Some properties of samples and mineral, such as the composition and growth of the mineral deposited on samples, porosity or pore size distribution of samples, the efficiency of protection, the bond behavior between the deposited mineral and substratum, were analyzed by Xray diffraction, scanning electron microscopy, mercury intrusion porosimetry and ultrasonic test. The results show that the phases of mineral crystal are calcite and vaterite, and the calcium source has an effect on the phase of calcium carbonate mineralization and precipitation. Bacteria act as nucleation sites in the course of precipitation of the mineral crystallization, and the crystal is deposited uniformly on the surface and subsurface of the matrix. The precipitation has no significant effect on the pore size distribution of the matrix, but results in a decrease of porosity, and mineral crystals are strongly attached to the substratum. Bacterial mineralization for remediation of historic buildings can be an ecological and novel alternative to traditional techniques.
机译:进行了实验室实验,以通过细菌诱导的大理石和混凝土样品表面的碳酸盐矿化作用来保护和巩固历史建筑遗产。通过X射线衍射,扫描仪分析了样品和矿物的一些特性,例如沉积在样品上的矿物的组成和生长,样品的孔隙率或孔径分布,保护效率,沉积的矿物与基质之间的键合行为。电子显微镜,压汞法和超声波测试。结果表明,矿物晶体的相为方解石和球v石,钙源对碳酸钙的矿化和析出相具有影响。细菌在矿物结晶沉淀过程中充当成核位点,并且晶体均匀地沉积在基质的表面和亚表面上。沉淀对基质的孔径分布没有明显影响,但会导致孔隙率降低,并且矿物晶体牢固地附着在基质上。修复历史建筑的细菌矿化可以是传统技术的一种生态和新颖的替代方法。

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