氧适应型混菌矿化调控混凝土裂缝自修复性能

Performance regulation of self-healing of cracks in concrete based on mineralization of oxygen-adaptive microbial consortia

  • 摘要: 为有效确保实际服役环境氧气浓度显著波动时混凝土裂缝自修复性能可控性,提出一种基于氧适应型混菌矿化调控的微生物自修复混凝土。首先开展氧适应型混菌矿化沉积效率测试,并设置4种实际服役环境氧气条件,考察氧环境波动下混凝土裂缝修复有效性;然后通过与好氧型混菌和纯菌对比,考察常态缺氧条件下混凝土裂缝自修复效果及其裂缝填充物微观形貌。试验结果表明:缺氧条件下氧适应型混菌呈现出更优异的矿化能力,矿化沉积量分别比好氧型混菌和纯菌高3.3倍和21.8倍;经缺氧修复56 d后,混凝土平均修复裂缝宽度和完全闭合率分别达0.48 mm和75.0%,裂缝修复效率较好氧型混菌和纯菌矿化分别提高40%和85%以上;与普通混凝土相比,该混菌对裂缝沿深度方向修复效果显著改善;裂缝填充物晶体为排列紧密均匀的规则块状方解石。

     

    Abstract: To ensure controllable crack-healing performance of concrete under significantly fluctuating oxygen concentrations in actual service environments, a bacteria-based self-healing concrete regulated by mineralization of oxygen-adaptive microbial consortia was proposed. The mineralization precipitation efficiency of oxygen-adaptive microbial consortia was first evaluated, and four oxygen conditions representing actual service environments were designed to examine the effectiveness of crack healing under oxygen fluctuations. Subsequently, by comparison with aerobic microbial consortia and pure culture, the crack-healing performance of concrete and the microstructure of crack-filling products under oxygen-deficient conditions were investigated. The test results show that the oxygen-adaptive microbial consortia exhibit markedly superior mineralization capacity under anaerobic conditions, with the precipitation mass being 3.3 times and 21.8 times higher than those of aerobic microbial consortia and pure culture, respectively. After 56 days of healing under oxygen-deficient conditions, the average values of healed crack widths and completely healed percentage reach 0.48 mm and 75.0%, representing improvements of over 40% and 85% compared with aerobic microbial consortia and pure culture, respectively. Compared with bacteria-free concrete, the oxygen-adaptive microbial consortia significantly improve the healing effectiveness of cracks along the depth direction. The crack-filling crystals are regular blocky calcite, densely and uniformly distributed.

     

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