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UREOLYTIC CALCIUM CARBONATE PRECIPITATION IN THE PRESENCE OF NON-UREOLYTIC COMPETING BACTERIA

机译:存在非尿素竞争细菌时尿酸钙碳酸酯的沉淀

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Stimulation of ureolytic Microbially Induced CaCO3 Precipitation (MICP) innatural soils is likely to be affected by interactions between ureolytic and nonureolyticbacteria. In order to study these interactions we performed a MICPexperiment in artificial groundwater medium, inoculated with two model bacteria:Sporosarcina pasteurii and Bacillus subtilis, and supplemented with Nutrient Brothand 7 mM of urea. Control was inoculated with S. pasteurii. The experiment lasted10 days, during which ammonium, dissolved calcium, pH, dissolved inorganiccarbon (DIC) and optical density (OD) were measured.Results show that dissolved calcium was depleted at a higher rate in thepresence of non-ureolytic bacteria, despite lower pH and CO32- concentration. ODmeasurements show higher growth rate than in control samples. We suggest that thepresence of the non-ureolytic bacteria, B. subtilis, accelerates MICP process, throughthe addition of nucleation sites in the form of bacterial cells.
机译:刺激尿素分解微生物诱导的CaCO3沉淀(MICP) 天然土壤可能会受到溶尿和非溶尿之间相互作用的影响 细菌。为了研究这些相互作用,我们进行了MICP 在人工地下水介质中进行实验,接种了两种模型细菌: 巴斯德孢子菌和枯草芽孢杆菌,并辅以营养肉汤 和7毫米尿素。用巴氏链球菌接种对照。实验持续了 10天,在此期间,铵盐,溶解的钙,pH,溶解的无机盐 测定了碳(DIC)和光密度(OD)。 结果表明,溶解钙以较高的速度消耗。 尽管pH和CO3较低,但仍存在非溶尿细菌 2-浓度。外径 测量显示比对照样品更高的生长速率。我们建议 非溶尿细菌枯草芽孢杆菌的存在通过以下途径加速了MICP过程 以细菌细胞的形式添加成核位点。

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