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Enzyme kinetic characterization of microbe-produced urease for microbe-driven calcite mineralization

机译:用于微生物驱动方解石矿化的微生物产生的脲酶的酶动力学表征

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摘要

Just as calcite precipitation rate is equal to CO_3~(2-) formation rate, this CO_3~(2-) formation rate is equal to that of urea hydrolysis in microbial calcite precipitation. This formative rate of CO_3~(2-) evolved a mode to assay the urea hydrolysis rate, which was influenced by urea and Ca~(2+) concentrations, pH, and temperature. To contrive the highest V_(max) of the Michaelis-Menten enzyme kinetics equation for the fastest urea hydrolysis rate, 35 °C, pH 10, 2 M urea and 2 M Ca~(2+) were the optimal conditions based on the studies.
机译:就像方解石的沉淀速率等于CO_3〜(2-)的生成速率一样,此CO_3〜(2-)的生成速率等于微生物方解石沉淀中尿素水解的速率。 CO_3〜(2-)的形成速率形成了一种测定尿素水解速率的模式,该模式受尿素和Ca〜(2+)浓度,pH和温度的影响。为了使Michaelis-Menten酶动力学方程的最高V_(max)达到最快的尿素水解速率,基于这些研究,35°C,pH 10、2 M尿素和2 M Ca〜(2+)是最佳条件。

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