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首页> 外文期刊>Applied and Environmental Microbiology >Kinetics of Manganese Oxidation by Cell-Free Extracts of Bacteria Isolated from Manganese Concretions from Soil
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Kinetics of Manganese Oxidation by Cell-Free Extracts of Bacteria Isolated from Manganese Concretions from Soil

机译:从土壤中锰提取物中分离出的细菌的无细胞提取物氧化锰的动力学

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A study of the kinetics of Mn2+ oxidation catalyzed by cell extracts of two bacterial isolates (E1, Pseudomonas III [new isolate] and E4, Citrobacter freundii) isolated from the core of manganese concretions from Greek soils is presented. The reaction velocity of Mn2+ oxidation was determined from the rate of consumption of Mn2+. The oxidation of Mn2+ was followed by measuring changes in Mn2+ concentration by activation analysis and by atomic absorption spectrophotometry. The reaction velocity was directly proportional to cell extract concentration when the reaction time was 1 h. At longer reaction times, the relationship deviated from linearity because substrate concentration became limiting. The rate of Mn2+ oxidation increased with the Mn2+ concentration. Analysis of the results by application of the integrated Michaelis equation for determining Michaelis constants and maximal velocities either in the presence (Km = 3.33 μmol/ml and Vmax = 1.25 μmol/ml·h) or in the absence of maleate buffer (Km = 2.52 μmol/ml and Vmax = 2.04 μmol/ml·h) indicated a strong affinity between the oxidizing system and manganese. All results in this study are consistent with an enzymatic manganese-oxidizing system and give an indication of the mechanism of biological Mn2+ oxidation in soil which differs from that in the marine environment.
机译:本文研究了从希腊土壤中的锰结石核心分离出的两种细菌分离物(E1,假单胞菌III [新分离物]和E4,弗氏柠檬酸杆菌)的细胞提取物催化的Mn2 +氧化动力学。由Mn 2+的消耗速度确定Mn 2+氧化的反应速度。 Mn2 +的氧化之后,通过活化分析和原子吸收分光光度法测量Mn2 +浓度的变化。当反应时间为1小时时,反应速度与细胞提取物浓度成正比。在更长的反应时间下,由于底物浓度变得有限,该关系偏离了线性。 Mn2 +的氧化速率随Mn2 +浓度的增加而增加。通过在存在(Km = 3.33μmol/ ml和Vmax = 1.25μmol/ ml·h)或不存在马来酸盐缓冲液(Km = 2.52)的情况下,使用积分Michaelis方程确定Michaelis常数和最大速度来分析结果μmol/ ml和Vmax = 2.04μmol/ ml·h)表示氧化体系与锰之间具有很强的亲和力。这项研究的所有结果均与酶促锰氧化系统一致,并表明了土壤中Mn2 +的生物氧化机制与海洋环境中的氧化机制不同。

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