Department of Microbiology and Public Health, Michigan State University, East Lansing, Michigan 48824.
Appl Environ Microbiol. 1982 Dec;44(6):1374-84. doi: 10.1128/aem.44.6.1374-1384.1982.
Michaelis-Menten kinetic parameters for H(2) consumption by three methanogenic habitats were determined from progress curve and initial velocity experiments. The influences of mass transfer resistance, endogenous H(2) production, and growth on apparent parameter estimates were also investigated. Kinetic parameters could not be determined for undiluted rumen fluid and some digestor sludge from gas-phase measurements of H(2), since mass transfer of H(2) across the gas-liquid interface was rate limiting. However, accurate values were obtained once the samples were diluted. H(2) consumption by digestor sludge with a long retention time and by hypereutrophic lake sediment was not phase transfer limited. The K(m) values for H(2) uptake by these habitats were similar, with means of 5.8, 6.0, and 7.1 muM for rumen fluid, digestor sludge, and sediment, respectively. V(max) estimates suggested a ratio of activity of approximately 100 (rumen fluid):10 (sludge):1 (sediment); their ranges were as follows: rumen fluid, 14 to 28 mM h; Holt sludge, 0.7 to 4.3 mM h; and Wintergreen sediment, 0.13 to 0.49 mM h. The principles of phase transfer limitation, studied here for H(2), are the same for all gaseous substrates and products. The limitations and errors associated with gas phase determination of kinetic parameters were evaluated with a mathematical model that combined mass transport and Michaelis-Menten kinetics. Three criteria are described which can be used to evaluate the possibility that a phase transfer limitation exists. If it does not exist, (i) substrate consumption curves are Michaelis-Menten and not first order, (ii) the K(m) is independent of initial substrate concentration, and (iii) the K(m) is independent of biomass (V(max)) and remains constant with dilution of sample. Errors in the Michaelis-Menten kinetic parameters are caused by endogenously produced H(2), but they were <15% for rumen fluid and 10% for lake sediment and digestor sludge. Increases in V(max) during the course of progress curve experiments were not great enough to produce systematic deviations from Michaelis-Menten kinetics.
米氏动力学参数为 H(2)的消耗由三个产甲烷栖息地从进展曲线和初始速度实验确定。传质阻力的影响,内源性 H(2)的生产,以及对表观参数估计的影响也进行了研究。动力学参数不能为未经稀释的瘤胃液和一些消化器污泥从气相测量的 H(2),因为 H(2)的传质通过气-液界面是限速的。然而,一旦样品被稀释,就可以得到准确的值。消化器污泥和超营养湖泊沉积物的 H(2)消耗不受相转移限制。这些栖息地的 H(2)摄取 K(m)值相似,平均值分别为 5.8、6.0 和 7.1 μM 用于瘤胃液、消化器污泥和沉积物。V(max)的估计表明,活性的比值约为 100(瘤胃液):10(污泥):1(沉积物);它们的范围如下:瘤胃液,14 至 28 mM h;Holt 污泥,0.7 至 4.3 mM h;和 Wintergreen 沉积物,0.13 至 0.49 mM h。在这里研究的 H(2)的相转移限制的原理是相同的,所有气态底物和产物。与气相动力学参数的测定相关的限制和误差通过一个数学模型进行了评估,该模型将质量传输和米氏动力学结合在一起。描述了三个标准,可以用来评估是否存在相转移限制。如果不存在,(i)底物消耗曲线是米氏酶动力学的,而不是一级的,(ii)K(m)与初始底物浓度无关,以及(iii)K(m)与生物质(V(max))无关,并且随着样品的稀释而保持不变。米氏酶动力学参数中的误差是由内源性产生的 H(2)引起的,但对于瘤胃液和 10%的湖泊沉积物和消化器污泥来说,误差<15%。在进展曲线实验过程中 V(max)的增加不足以产生与米氏酶动力学的系统偏差。