Department of Environmental Sciences and Engineering, School of Public Health, University of North Carolina, 27514, Chapel Hill, North Carolina, USA.
Microb Ecol. 1988 May;15(3):257-73. doi: 10.1007/BF02012641.
A method is described for determining biodegradation kinetics of both naturally occurring and xenobiotic compounds in surface and sub-surface soil samples. The method measures both respiration and uptake into cellular biomass of(14)C-labeled substrates. The estimation of biomass incorporation entailed removal of cells from soil particles by washing the soil with a polyvinyl-pyrrolidone/pyrophosphate solution and H2O2. After separation of the cells and the soil particles by centrifugation, the cells were trapped on membrane filters for liquid scintillation counting. Mass balances were easily obtained. The technique was used to measure metabolic activity in soil profiles, including unsaturated and saturated zones. First order rate constants (K1) were in the range of 10(-3)-10(-2) hour(-1) for amino acid metabolism and 10(-5)-10(-4) hour(-1) for m-cresol metabolism. Saturation kinetics were observed for amino acids and m-cresol. m-Cresol K1 values for uptake often exceeded those for respiration by greater than a factor of ten. Vmax values were low (amino acids, 10(1)-10(2) ng g(-1) hour(-1); m-cresol, 10(-1) ng g(-1) hour(-1)), whereas Km values were quite high (amino acids, 10(3)-10(4) ng g(-1); m-cresol 10(3)-10(5) ng g(-1)). Saturation was not observed in many horizons even at 10(5) ng g(-1) dry soil. Frequently, respiration obeyed saturation kinetics whereas uptake was first order. It is concluded that measuring only kinetics of respiration may lead to severe underestimations of biodegradation rates.
描述了一种用于测定地表和地下土壤样品中天然和外来化合物生物降解动力学的方法。该方法测量(14)C 标记底物的呼吸作用和细胞生物量的摄取。通过用聚乙烯吡咯烷酮/焦磷酸盐溶液和 H2O2 洗涤土壤来去除细胞,从而估算生物量的掺入。通过离心分离细胞和土壤颗粒后,将细胞捕获在膜过滤器上进行液体闪烁计数。很容易获得质量平衡。该技术用于测量土壤剖面中的代谢活性,包括不饱和和饱和区。氨基酸代谢的一级速率常数(K1)在 10(-3)-10(-2)小时(-1)范围内,间甲酚代谢的 K1 在 10(-5)-10(-4)小时(-1)范围内。对于氨基酸和间甲酚,观察到饱和动力学。对于间甲酚的摄取,K1 值通常比呼吸作用高出 10 倍以上。Vmax 值较低(氨基酸,10(1)-10(2)ng g(-1)小时(-1);间甲酚,10(-1)ng g(-1)小时(-1)),而 Km 值则相当高(氨基酸,10(3)-10(4)ng g(-1);间甲酚 10(3)-10(5)ng g(-1))。即使在 10(5)ng g(-1)干土中,许多地层也没有观察到饱和。经常,呼吸作用遵循饱和动力学,而摄取是一级动力学。因此,仅测量呼吸作用的动力学可能会导致生物降解速率的严重低估。