Shi W, Becker J, Bischoff M, Turco R F, Konopka A E
Department of Biological Sciences. Department of Agronomy, Purdue University, West Lafayette, Indiana 47907, USA.
Appl Environ Microbiol. 2002 Aug;68(8):3859-66. doi: 10.1128/AEM.68.8.3859-3866.2002.
Microbial community composition and activity were characterized in soil contaminated with lead (Pb), chromium (Cr), and hydrocarbons. Contaminant levels were very heterogeneous and ranged from 50 to 16,700 mg of total petroleum hydrocarbons (TPH) kg of soil(-1), 3 to 3,300 mg of total Cr kg of soil(-1), and 1 to 17,100 mg of Pb kg of soil(-1). Microbial community compositions were estimated from the patterns of phospholipid fatty acids (PLFA); these were considerably different among the 14 soil samples. Statistical analyses suggested that the variation in PLFA was more correlated with soil hydrocarbons than with the levels of Cr and Pb. The metal sensitivity of the microbial community was determined by extracting bacteria from soil and measuring [(3)H]leucine incorporation as a function of metal concentration. Six soil samples collected in the spring of 1999 had IC(50) values (the heavy metal concentrations giving 50% reduction of microbial activity) of approximately 2.5 mM for CrO(4)2- and 0.01 mM for Pb2+. Much higher levels of Pb were required to inhibit [14C]glucose mineralization directly in soils. In microcosm experiments with these samples, microbial biomass and the ratio of microbial biomass to soil organic C were not correlated with the concentrations of hydrocarbons and heavy metals. However, microbial C respiration in samples with a higher level of hydrocarbons differed from the other soils no matter whether complex organic C (alfalfa) was added or not. The ratios of microbial C respiration to microbial biomass differed significantly among the soil samples (P < 0.05) and were relatively high in soils contaminated with hydrocarbons or heavy metals. Our results suggest that the soil microbial community was predominantly affected by hydrocarbons.
对受铅(Pb)、铬(Cr)和碳氢化合物污染的土壤中的微生物群落组成和活性进行了表征。污染物水平非常不均匀,总石油烃(TPH)含量范围为50至16700 mg/kg土壤,总铬含量范围为3至3300 mg/kg土壤,铅含量范围为1至17100 mg/kg土壤。根据磷脂脂肪酸(PLFA)模式估算微生物群落组成;这在14个土壤样品中差异很大。统计分析表明,PLFA的变化与土壤碳氢化合物的相关性比与Cr和Pb的水平更高。通过从土壤中提取细菌并测量[³H]亮氨酸掺入量作为金属浓度的函数来确定微生物群落对金属的敏感性。1999年春季采集的6个土壤样品中,CrO₄²⁻的IC₅₀值(使微生物活性降低50%的重金属浓度)约为2.5 mM,Pb²⁺的IC₅₀值约为0.01 mM。直接抑制土壤中[¹⁴C]葡萄糖矿化需要更高水平的Pb。在对这些样品进行的微观实验中,微生物生物量以及微生物生物量与土壤有机碳的比率与碳氢化合物和重金属的浓度无关。然而,无论是否添加复杂有机碳(苜蓿),碳氢化合物含量较高的样品中的微生物碳呼吸与其他土壤不同。土壤样品中微生物碳呼吸与微生物生物量的比率差异显著(P < 0.05),在受碳氢化合物或重金属污染的土壤中相对较高。我们的结果表明,土壤微生物群落主要受碳氢化合物的影响。