Appl Environ Microbiol. 1997 Nov;63(11):4346-54. doi: 10.1128/aem.63.11.4346-4354.1997.
The oxidation of [(sup14)C]methyl bromide ([(sup14)C]MeBr) to (sup14)CO(inf2) was measured in field experiments with soils collected from two strawberry plots fumigated with mixtures of MeBr and chloropicrin (CCl(inf3)NO(inf2)). Although these fumigants are considered potent biocides, we found that the highest rates of MeBr oxidation occurred 1 to 2 days after injection when the fields were tarped, rather than before or several days after injection. No oxidation of MeBr occurred in heat-killed soils, indicating that microbes were the causative agents of the oxidation. Degradation of MeBr by chemical and/or biological processes accounted for 20 to 50% of the loss of MeBr during fumigation, with evasion to the atmosphere inferred to comprise the remainder. In laboratory incubations, complete removal of [(sup14)C]MeBr occurred within a few days, with 47 to 67% of the added MeBr oxidized to (sup14)CO(inf2) and the remainder of counts associated with the solid phase. Chloropicrin inhibited the oxidation of MeBr, implying that use of this substance constrains the extent of microbial degradation of MeBr during fumigation. Oxidation was by direct bacterial attack of MeBr and not of methanol, a product of the chemical hydrolysis of MeBr. Neither nitrifying nor methane-oxidizing bacteria were sufficiently active in these soils to account for the observed oxidation of MeBr, nor could the microbial degradation of MeBr be linked to cooxidation with exogenously supplied electron donors. However, repeated addition of MeBr to live soils resulted in higher rates of its removal, suggesting that soil bacteria used MeBr as an electron donor for growth. To support this interpretation, we isolated a gram-negative, aerobic bacterium from these soils which grew with MeBr as a sole source of carbon and energy.
在使用从用溴甲烷和氯化苦(CCl(inf3)NO(inf2))熏蒸的两个草莓地采集的土壤进行的田间试验中,测量了 [(sup14)C]甲基溴化物 ([(sup14)C]MeBr) 氧化为 (sup14)CO(inf2) 的速率。尽管这些熏蒸剂被认为是有效的杀菌剂,但我们发现,在田地被覆盖后的 1 到 2 天内,即在注入之前或之后几天,MeBr 的氧化速率最高。在热失活的土壤中没有发生 MeBr 氧化,表明微生物是氧化的原因。化学和/或生物过程对 MeBr 的降解导致在熏蒸过程中损失了 20%到 50%的 MeBr,其余部分推断为逸散到大气中。在实验室培养中,在几天内完全去除了 [(sup14)C]MeBr,添加的 MeBr 有 47%到 67%被氧化为 (sup14)CO(inf2),其余的计数与固相有关。氯化苦抑制了 MeBr 的氧化,这意味着使用这种物质会限制熏蒸过程中微生物对 MeBr 的降解程度。氧化是通过 MeBr 的直接细菌攻击,而不是通过 MeBr 的化学水解产物甲醇进行的。在这些土壤中,硝化菌和甲烷氧化菌都没有足够活跃,无法解释观察到的 MeBr 氧化,也无法将 MeBr 的微生物降解与外加电子供体的共氧化联系起来。然而,向活土壤中重复添加 MeBr 会导致其去除率更高,这表明土壤细菌将 MeBr 用作生长的电子供体。为了支持这一解释,我们从这些土壤中分离出一种革兰氏阴性、需氧细菌,该细菌可以将 MeBr 作为唯一的碳源和能源进行生长。