首页> 美国卫生研究院文献>Applied and Environmental Microbiology >Mineralization of the Cyclic Nitramine Explosive Hexahydro-135-Trinitro-135-Triazine by Gordonia and Williamsia spp.
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Mineralization of the Cyclic Nitramine Explosive Hexahydro-135-Trinitro-135-Triazine by Gordonia and Williamsia spp.

机译:Gordonia和Williamsia spp对环硝胺爆炸性六氢-135-三硝基-135-三嗪的矿化作用。

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摘要

Hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) is a cyclic nitroamine explosive that is a major component in many military high-explosive formulations. In this study, two aerobic bacteria that are capable of using RDX as the sole source of carbon and nitrogen to support their growth were isolated from surface soil. These bacterial strains were identified by their fatty acid profiles and 16S ribosomal gene sequences as Williamsia sp. KTR4 and Gordonia sp. KTR9. The physiology of each strain was characterized with respect to the rates of RDX degradation and [U-14C]RDX mineralization when RDX was supplied as a sole carbon and nitrogen source in the presence and absence of competing carbon and nitrogen sources. Strains KTR4 and KTR9 degraded 180 μM RDX within 72 h when RDX served as the only added carbon and nitrogen source while growing to total protein concentrations of 18.6 and 16.5 μg/ml, respectively. Mineralization of [U-14C]RDX to 14CO2 was 30% by strain KTR4 and 27% by KTR9 when RDX was the only added source of carbon and nitrogen. The addition of (NH4)2SO4 greatly inhibited KTR9's degradation of RDX but had little effect on that of KTR4. These are the first two pure bacterial cultures isolated that are able to use RDX as a sole carbon and nitrogen source. These two genera possess different physiologies with respect to RDX mineralization, and each can serve as a useful microbiological model for the study of RDX biodegradation with regard to physiology, biochemistry, and genetics.
机译:六氢-1,3,5-三硝基-1,3,5-三嗪(RDX)是环状硝胺炸药,是许多军事高爆配方中的主要成分。在这项研究中,从表层土壤中分离出了两种有氧细菌,它们能够利用RDX作为唯一的碳和氮源来支持其生长。这些细菌菌株通过其脂肪酸谱和16S核糖体基因序列被鉴定为Williamsia sp。 KTR4和Gordonia sp。 KTR9。在存在和不存在竞争碳的情况下,当RDX作为唯一碳源和氮源提供时,根据RDX降解速率和[U- 14 C] RDX矿化来表征每种菌株的生理学和氮源。当RDX用作唯一添加的碳和氮源时,菌株KTR4和KTR9在72小时内降解了180μMRDX,同时分别增长到总蛋白浓度为18.6和16.5μg/ ml。当RDX是唯一添加的碳和氮源时,KTR4菌株将[U- 14 C] RDX矿化为 14 CO2的量为30%,而KTR9的量为27%。 (NH4)2SO4的添加大大抑制了KTR9对RDX的降解,但对KTR4的影响很小。这是分离的前两种纯细菌培养物,它们能够使用RDX作为唯一的碳和氮源。这两个属在RDX矿化方面具有不同的生理学,并且每个都可以用作研究RDX在生物学,生物化学和遗传学方面的生物降解的有用的微生物学模型。

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