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首页> 外文期刊>Applied and Environmental Microbiology >Nitrogen limitation and nitrogen fixation during alkane biodegradation in a sandy soil.
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Nitrogen limitation and nitrogen fixation during alkane biodegradation in a sandy soil.

机译:沙质土壤中烷烃生物降解过程中的氮限制和固氮作用。

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We investigated nutrient limitations during hydrocarbon degradation in a sandy soil and found that fixed nitrogen was initially a limiting nutrient but that N limitation could sometimes be overcome by N2 fixation. Hydrocarbon biodegradation was examined in an unsaturated sandy soil incubated aerobically at 20 degrees C with propane or butane and various added nutrients. Propane and butane degradation proceeded similarly during the first 3 months of incubation. That is, bacteria in soil amended with N oxidized these hydrocarbons more rapidly than in controls without nutrient additions or in soil with added phosphate or trace minerals. Both propane- and butane-amended soil apparently became N limited after the initial available inorganic N was utilized, as indicated by a decrease in the rates of hydrocarbon degradation. After 3 months, propane and butane degradation proceeded differently. Bacteria in propane-degrading soil apparently remained N limited because propane degradation rates stayed low unless more N was added. In contrast, bacteria in butane-degrading soil appeared to overcome their N limitation because butane degradation rates later increased regardless of whether more N was added. Analyses of total N and acetylene reduction assays supported this apparent surplus of N in butane-amended soil. Total N was significantly (P < 0.01) higher in soil incubated with butane and no N amendments than in soil incubated with propane, even when the latter was amended with N. Acetylene reduction occurred only in butane-amended soil. These results indicate that N2 fixation occurred in butane-amended soil but not in propane-amended soil.
机译:我们研究了沙质土壤中碳氢化合物降解过程中的养分限制,发现固定氮最初是限制性养分,但有时N2固定可以克服N的限制。在不饱和的沙质土壤中检查了碳氢化合物的生物降解作用,该土壤在20摄氏度下与丙烷或丁烷和各种添加的养分进行有氧培养。在孵育的前三个月中,丙烷和丁烷的降解过程相似。也就是说,与不添加营养物的对照组或添加磷酸盐或微量矿物质的土壤相比,用N修饰的土壤中的细菌氧化这些碳氢化合物的速度更快。丙烷和丁烷改性的土壤在利用了最初可用的无机氮后,显然都受到了氮的限制,这是由烃降解速率的降低所表明的。 3个月后,丙烷和丁烷的降解过程有所不同。丙烷降解土壤中的细菌显然仍受氮的限制,因为除非添加更多的氮,否则丙烷的降解率仍然很低。相反,丁烷降解土壤中的细菌似乎克服了它们的N限制,因为无论是否添加更多的N,丁烷的降解率随后都会增加。总氮和乙炔还原分析的分析结果支持了丁烷改良土壤中氮的明显过剩。与丙烷一起培养的土壤中,总氮显着(P <0.01)高于与丙烷一起培养的土壤,即使后者被N改性。乙炔还原仅在丁烷改性的土壤中发生。这些结果表明,在丁烷改良的土壤中发生了N2固定,而在丙烷改良的土壤中没有发生。

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