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Differential Metabolism of Dimethylsulfoniopropionate and Acrylate in Saline and Brackish Intertidal Sediments.盐渍和微咸潮间带沉积物中二甲巯基丙酸内盐和丙烯酸酯的差异代谢
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Aerobic and anaerobic growth of rifampin-resistant denitrifying bacteria in soil.土壤中耐利福平反硝化细菌的需氧和厌氧生长
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10
Biodegradation of organic compounds in vadose zone and aquifer sediments.包气带和含水层沉积物中有机化合物的生物降解。
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本文引用的文献

1
Relative rates of nitric oxide and nitrous oxide production by nitrifiers, denitrifiers, and nitrate respirers.硝化菌、反硝化菌和硝酸盐呼吸菌产生一氧化二氮和一氧化氮的相对速率。
Appl Environ Microbiol. 1986 May;51(5):938-45. doi: 10.1128/aem.51.5.938-945.1986.
2
Persistence of denitrifying enzyme activity in dried soils.在干燥土壤中,反硝化酶活性的持续存在。
Appl Environ Microbiol. 1985 Feb;49(2):316-20. doi: 10.1128/aem.49.2.316-320.1985.
3
Denitrification: ecological niches, competition and survival.反硝化作用:生态位、竞争与生存
Antonie Van Leeuwenhoek. 1982;48(6):569-83. doi: 10.1007/BF00399542.
4
Reduction of nitrogenous oxides by microorganisms.微生物对氮氧化物的还原作用。
Bacteriol Rev. 1973 Dec;37(4):409-52. doi: 10.1128/br.37.4.409-452.1973.
5
Survival strategies of bacteria in the natural environment.细菌在自然环境中的生存策略。
Microbiol Rev. 1987 Sep;51(3):365-79. doi: 10.1128/mr.51.3.365-379.1987.

土壤反硝化菌种群动态:酶活性、最可能数计数与实际 N 气体损失之间的关系。

Dynamics of Soil Denitrifier Populations: Relationships between Enzyme Activity, Most-Probable-Number Counts, and Actual N Gas Loss.

机构信息

Department of Agronomy, University of Kentucky, Lexington, Kentucky 40546.

出版信息

Appl Environ Microbiol. 1988 Nov;54(11):2711-6. doi: 10.1128/aem.54.11.2711-2716.1988.

DOI:10.1128/aem.54.11.2711-2716.1988
PMID:16347773
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC204360/
Abstract

To better understand temporal variability in soil denitrification, denitrifying enzyme activity (DEA) and denitrifier populations (as determined by most-probable-number [MPN] counts) were measured in field and laboratory experiments. Measurements of DEA and MPN provided highly contradictory indications of denitrifier dynamics. In laboratory incubations, under conditions favoring active denitrification, the synthesis of new denitrifying enzymes and the actual amount of denitrification were closely related. In other experiments, however, both DEA and MPN counts were poor indicators of actual denitrification. In some cases, we found significant increases in DEA but no significant production of N gas. Except with unnaturally high substrate amendments, changes in DEA were small relative both to the persistently high DEA background and to changes in MPN. As estimated by MPN counts, denitrifier populations increased significantly during denitrification events. It was apparent that only a small fraction of the denitrifiers were included in the MPN counts, but it appeared that this isolatable fraction increased during periods of active denitrifier growth. Use of DEA as an index of biomass of cells which have synthesized denitrifying enzymes suggested that denitrifier populations were persistent, stable, and much larger than indicated by MPN procedures.

摘要

为了更好地理解土壤反硝化的时间变异性,我们在野外和实验室实验中测量了反硝化酶活性(DEA)和反硝化菌数量(通过最可能数[MPN]计数确定)。DEA 和 MPN 的测量结果对反硝化菌动态提供了高度矛盾的指示。在实验室培养中,在有利于反硝化活性的条件下,新的反硝化酶的合成和实际的反硝化作用密切相关。然而,在其他实验中,DEA 和 MPN 计数都不能很好地指示实际的反硝化作用。在某些情况下,我们发现 DEA 显著增加,但没有显著产生 N 气体。除了采用不自然的高底物添加外,DEA 的变化相对于持续的高 DEA 背景和 MPN 的变化都很小。根据 MPN 计数估计,反硝化菌数量在反硝化事件中显著增加。显然,只有一小部分反硝化菌被包括在 MPN 计数中,但似乎在反硝化菌生长活跃期间,可分离的部分增加了。使用 DEA 作为已经合成反硝化酶的细胞生物量的指标表明,反硝化菌种群是持久的、稳定的,而且比 MPN 方法所指示的要大得多。