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首页> 外文期刊>Soil Biology & Biochemistry >Sequential extraction of denitrifying organisms from soils; strongly attached cells produce less N2O than loosely attached cells
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Sequential extraction of denitrifying organisms from soils; strongly attached cells produce less N2O than loosely attached cells

机译:从土壤中依次提取反硝化生物;牢固附着的细胞产生的N2O少于松弛附着的细胞

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摘要

Soil denitrifier communities (DC) have been studied intensively because their phenotypic characteristics may influence the emission of NO and N2O. In the present study, we challenge the concept of soil DC as one assemblage of organisms, and propose that DCs are functionally stratified based on their position within the soil matrix. We hypothesize that the soils contain "inner" and "outer" habitats; the inner meaning sites within crevices and cavities of the soil mineral material, structured organic materials and strong biofilms, the outer meaning exposed surfaces and macropores of the soil. We used sequential dispersion/density gradient centrifugation (DGC), to obtain two contrasting fractions of cells differing in the strength of attachment to soil particles. We define loosely attached cells (LAC) as those which are liberated from soil particles by moderate dispersion of the soils. LAC were harvested by DGC, and the pellets at the bottom of the gradients were then re-dispersed with higher shear force to release more strongly attached cells (SAC) which were again harvested by DGC. We hypothesized that SAC are cells situated deeper into biofilms and structures than LAC, hence SAC would experience more frequent and/or longer anoxic spells than LAC. For this reason, we hypothesized 1) that the relative frequency of denitrifying organisms is higher in SAC than LAC and 2) that N2O-reductase is expressed earlier and stronger in SAC than in LAC. The results suggest a rejection of the first hypothesis but lend strong support for the second: In response to oxygen depletion, the two fractions (LAC and SAC) expressed similar rates of denitrification, both produced a mixture of NO, N2O and N-2, but the relative amount of N2O produced was much higher for LAC than SAC. The soils' matrix appears to contain strata which select for specific denitrification phenotypes, with implications for N2O-emission
机译:土壤反硝化菌群落(DC)的表型特征可能会影响NO和N2O的排放,因此已对其进行了深入研究。在本研究中,我们挑战土壤DC作为一种有机体的概念,并提出DC在功能上根据其在土壤基质中的位置进行分层。我们假设土壤包含“内部”和“外部”栖息地。内部含义是土壤矿物材料,结构化有机材料和强生物膜的缝隙和空腔内,外部含义是土壤的裸露表面和大孔。我们使用顺序分散/密度梯度离心(DGC),获得了两个对比部分的细胞,其附着在土壤颗粒上的强度不同。我们将松散附着的细胞(LAC)定义为通过适度分散土壤而从土壤颗粒中释放出来的细胞。用DGC收获LAC,然后用较高的剪切力将梯度底部的沉淀物重新分散,以释放更牢固附着的细胞(SAC),然后再用DGC收获。我们假设SAC是比LAC更深入生物膜和结构的细胞,因此SAC比LAC经历更频繁和/或更长时间的缺氧咒语。因此,我们假设1)SAC中反硝化生物的相对频率高于LAC,2)SAC中N2O还原酶的表达早于LAC,并且比LAC更强。结果表明拒绝了第一种假设,但为第二种假设提供了有力的支持:响应氧气耗竭,这两个馏分(LAC和SAC)表现出相似的反硝化速率,均产生了NO,N2O和N-2的混合物,但是LAC产生的N2O的相对数量要比SAC高得多。土壤的基质似乎包含选择特定反硝化表型的地层,这会影响N2O的排放

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