首页> 外文期刊>Agriculture, Ecosystems & Environment: An International Journal for Scientific Research on the Relationship of Agriculture and Food Production to the Biosphere >Influences of over winter conditions on denitrification and nitrous oxide-producing microorganism abundance and structure in an agricultural soil amended with different nitrogen sources.
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Influences of over winter conditions on denitrification and nitrous oxide-producing microorganism abundance and structure in an agricultural soil amended with different nitrogen sources.

机译:冬季条件对不同氮源改良的农业土壤中反硝化作用和产生一氧化二氮的微生物丰度和结构的影响。

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摘要

Changes in nitrifier and denitrifier abundance, composition and nitrous oxide (N2O) emissions during the winter period in soils with spring application of nitrogen (N) as mineral fertilizer, cattle manure or poultry manure were evaluated. Soil samples were collected from an agricultural field in Eastern Canada during winters of 2009-2010 and 2010-2011. Surprisingly, N2O emission rates were up to 150 fold greater in the coldest dates compared to other dates for the two winters, however rates were similar among N sources. Abundance of nitrifiers (Nitrobacter-like nxrA, archaeal amoA) and denitrifiers (nirK, nirS) increased in March and April compared with other sampling dates. Nitrifier abundance (nxrA) was the greatest in soils amended with cattle manure, while denitrifiers (nirK, nirS) were more abundant in soils amended with poultry manure. Nitrifiers and denitrifiers showed different composition depending on sampling date and N sources in the two winters, suggesting that changes in environmental conditions and N sources both influenced these communities. Our findings demonstrate that N2O emissions occur at significant rates in snow covered agricultural soils. Moreover, the abundance and diversity of denitrifier and nitrifier communities evolved throughout winter and appeared to be influenced by soil conditions and N sources applied in the previous spring.
机译:评价了冬季春季施用氮(N)作为矿物肥料,牛粪或家禽粪便的土壤中硝化和反硝化丰度,组成和一氧化二氮(N 2 O)排放的变化。在2009-2010年和2010-2011年冬季从加拿大东部的一块农田中收集了土壤样品。令人惊讶的是,与两个冬季的其他日期相比,最冷的日期N <2> O O排放速率高出150倍,但氮源之间的排放速率相似。与其他采样日期相比,3月和4月硝化剂(如硝化细菌的nxrA,古细菌amoA)和反硝化剂(nirK,nirS)的丰度增加了。在用牛粪肥改良的土壤中,硝化氮丰度(nxrA)最大,而在用家禽粪肥改良的土壤中,反硝化氮(nirK,nirS)含量更高。硝化剂和反硝化剂的成分不同,取决于采样日期和两个冬季的N来源,这表明环境条件的变化和N来源都影响了这些群落。我们的研究结果表明,N 2 O排放物在积雪的农业土壤中以显着速率发生。此外,反硝化和硝化群落的丰富度和多样性在整个冬季演化,并且似乎受到土壤条件和前一年春季施用的氮源的影响。

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