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首页> 外文期刊>Grass and forage science: the journal of the British Grassland Society. >Effects of in situ freezing on soil net nitrogen mineralization and net nitrification in fertilized grassland of northern China.
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Effects of in situ freezing on soil net nitrogen mineralization and net nitrification in fertilized grassland of northern China.

机译:原位冷冻对华北施肥草地土壤净氮矿化和净硝化的影响。

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摘要

Effects of soil freezing on nitrogen (N) mineralization have been the subject of increased attention in the ecological literature, though fewer studies have examined N mineralization responses to successive mild freezing, severe freezing and cyclic freeze-thaw events. Even less is known about relationships of responses to soil N status. This study measured soil N mineralization and nitrification in the field along an experimental N gradient in a grassland of northern China during the dormant season (October 2005-April 2006), a period in which freezing naturally occurs. Net N mineralization exhibited great temporal variability, with nitrification being the predominant N transformation process. Soil microbial biomass C and N and extractable NH4+ pools declined by 40, 52, and 56%, respectively, in April 2006, compared with their initial concentrations in October 2005; soil NO3- pools increased by 84%. Temporal patterns of N mineralization were correlated with soil microbial biomass C and N. N mineralization and nitrification increased linearly with added N. Microbial biomass C in treated soils increased by 10% relative to controls, whereas microbial N declined by 9%. Results further suggest that freezing events greatly alter soil N dynamics in the dormant season at this site, with considerable available N accumulating during this period.
机译:土壤冻结对氮(N)矿化的影响已成为生态文献中越来越受到关注的主题,尽管很少有研究研究氮对连续轻度冻结,重度冻结和循环冻融事件的响应。关于土壤氮素状况的响应关系知之甚少。这项研究在休眠期(2005年10月至2006年4月)这一自然冻结的时期,沿着实验性的N梯度测量了田间土壤氮的矿化和硝化作用。净氮矿化表现出很大的时间变异性,其中硝化作用是氮的主要转化过程。与2005年10月的初始浓度相比,2006年4月土壤微生物量碳和氮以及可提取的NH 4 + 库分别下降了40%,52%和56%。 ;土壤NO 3 -池增加了84%。氮矿化的时间模式与土壤微生物量碳和氮相关。氮矿化和硝化作用与氮的增加呈线性关系。处理过的土壤中微生物量碳相对于对照增加了10%,而微生物氮减少了9%。结果进一步表明,冻结事件极大地改变了该地点在休眠期的土壤氮素动态,在此期间累积了大量可利用的氮素。

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