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Soil gross nitrogen transformations along the Northeast China Transect (NECT) and their response to simulated rainfall events

机译:东北样带(NECT)上土壤总氮的转化及其对模拟降雨事件的响应

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摘要

Climate changes are predicted to increase extreme rainfall events in semiarid and arid region in Northern Hemisphere. Nutrient cycles will be affected by the precipitation changes but so far only very little is known how soil N transformations may respond. Here we investigated gross soil N transformation rates and their response to simulated rainfall events across Northeast China Transect (NECT). The results showed that gross N mineralisation rate, nitrification rate and nitrification to mineralisation ratio significantly increased as the humidity index decreased along NECT, resulting in NO3 as the predominant inorganic N form. These characteristics could increase the risk of NO3 losses but at the same time reduce the risk of N losses via volatilization in the semiarid and arid region. The soil-plant ecosystems have developed effective N conservation strategies in the long term with respect to the prevailing climate in arid region. However, compared to humid soils more dramatic changes of soil N transformation rates are likely to occur in arid soils, after sudden soil moisture increases. Soil N conservation mechanisms in arid regions were drastically affected when the heavy rainfall frequently occurred. Arid ecosystems are expected to be more vulnerable than humid ecosystems in response to extreme rainfall events.
机译:预计气候变化将增加北半球半干旱和干旱地区的极端降雨事件。营养循环将受到降水变化的影响,但到目前为止,人们对土壤氮转化如何响应的了解还很少。在这里,我们调查了整个东北样带(NECT)的土壤总氮转化率及其对模拟降雨事件的响应。结果表明,随着NECT上湿度指数的降低,总氮矿化率,硝化率和硝化矿化率显着增加,从而导致NO3 -为主要的无机氮形态。这些特征可能会增加NO3 -损失的风险,但同时会通过半干旱和干旱地区的挥发降低N损失的风险。从长远来看,土壤植物生态系统已经针对干旱地区的主要气候条件制定了有效的氮保护策略。但是,与湿润的土壤相比,在土壤水分突然增加之后,干旱土壤中土壤氮转化率可能会发生更大的变化。当频繁发生强降雨时,干旱地区的土壤氮养护机制受到严重影响。响应极端降雨事件,干旱的生态系统比潮湿的生态系统更加脆弱。

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