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Impacts of increased nitrogen deposition and altered precipitation regimes on soil fertility and functioning in semiarid Mediterranean shrublands

机译:氮肥增加和降水方式改变对地中海半干旱灌丛土壤肥力和功能的影响

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We studied the impacts of nitrogen (N) deposition and precipitation gradients on soil chemistry and functioning of calcareous soils from semiarid Mediterranean shrublands. Under greenhouse conditions, N fertilization at 0, 10, 20 and 50 kg N ha~(-1) yr~(-1) and low water increased inorganic N. The concentration of extractable cations was higher under low water due to reduced leaching, whereas soil carbon (C) to N ratio was affected by the interaction of N fertilization and water supply, suggesting the role of rainfall in the response of soil C and N storage capacity to N deposition. Soil phosphatase activity increased with N as a consequence of an induced N to phosphorus imbalance, whereas N-fixation was down-regulated by N fertilization, a response attributed to high levels of nitrate. Net N mineralization and nitrification were also reduced by N fertilization. Under field conditions, N availability was positively related to the N deposition gradient (3.98-6.05 kg N ha~(-1) yr~(-1)). Nutrient availability was primarily and positively related to rainfall and temperature, although N deposition contributed to an overall cation depletion. Finally, we suggest the importance of conducting additional studies on the effects of N deposition and climate change on calcareous soils in Mediterranean ecosystems.
机译:我们研究了氮(N)的沉积和降水梯度对土壤化学和地中海半干旱灌丛钙质土壤功能的影响。在温室条件下,在0、10、20和50 kg N ha〜(-1)yr〜(-1)和低水下施氮会增加无机氮。由于减少了浸出,在低水下可萃取阳离子的浓度较高,施氮与供水之间的相互作用影响了土壤碳(C)与氮的比率,表明降雨在土壤碳和氮储量对氮沉降的响应中的作用。 N诱导的磷磷失衡导致土壤磷酸酶活性随N的增加而增加,而N的施肥则下调了N固定,这归因于硝酸盐的高含量。施氮还减少了净氮矿化和硝化作用。在田间条件下,氮的有效性与氮沉降梯度(3.98-6.05 kg N ha〜(-1)yr〜(-1))成正相关。营养素的利用主要与降雨和温度成正相关,尽管氮的沉积会导致整个阳离子的消耗。最后,我们建议对氮的沉积和气候变化对地中海生态系统钙质土壤的影响进行更多研究的重要性。

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