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Soil respiration response to alterations in precipitation and nitrogen addition in a desert steppe in northern China

机译:中国北方荒漠草原土壤呼吸对降水和氮素变化的响应

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Global climate change is expected to significantly influence soil respiration. When limited, rainfall and nitrogen (N) deposition strongly modify soil respiration in a broad range of biomes, but uncertainty remains with regards to the influence of the interactions of seasonal rainfall distribution and N deposition on soil respiration in an arid steppe. In the present study, we manipulated precipitation using V-shaped plexiglass gutters (minus 50%, control, and plus 50% treatments) and tested various N additions (control and plus 35 kg N ha(-1) yr(-1)) to evaluate their impact on soil respiration, measured using a Li-Cor 8100, in a desert steppe in China. Increased precipitation stimulated soil respiration by 26.1%, while decreased precipitation significantly reduced soil respiration by 10.8%. There was a significant increase in soil respiration under N addition at 11.5%. Statistical assessment of their interactions demonstrated that N supplementation strengthened the stimulation of soil respiration under increased precipitation, whereas decreased precipitation offset the positive impact of N addition and led to a reduction in soil respiration. Contrasting interannual precipitation patterns strongly influenced the temporal changes in soil respiration as well as its response to N addition, indicating that the desert steppe plant community was co-limited by water and N. Net primary productivity (aboveground and belowground) predominantly drove soil respiration under altered precipitation and N addition. As grasses are better equipped for water deficit due to their previous exposure to long periods without water, there could be a shift from forb to grass communities under drier conditions. These findings highlight the importance of assessing the differential impacts of plant traits and soil physiochemical properties on soil respiration under altered precipitation and N addition. (C) 2019 Published by Elsevier B.V.
机译:预计全球气候变化将严重影响土壤呼吸。当受到限制时,降雨和氮(N)沉积会在广泛的生物群落中强烈改变土壤呼吸,但是在干旱草原中,季节性降雨分布和氮沉积对土壤呼吸的相互作用的影响仍然不确定。在本研究中,我们使用V形有机玻璃水槽(负50%,对照和加50%处理)处理降水,并测试了各种氮素添加量(对照和35 kg N ha(-1)yr(-1))。评估它们在中国沙漠草原中使用Li-Cor 8100测得的对土壤呼吸的影响。降水增加使土壤呼吸增加26.1%,而降水减少则使土壤呼吸减少10.8%。施氮量为11.5%时,土壤呼吸显着增加。对它们之间相互作用的统计评估表明,在增加降水量的情况下,补充氮肥可增强对土壤呼吸的刺激,而减少的降水抵消了氮素添加的积极影响,并导致土壤呼吸作用的降低。不同的年际降水模式强烈影响土壤呼吸的时间变化及其对氮的响应,表明沙漠草原植物群落受到水和氮的共同限制。净初级生产力(地上和地下)主要推动了土壤呼吸。改变了降水和氮的添加。由于草由于以前长期缺水而更适合缺水,因此在较干燥的条件下,草可能会从草群落转变为草群落。这些发现凸显了评估降雨和氮添加变化下植物性状和土壤理化特性对土壤呼吸的不同影响的重要性。 (C)2019由Elsevier B.V.发布

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