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干旱刺激了根系产生和周转对变暖的响应,但抑制了对中国北方温带草原氮添加的响应。

Aridity stimulates responses of root production and turnover to warming but suppresses the responses to nitrogen addition in temperate grasslands of northern China.

机构信息

State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China; University of Chinese Academy of Sciences, Beijing 100049, China.

State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China; State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, China.

出版信息

Sci Total Environ. 2021 Jan 20;753:142018. doi: 10.1016/j.scitotenv.2020.142018. Epub 2020 Aug 26.

Abstract

Global warming and nitrogen (N) deposition are known to affect root dynamics in grasslands. However, previous studies were based only on a single ecosystem type, so it is unclear how warming and N addition affect root traits (root biomass, root-shoot ratio, root production and turnover) along the aridity gradient. In this study, we conducted an experiment to determine the effects of warming and N addition on root traits in desert, typical, and meadow grasslands in northern China, where the aridity gradually decreases from west to east across the region. Warming increased root-shoot ratio in dry year due to decline in soil water, but had a downward trend in root production and turnover in all three grasslands. N addition decreased root-shoot ratio in humid year due to increase in soil N, whereas did not significantly affect root production in any grasslands and increased root turnover in desert and meadow grasslands rather than typical grassland. Warming combined with N addition had negatively additive effects on root turnover in typical and meadow grasslands rather than desert grassland. N addition-induced changes in root biomass and root-shoot ratio were negatively affected by aridity in dry year. Aridity positively affected responses of root production and turnover to warming but negatively affected those responses to N addition. However, root-shoot ratio, root production and turnover under warming combined with N addition were not affected by aridity. Our results suggest that warming suppresses root carbon (C) input but N addition may exacerbate it in temperate grasslands, and warming combined with N addition suppresses it only in wet grasslands. Aridity promotes root C input under warming but suppresses it under N addition. However, aridity may little affect soil C and nutrient dynamics under global warming combined with N deposition in temperate grasslands in the future.

摘要

全球变暖与氮(N)沉降已知会影响草原根系动态。然而,先前的研究仅基于单一生态系统类型,因此尚不清楚变暖与 N 添加如何沿干旱梯度影响根系特征(根系生物量、根冠比、根系生产与周转率)。本研究通过野外控制实验,探讨了增温和 N 添加对中国北方荒漠、典型和草甸草原根系特征的影响,这些草原的干旱程度由西向东逐渐降低。变暖在干旱年增加了根冠比,因为土壤水分下降,但在所有三种草原中,根系生产与周转率均呈下降趋势。N 添加在湿润年降低了根冠比,因为土壤 N 增加,而在任何草原中对根系生产均无显著影响,在荒漠和草甸草原中反而增加了根系周转率。与荒漠草原相比,增温和 N 添加对典型和草甸草原根系周转率的复合效应呈负向相加。干旱度负向影响了 N 添加对干旱年根系生物量和根冠比的影响,正向影响了对变暖的响应,但负向影响了对 N 添加的响应。然而,在增温和 N 添加下,根冠比、根系生产和周转率不受干旱度影响。我们的研究结果表明,变暖抑制了根系的碳(C)输入,但 N 添加可能会加剧这种情况,而在湿润草原中,增温和 N 添加的复合效应会抑制这种情况。干旱度在变暖下促进了根系 C 输入,但在 N 添加下抑制了它。然而,在未来全球变暖与 N 沉降的共同作用下,干旱度可能对温带草原的土壤 C 和养分动态影响较小。

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