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首页> 外文期刊>Global change biology >Response of ecosystem carbon exchange to warming and nitrogen addition during two hydrologically contrasting growing seasons in a temperate steppe
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Response of ecosystem carbon exchange to warming and nitrogen addition during two hydrologically contrasting growing seasons in a temperate steppe

机译:温带草原两个水文相反的生长季节中生态系统碳交换对变暖和氮添加的响应

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A large remaining source of uncertainty in global model predictions of future climate is how ecosystem carbon (C) cycle feedbacks to climate change. We conducted a field manipulative experiment of warming and nitrogen (N) addition in a temperate steppe in northern China during two contrasting hydrological growing seasons in 2006 [wet with total precipitation 11.2% above the long-term mean (348 mm)] and 2007 (dry with total precipitation 46.7% below the long-term mean). Irrespective of strong intra- and interannual variations in ecosystem C fluxes, responses of ecosystem C fluxes to warming and N addition did not change between the two growing seasons, suggesting independence of warming and N responses of net ecosystem C exchange (NEE) upon hydrological variations in the temperate steppe. Warming had no effect on NEE or its two components, gross ecosystem productivity (GEP) and ecosystem respiration (ER), whereas N addition stimulated GEP but did not affect ER, leading to positive responses of NEE. Similar responses of NEE between the two growing seasons were due to changes in both biotic and abiotic factors and their impacts on ER and GEP. In the wet growing season, NEE was positively correlated with soil moisture and forb biomass. Negative effects of warming-induced water depletion could be ameliorated by higher forb biomass in the warmed plots. N addition increased forb biomass but did not affect soil moisture, leading to positive effect on NEE. In the dry growing season, NEE showed positive dependence on grass biomass but negative dependence on forb biomass. No changes in NEE in response to warming could result from water limitation on both GEP and ER as well as little responses of either grass or forb biomass. N addition stimulated grass biomass but reduced forb biomass, leading to the increase in NEE. Our findings highlight the importance of changes in abiotic (soil moisture, N availability) and biotic (growth of different plant functional types) in mediating the responses of NEE to climatic warming and N enrichment in the semiarid temperate steppe in northern China.
机译:在未来气候的全球模型预测中,不确定性的一个主要来源是生态系统碳(C)如何循环反馈到气候变化。我们在2006年的两个相反的水文生长季节[湿润,总降水量比长期平均值(348 mm)高11.2%]的情况下,在中国北方的温带草原进行了增温和氮(N)添加的野外操作实验。干燥,总降水量低于长期平均值的46.7%)。不论生态系统碳通量的年内和年际变化如何,在两个生长季节之间,生态系统碳通量对变暖和氮添加的响应都没有变化,表明变暖和净生态系统碳交换(NEE)对水文变化的响应独立在温带草原。气候变暖对NEE或其两个组成部分,即生态系统总生产力(GEP)和生态系统呼吸(ER)没有影响,而氮的添加刺激了GEP,但不影响ER,导致NEE产生积极反应。在两个生长期之间,NEE的响应类似,这是由于生物和非生物因子的变化及其对ER和GEP的影响。在潮湿的生长季节,NEE与土壤水分和禁止生物量呈正相关。变暖地块中较高的forb生物量可以减轻变暖引起的水耗的负面影响。氮的添加增加了前生生物量,但不影响土壤水分,从而对NEE产生了积极影响。在干旱的生长季节,NEE对草的生物量呈正相关,而对草的生物量呈负相关。对GEP和ER的水分限制以及草或Forb生物量的响应很少,因此不会因变暖而导致NEE发生变化。氮的添加刺激了草的生物量,但减少了草的生物量,导致NEE增加。我们的研究结果突出了非生物(土壤水分,氮的有效性)和生物(不同植物功能类型的生长)的变化在介导中国北部半干旱温带草原的NEE对气候变暖和氮富集的响应中的重要性。

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