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首页> 外文期刊>Rangeland Ecology & Management >Grassland Carbon Sequestration Ability in China: A New Perspective from Terrestrial Aridity Zones
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Grassland Carbon Sequestration Ability in China: A New Perspective from Terrestrial Aridity Zones

机译:中国草原碳汇能力:陆地干旱区的新视角

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Current climate change (e.g., temperature and precipitation variations) profoundly influences terrestrial vegetation growth and production, ecosystem respiration, and nutrient circulation. Grasslands are sensitive to climate change, and the carbon sequestration ability is closely related to water availability. However, how the terrestrial water budget influences regional carbon sequestration by the grassland ecosystem is still unclear. In this study, we modified a terrestrial biogeochemical model to investigate net ecosystem productivity (NEP) of Chinese grasslands under different aridity index (AI) levels from 1982 to 2008. The results showed that Chinese grasslands acted as a carbon sink of 33.7 TgC. yr(-1), with a clear decrease in the spatial distribution from the humid end (near-forest) to the arid end (near-desert). During these 27 years, gross primary productivity (GPP) and net primary productivity (NPP) significantly increased with regional warming over the entire range of the AI, but no significant tendency was found for NEP. Meanwhile, only NPP in the arid zone (AR) and the semiarid zone (SAR) were significantly correlated with mean annual precipitation (MAP), and no significant correlation was found between heterotrophic respiration (R-h) and MAP; NPP and R-h were both positively correlated with mean annual temperature (MAT) in all AI zones except for NPP in AR; no significant correlation between NEP and MAP or MAT was found. These results revealed that the grasslands with different AI levels keep different response patterns to temperature and precipitation variations. On the basis of these results, we predicted that the gap of carbon sequestration ability between humid and arid grassland will expand. The total carbon sink in Chinese grasslands will continue to fluctuate, but there is a danger that it might shrink in the future because of a combination of climatic and human factors, although CO2 fertilization and N deposition might partly mitigate this reduction. (C) 2016 Society for Range Management. Published by Elsevier Inc. All rights reserved.
机译:当前的气候变化(例如温度和降水变化)深刻影响着陆地植被的生长和生产,生态系统的呼吸作用以及养分循环。草原对气候变化敏感,固碳能力与水的供应量密切相关。但是,目前尚不清楚陆地水预算如何影响草地生态系统对区域碳固存的影响。在这项研究中,我们修改了陆地生物地球化学模型,以研究1982年至2008年不同干旱指数(AI)水平下中国草原的净生态系统生产力(NEP)。结果表明,中国草原的碳汇为33.7 TgC。 yr(-1),从湿端(近森林)到干旱端(近沙漠)的空间分布明显减少。在这27年中,随着AI整个范围的区域变暖,总初级生产力(GPP)和净初级生产力(NPP)显着增加,但是NEP却没有发现显着趋势。同时,仅干旱区(AR)和半干旱区(SAR)的NPP与年均降水量(MAP)显着相关,异养呼吸(R-h)与MAP之间无显着相关性。除了AR中的NPP外,所有AI区的NPP和R-h均与年平均温度(MAT)呈正相关。 NEP与MAP或MAT之间无显着相关性。这些结果表明,不同AI水平的草地对温度和降水变化的响应方式也不同。根据这些结果,我们预测湿地和干旱草原之间的固碳能力差距将会扩大。中国草原的总碳汇将继续波动,但存在危险,由于气候和人为因素的综合影响,将来可能会减少,尽管二氧化碳施肥和氮沉降可能会部分减轻这种减少。 (C)2016年范围管理学会。由Elsevier Inc.出版。保留所有权利。

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