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1986-2015 年中国黄土高原植被恢复对净初级生产力的响应。

Response of net primary productivity to vegetation restoration in Chinese Loess Plateau during 1986-2015.

机构信息

School of Environmental and Chemical Engineering, Foshan University, Foshan, China.

Department of Environmental Engineering, School of Environmental Science and Engineering, Guangdong University of Technology, Guangzhou, P. R. China.

出版信息

PLoS One. 2019 Jul 10;14(7):e0219270. doi: 10.1371/journal.pone.0219270. eCollection 2019.

Abstract

Land use and land cover change induced by large scale ecological restoration programs has a significant impact on the terrestrial ecosystem carbon cycle, especially on the net primary productivity (NPP) in arid and semi-arid regions. This study investigated the change in NPP caused by the large-scale ecological restoration in the Chinese Loess Plateau (LPR) region from 1986 to 2015 based on land cover datasets and NPP calculated using the Carnegie-Ames-Stanford Approach model. The results indicated that the annual total NPP exhibited a significant uptrend (P < 0.01) throughout the whole vegetation restoration region during the last 30 years, with an annual increase of 0.137 Tg C. A significant abrupt change was detected in 2006 for the annual total NPP series. Over half of the restoration region showed an increase in NPP in the past three decades, however, about 30~40% of the vegetation restoration region exhibited NPP loss before 2006, but subsequently NPP loss was found in only approximately 20% of the study region. Overall, the increase in NPP attributed to the vegetation restoration reached 51.14 Tg C in the past three decades, indicating that these large-scale vegetation restoration programs increased the carbon sequestration capacity of terrestrial ecosystems in the Loess Plateau. The findings of this study improve our understanding of the effects of the green campaign on terrestrial ecosystems.

摘要

大规模生态恢复计划引起的土地利用和土地覆盖变化对陆地生态系统碳循环有重大影响,特别是在干旱和半干旱地区。本研究基于土地覆盖数据集和利用 Carnegie-Ames-Stanford 方法模型计算的净初级生产力 (NPP),调查了 1986 年至 2015 年中国黄土高原地区大规模生态恢复引起的 NPP 变化。结果表明,在过去 30 年整个植被恢复区,年总 NPP 呈显著上升趋势(P < 0.01),年增长率为 0.137 Tg C。在 2006 年,年总 NPP 序列检测到一个显著的突然变化。在过去的三十年中,超过一半的恢复区的 NPP 增加,然而,大约 30%到 40%的植被恢复区在 2006 年前表现出 NPP 损失,但随后在研究区域中只有大约 20%的区域发现 NPP 损失。总体而言,过去三十年植被恢复带来的 NPP 增加量达到 51.14 Tg C,表明这些大规模的植被恢复计划增加了黄土高原陆地生态系统的碳固存能力。本研究的结果增进了我们对绿色运动对陆地生态系统影响的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2233/6619688/2206e87ae4d8/pone.0219270.g001.jpg

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