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Understanding Grassland Degradation and Restoration from the Perspective of Ecosystem Services: A Case Study of the Xilin River Basin in Inner Mongolia, China

机译:从生态系统服务的角度理解草地退化与恢复-以内蒙古锡林河流域为例

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Ecosystem services (ESs) and their transformations in northern China play a crucial role in regional sustainability. During the past several decades, grassland degradation has become one of the most important ecological and economic issues in this region. Therefore, understanding the impacts of grassland degradation and restoration on ESs is essential for maintaining ecological resilience and social security of Northern China. Our objective was to explore the relationship between ESs and grassland changes induced by vegetation succession in the Xilin River Basin, Inner Mongolia, China. Using vegetation maps derived from remotely sensed imagery collected in 1983, 1989, 2000, and 2011, we calculated the degree of grassland degradation using the Grassland Degradation Index (GDI). Aboveground biomass (AGB), soil conservation (SC), and water retention (WR) were also estimated to assess ESs for each year. Our results show that: (1) GDI increased during 1983–2000 and decreased during 2000–2011 indicating that after experiencing two decades of severe degradation the grassland has been restored since 2000. (2) AGB and SC were significantly negatively correlated with GDI. Changes in grassland conditions significantly affected WR and SC with both declining during 1983–2000 and increasing afterwards. The increase of SC, however, was slow compared to AGB and WR, which is an indication of time lag in soil restoration. (3) Grasslands in the middle and lower reaches experienced worse degradation than in the upper reaches. (4) AGB and SC exhibited a synergy, while trade-offs existed between AGB and WR and SC and WR. In summary, significant changes in grassland ecosystems in the Xilin River Basin over the past three decades affected the dynamics of ESs among which SC and WR require special attention in the future.
机译:中国北方的生态系统服务(ESs)及其转变在区域可持续发展中发挥着至关重要的作用。在过去的几十年中,草地退化已成为该地区最重要的生态和经济问题之一。因此,了解草地退化和恢复对生态系统的影响对于维持中国北方的生态适应力和社会保障至关重要。我们的目的是探讨内蒙古锡林河流域的生态系统因子与植被演替引起的草地变化之间的关系。使用从1983年,1989年,2000年和2011年收集的遥感图像得出的植被图,我们使用草地退化指数(GDI)计算了草地退化的程度。还估算了地上生物量(AGB),土壤保持(SC)和保水(WR)来评估每年的ES。我们的结果表明:(1)GDI在1983–2000年期间增加,而在2000–2011年期间下降,这表明在经历了20年的严重退化之后,2000年以来草地已经恢复。(2)AGB和SC与GDI显着负相关。草地条件的变化对WR和SC影响显着,在1983-2000年期间均下降,此后又增加。然而,与AGB和WR相比,SC的增加缓慢,这表明土壤恢复存在时间滞后。 (3)中下游草原的退化程度比上游草原严重。 (4)AGB和SC表现出协同作用,而AGB和WR以及SC和WR之间存在取舍。总之,在过去的三十年中,锡林河流域的草地生态系统发生了重大变化,影响了ES的动态,其中SC和WR将来需要特别关注。

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