气候变化和植被恢复对黄土高原水源涵养功能时空变化的影响
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陕西省重点研发计划一般项目(2023-YBSF-380;2024SF-YBXM-533);水圈科学与水利工程全国重点实验室开放基金资助项目(sklhse-2023-A-05)


Spatial and temporal changes in water conservation in the Loess Plateau under the influence of climate change and vegetation restoration
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General Project of Shaanxi Provincial Key R&D Program (2023-YBSF-380;2024SF-YBXM-533); Project funded by Open Fund of National Key Laboratory of Hydrosphere Science and Hydraulic Engineering (sklhse-2023-A-05)

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    摘要:

    黄土高原是我国典型的气候变化敏感区和生态环境脆弱区,针对局部地区或流域尺度产水量及水源涵养量的研究大幅增加,然而定量评估气候变化和植被恢复下黄土高原整个区域水平的水源涵养功能时空变化的研究较为鲜见。以黄土高原为研究区,基于InVEST模型量化分析1982-2020年产水量及水源涵养功能的时空变化特征。结合皮尔逊相关分析和地理探测器方法,探讨了气候变化和植被恢复对水源涵养功能的影响。结果表明,1982-2020年黄土高原区水源涵养能力变化趋势稳定;1999年退耕还林工程实施后,年平均水源涵养总量相比2000年前增加了5%,且在空间上约66.7%的区域水源涵养能力有所提高,其中黄土丘陵沟壑区和黄土高原沟壑区的多年平均水源涵养能力增加显著,相较于2000年前分别提升了11.2%和18.4%。降水量的增加,潜在蒸发量的减少,均会导致水源涵养能力有所提高。植被覆盖度的增加,能够提高区域水源涵养能力。黄土高原大部分区域(约71.7%)叶面积指数(Leaf area index,LAI)与水源涵养能力呈正相关,其中黄土高原沟壑区和黄土丘陵沟壑区的相关性最强。影响水源涵养能力的因子解释程度排序为:降水量 > 潜在蒸发量 > LAI,降水量、潜在蒸发量和LAI双因子的交互作用对水源涵养能力的影响明显强于单一因子的影响,其中气候因素间的交互作用对水源涵养能力的影响程度最大,说明气候变化是黄土高原区水源涵养能力的主要影响因素。退耕还林工程的实施,显著增强了LAI和降水量对水源涵养能力的影响。退耕还林工程实施后,黄土高原水源涵养能力的提高主要受降水量的增加影响。建议将LAI控制在合理范围,保持植被的适度恢复,提高流域生态系统的水源涵养能力。研究结果可为制定区域生态恢复政策,提高水资源可持续利用与水源涵养能力,并保护生态系统功能提供重要理论依据。

    Abstract:

    The Loess Plateau, known for its sensitivity to climate change and ecological fragility, has seen a surge in research on water yield and conservation at local and watershed scales. However, regional-level studies quantifying the water conservation function, especially in the context of climate change and vegetation restoration, are scarce. This study addresses this gap by quantifying the spatial and temporal changes in water conservation on the Loess Plateau from 1982 to 2020, using the InVEST model's water yield module. Pearson's correlation coefficient and the Geodetector methods were employed to analyze the impacts of climate change and vegetation restoration on the water conservation. The results indicate a stable trend in water conservation from 1982 to 2020. Following the implementation of grain to green program in 1999, the average annual total water conservation volume improved by 5% compared to those during the pre-2000 period, approximately 66.7% of the regions exhibited increased water conservation, with particularly significant increases in the Loess Plateau gully and Loess Hills gully areas, by 11.2% and 18.4%, respectively. The increased precipitation and decreased evapotranspiration both enhance the water conservation. Increased vegetation cover improves regional water conservation. The Leaf area index (LAI) was positively correlated with water conservation in most areas of the Loess Plateau (about 71.7%), showing the strongest correlation in the Loess Plateau gully and Loess Hills gully areas. The explanation degree of each influencing factor of water conservation was ranked as follows: precipitation > potential evapotranspiration > LAI. The interaction of precipitation, potential evapotranspiration and LAI was significantly stronger than that of a single factor, and the interaction between climate factors had the greatest influence on water conservation, indicating that climate change is the main influence on water conservation in the Loess Plateau region. In addition, the implementation of grain to green program in 1999 has significantly enhanced effects of LAI and precipitation on water conservation. After the implementation of the fallow-land reforestation project, the enhancemetn of the water conservation of the Loess Plateau was primarily attributed to increase in precipitation. In future ecological management, LAI should be controlled in a reasonable range, and moderate restoration of vegetation should be maintained to improve the water conservation of the watershed ecosystem, Preventing the decline of regional water conservation due to over-restoration of vegetation cover. The research results would provide important theoretical basis for formulating regional ecological restoration policies, improving sustainable utilization of water resources and water conservation, and protecting ecosystem functions in various river basins.

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谢展,李萍,刘文倩,降亚楠.气候变化和植被恢复对黄土高原水源涵养功能时空变化的影响.生态学报,2024,44(23):10915~10935

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