黄河流域水源涵养服务功能动态演变及驱动因素
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国家自然科学基金(U1910207,U21A2041);城市与区域生态国家重点实验室开放基金(SKLURE2022-2-2)


Dynamic evolution and driving factors of water conservation service function in the Yellow River Basin
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National Natural Science Foundation of China(U1910207,U21A2041);Open Foundation of the State Key Laboratory of Urban and Regional Ecology of China(SKLURE2022-2-2)

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    摘要:

    黄河流域是中国重要的生态屏障,研究其水源涵养服务功能对推动黄河流域生态保护与高质量发展具有重大意义。采用InVEST模型量化黄河流域1980-2020年水源涵养服务功能,使用空间自相关分析黄河流域水源涵养服务功能空间分布模式,并运用地理探测器分析黄河流域水源涵养服务功能的驱动因素。结果表明:(1)1980-2020年黄河流域水源涵养量为174.8639亿m3-378.4538亿m3,多年平均水源涵养量265.0475亿m3,其中草地与林地多年平均水源涵养量分别占黄河全流域水源涵养总量的52.94%和24.27%。全流域水源涵养量呈现上下游地区较高,中游地区较低的分布格局。(2)全局莫兰指数为0.875,表明黄河流域水源涵养服务在空间上呈现聚集分布,以低-低聚集与高-高聚集为主。(3)1980-2020年不同地类平均水源涵养能力排序:灌木林>有林地>高覆盖草地>其他林地>中覆盖草地>低覆盖草地>旱地>建设用地>未利用地>水田>水域。(4)降水量是影响黄河流域水源涵养量变化的主要驱动因子,降水量与土地利用间交互作用对黄河流域水源涵养服务功能空间分异解释力显著增强。研究结果可为黄河流域生态系统管理与高质量发展提供重要参考。

    Abstract:

    The Yellow River Basin is an important ecological barrier in China. With the increasing interference of human activities, the ecological problems of the Yellow River Basin have received more attention from the academic community. On April 1, 2023, the Yellow River Protection Law of the People's Republic of China was formally implemented, which explicitly required to strengthen the synergistic management of the Yellow River's water resources, water environment, and water ecology in order to realize the harmony between human and nature. It is of great significance to study water conservation service function to promote ecological protection and high-quality development in the Yellow River Basin. Based on the InVEST model, this study quantitatively evaluated the water conservation service function of the Yellow River Basin from 1980 to 2020. We analyzed the spatial distribution pattern of the water conservation service function by the spatial autocorrelation and analyzed the factors affecting change of the water conservation service function via geographical detector. The results showed that: (1) the water conservation volume of the Yellow River Basin from 1980 to 2020 ranged from 17486.39 million m3 to 37845.38 million m3, with the averagely annual water conservation volume of 26504.75 million m3. The multi-year average water conservation volume of the grassland and forestland accounted for 52.94% and 24.27% of the total water conservation volume in the Yellow River Basin, respectively. A higher distribution pattern in the upstream and downstream regions and a lower distribution pattern in the middle reaches were presented. (2) The global Moran index was 0.875, indicating that the spatial distribution of water conservation service in the Yellow River Basin showed aggregation distribution, which was dominated by low-low aggregation and high-high aggregation. (3) From 1980 to 2020, the order of average water conservation amount of different land types was shrubbery>forest land>high cover grassland>other forest land>medium cover grassland>low cover grassland>dry land>construction land>unused land>paddy field>water area. (4) Precipitation was the main driving factor affecting water conservation in the Yellow River Basin. The interaction between precipitation and land use significantly enhanced the explanatory power of spatial differentiation of water conservation service functions in the Yellow River Basin. The results could provide an important reference for the ecosystem management and high-quality development of the Yellow River Basin. Regarding the uncertainties of the methodology and model, research on parameter localization should be strengthened. More social and economic factors should be taken into account such as population and GDP in the future.

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吕明轩,张红,贺桂珍,张霄羽,刘勇.黄河流域水源涵养服务功能动态演变及驱动因素.生态学报,2024,44(7):2761~2771

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