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基于补给地下水的黄河源区湿地网络构建及评估

Construction and evaluation of a wetland network in the Yellow River source region based on groundwater recharge

  • 摘要: 黄河源区湿地是黄河重要的水源涵养地,对维持流域经济社会和生态系统的安全具有非常重要的战略意义。利用MSPA-Conefor-MCR 模型构建黄河源区的湿地生态网络,通过计算黄河源区湿地补给地下水的水量和价值量分析其功能特征,并采用连接鲁棒性指数评估其结构特征。研究结果表明,黄河源区湿地生态网络由74个生态节点和670条生态廊道组成。除水体外面积较大的湿地斑块,补给地下水的水量和价值量较高,在补给价值量较大的斑块中,大部分为寒钙土、草甸土和黑毡土。在功能性上,黄河源区补给地下水价值量较大的湿地斑块与周围湿地的连接性较强,这些湿地斑块周围的生态阻力值跨度较大,与其相连的湿地斑块权重大小具有一定的随机性。在结构性上,东北部和东南部地区的湿地斑块相互建立联系的潜力较强,而西北部地区则较弱。

     

    Abstract: Wetlands in the source region of the Yellow River are critical for water regulation and serve as a key water supply for the river, playing a strategic role in ensuring the economic, social, and ecological security of the basin. The MSPA-Conefor-MCR model was applied to construct the wetland ecological network in this region, and its functional characteristics were analyzed by quantifying the groundwater recharge volume and value provided by the wetlands. The structural characteristics were evaluated using the connectivity robustness index. The results show that the wetland ecological network in the Yellow River source region comprises of 74 ecological nodes and 670 ecological corridors. Larger wetland patches, excluding water bodies, exhibit higher groundwater recharge volumes and greater recharge value. Among the patches with the highest recharge values, most are located in cold calcareous soils, meadow soils, and black felt soils. Functionally, wetland patches with higher groundwater recharge values are better connected to surrounding wetlands. These patches also have a wider range of ecological resistance values, and the weight sizes of the wetland patches they connect to show some degree of randomness. Structurally, wetland patches in the northeastern and southeastern regions have a stronger potential for connection, while those in the northwestern region have weaker connectivity.

     

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