叶立娟,刘翠善,王国庆,等. 2000—2020年黄河源区水源涵养能力模拟与分析[J]. 水利水运工程学报,2023(6):46-56.. doi: 10.12170/20230509002
引用本文: 叶立娟,刘翠善,王国庆,等. 2000—2020年黄河源区水源涵养能力模拟与分析[J]. 水利水运工程学报,2023(6):46-56.. doi: 10.12170/20230509002
(YE Lijuan, LIU Cuishan, WANG Guoqing, et al. Modeling and analysis of water conservation capacity in the source region of the Yellow River from 2000 to 2020[J]. Hydro-Science and Engineering, 2023(6): 46-56. (in Chinese)). doi: 10.12170/20230509002
Citation: (YE Lijuan, LIU Cuishan, WANG Guoqing, et al. Modeling and analysis of water conservation capacity in the source region of the Yellow River from 2000 to 2020[J]. Hydro-Science and Engineering, 2023(6): 46-56. (in Chinese)). doi: 10.12170/20230509002

2000—2020年黄河源区水源涵养能力模拟与分析

Modeling and analysis of water conservation capacity in the source region of the Yellow River from 2000 to 2020

  • 摘要: 黄河源区是黄河流域的重要产水区和水源涵养区,其水源涵养能力对河流上中下游区域的社会经济发展影响重大。基于InVEST模型计算了2000—2020年黄河源区的产水量和水源涵养量,结果表明,多年平均产水总量和水源涵养总量分别为198.8×108和35.3×108 m3。产水量和水源涵养量空间分布基本一致,呈现自东向西、自南向北递减的特点。在研究时段内,二者均呈显著上升趋势,整体上升速率分别为3.8和0.7 mm/a,自东南向西北依次表现为极显著上升、显著上升、轻微上升及没有明显变化。各土地利用类型的水源涵养总量由高到低分别为草地、耕地、湿地、林地、未利用地及城镇用地。降水是导致水源涵养量变化的主要原因,其次是蒸散发和土地利用类型。水源涵养量对不同土地利用类型变化响应的结果表明,湿地面积增大能为黄河源区水源涵养量提供最大的增益,其次为草地,城镇用地面积增大对其增益最小。

     

    Abstract: The source area of the Yellow River plays a vital role in water yield and conservation within the Yellow River Basin, impacting socio-economic development along the river’s upper, middle, and lower reaches. This study employs the InVEST model to analyze the water yield and conservation capacity of the Yellow River source area from 2000 to 2020. The findings indicate an average annual water yield of 198.8×108 m3 and a water conservation capacity of 35.3×108 m3. Spatially, both water yield and conservation capacity exhibit similar patterns, gradually decreasing from east to west and south to north. Over the study period, both metrics display a significant increasing trend, with growth rates of 3.8 mm/a and 0.7 mm/a, respectively. Notably, the increase varies across regions, ranging from highly significant to no significant change as one moves from the southeast to the northwest. The land use types with the highest to lowest total water conservation capacities are grassland, cropland, wetland, forest, bareland, and urban land. Precipitation serves as the primary driver of water conservation changes, followed by evapotranspiration and land use. Furthermore, the study reveals that an increase in wetland area yields the greatest improvement in water conservation within the Yellow River source area, followed by grassland, while an increase in urban land area provides the least improvement.

     

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