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应用生态学报 ›› 2025, Vol. 36 ›› Issue (8): 2487-2496.doi: 10.13287/j.1001-9332.202508.023

• 研究论文 • 上一篇    下一篇

西汉水流域水源涵养时空分异特征及影响因素

陈娜娜, 程玉菲*, 王军德   

  1. 甘肃省水利科学研究院, 兰州 730000
  • 收稿日期:2024-12-17 接受日期:2025-06-09 出版日期:2025-08-18 发布日期:2026-02-18
  • 通讯作者: *E-mail: 150152067@qq.com
  • 作者简介:陈娜娜, 女, 1990年生, 工程师。主要从事水资源与环境研究。E-mail: 1611431943@qq.com
  • 基金资助:
    甘肃省科技厅基础研究计划软科学专项(25JRZA044)、甘肃省科技厅重点研发计划项目(23YFFA0017)和甘肃省水利科学试验研究及技术推广计划项目(甘水建管发〔2025〕24号)

Spatial-temporal variations of water conservation capacity and the influencing factors in Xihanshui Basin, Northwest China

CHEN Nana, CHENG Yufei*, WANG Junde   

  1. Gansu Academy for Water Conservancy, Lanzhou 730000, China
  • Received:2024-12-17 Accepted:2025-06-09 Online:2025-08-18 Published:2026-02-18

摘要: 分析山区和小流域的水源涵养功能,及其与自然气候、人类活动之间的时空格局和相关关系,是区域生态修复和水资源管理的基础。本研究基于InVEST模型中的产水模块,结合Pearson相关系数,分析西汉水流域水源涵养量的时空变化,并利用假定情景模拟、地理探测器模型等,探索水源涵养对气候、人类活动的响应及空间分异驱动因子。结果表明: 1990—2020年,西汉水流域的水源涵养量呈整体上升趋势,平均值为38.35 mm,呈西北高、东南高、东北低以及山区高、黄土丘陵区低的空间分布格局;降水量和水源涵养量均呈现先减小后增加的变化趋势。降水量、潜在蒸散发量、气温与水源涵养量分别存在极显著正相关、显著负相关、不显著正相关关系。区域水源涵养量主要由林地、草地和耕地贡献,占比超过60%,其单位面积水源涵养量分别为61.66、41.28、33.31 -2。各驱动因子两两交互对水源涵养的解释力均高于对应单一因子解释力,土地利用程度综合指数与潜在蒸散发、土地利用程度综合指数与归一化植被指数的交互作用解释力度均较高。随着未来气候变化不确定性的增加,降水减小会成为限制西汉水流域水源涵养的关键因素;此外,推动未利用土地转化为生态地类,将促进区域生态环境质量稳步提升。

关键词: 水源涵养能力, InVEST模型, 地理探测器, 西汉水流域

Abstract: Analysis of water conservation functions of mountainous areas and small watersheds, as well as the spatio-temporal patterns and correlations between water conservation and climate and human activities, is the foundation for regional ecological restoration and water resource management. We analyzed the spatial and temporal variations of water conservation in Xihanshui Basin based on the water production module in the InVEST model, combined with the Pearson correlation coefficient. We used scenario simulation and geoDetector modeling to explore the response of water conservation to climate and human activities and spatial differentiation driving factors. The results showed that water conservation of Xihanshui Basin showed an overall upward trend from 1990 to 2020, with an average value of 38.35 mm. There was a spatial distribution pattern of high in the northwest, high in the southeast, low in the northeast, and high in the mountainous areas and low in the loess hilly areas. Both precipitation and water conservation showed a trend of first decreasing and then increasing. Precipitation, potential evapotranspiration, and temperature had highly significant positive, significant negative, and non-significant positive correlations with water conservation. The water conservation was mainly contributed by forest, grassland and cultivated land, accounting for more than 60%. Water conservation per unit area of each class was 61.66, 41.28 and 33.31 mm·km-2, respectively. The explanatory power of the pair interaction of different driving factors on the water conservation was higher than that of any single factor. The explanatory power of the interaction between the comprehensive index of land use degree and potential evapotranspiration, the comprehensive index of land use degree and NDVI, was relatively high. With the increases of uncertainty of future climate change, the decrease of precipitation would become the key factor limiting water conservation. In addition, promoting the conversion of unused land into eco-logical land types would promote the steady improvement of regional ecological environment quality.

Key words: water conservation capacity, InVEST model, geoDetector, Xihanshui Basin