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干旱区地理 ›› 2025, Vol. 48 ›› Issue (9): 1531-1540.doi: 10.12118/j.issn.1000-6060.2024.611 cstr: 32274.14.ALG2024611

• 水文与水资源 • 上一篇    下一篇

宁夏小流域尺度水土资源耦合特征及影响因素

徐建斌1(), 曹小曙2()   

  1. 1.山西财经大学资源环境学院,山西 太原 030006
    2.广州大学建筑与城市规划学院,广东 广州 510006
  • 收稿日期:2024-10-11 修回日期:2025-01-04 出版日期:2025-09-25 发布日期:2025-09-17
  • 通讯作者: 曹小曙(1970-),男,博士,教授,主要从事国土空间生态修复等相关研究. E-mail: caoxsh@snnu.edu.cn
  • 作者简介:徐建斌(1991-),男,博士,副教授,主要从事生态经济、乡村地理相关研究. E-mail: xujianbin@sxufe.edu.cn
  • 基金资助:
    国家自然科学基金(42201265);教育部人文社会科学研究项目(22YJCZH200);山西省基础研究计划(20210302123305)

Coupling characteristics and influencing factors of water and soil resources at the small watershed scale in Ningxia

XU Jianbin1(), CAO Xiaoshu2()   

  1. 1. College of Resources and Environment, Shanxi University of Finance and Economics, Taiyuan 030006, Shanxi, China
    2. College of Architecture and Urban Planning, Guangzhou University, Guangzhou 510006, Guangdong, China
  • Received:2024-10-11 Revised:2025-01-04 Published:2025-09-25 Online:2025-09-17

摘要:

水土资源的耦合协调对于小流域生态系统服务功能的可持续发展具有重要意义。以宁夏小流域为研究单元,采用耦合协调度模型对研究区水土资源耦合协调度进行测度,并采用多尺度地理加权回归模型探究了水土资源耦合协调度的影响因素及空间异质性。 结果表明:(1) 2005—2020年宁夏小流域水土资源耦合协调度从0.37上升到0.43,区域水土资源匹配程度从失调向协调方向发展。(2) 宁夏小流域水土资源耦合协调度呈现出南高北低的空间格局,且2000—2020年南部小流域水土资源耦合协调度的高值区向周边扩展。(3) 宁夏小流域的梯田面积占比、县域可达性和年平均降水量对水土资源耦合协调度会产生显著的正向影响,而年平均气温、植被覆盖度和侵蚀强度对小流域的水土资源耦合协调度会起到显著负向影响;相较于宁夏北部小流域,小流域梯田面积占比和年平均气温对宁夏南部小流域的水土资源耦合协调度影响较大,而县域可达性和年平均降水量对宁夏南部小流域水土资源耦合协调度影响较小。研究结果可为宁夏小流域尺度水土保持措施的科学规划提供参考。

关键词: 水土保持, 水土资源耦合, 耦合协调度, 空间相关性, 小流域, 宁夏

Abstract:

The coupling coordination of water and soil resources is of great significance to the sustainable development of ecosystem services in small watersheds. Taking small watersheds of Ningxia, China as the research unit, this study employs the coupling coordination degree model to measure the coupling coordination degree of water-soil resources in the study area. Additionally, the multi-scale geographically weighted regression model is used to explore the influencing factors and spatial heterogeneity of the coupling coordination degree of water-soil resources. The results indicate that: (1) From 2005 to 2020, the coupling coordination degree of water-soil resources in small watersheds of Ningxia increased from 0.37 to 0.43, demonstrating a transition from imbalance to coordination in the regional water and soil resource matching degree. (2) The coupling coordination degree of water-soil resources in small watersheds of Ningxia exhibits a spatial pattern of being higher in the south and lower in the north. Furthermore, from 2000 to 2020, areas of water-soil resources having a coupling coordination degree of high value expanded outward in the southern small watersheds. (3) The proportion of terraced field area, county-level accessibility, and annual average precipitation exert a significant positive impact on the coupling coordination degree of water-soil resources, whereas annual average temperature, vegetation coverage, and erosion intensity have a significant negative impact. The proportion of terraced field area and annual average temperature exert a greater influence on the coupling coordination degree of water-soil resources in the southern small watersheds of Ningxia compared to northern ones, while county-level accessibility and annual average precipitation demonstrate a more significant impact on the same coupling coordination degree in the northern small watersheds of Ningxia than in the southern counterparts. The findings of this study provide a scientific reference for the planning of soil and water conservation measures at the small watershed scale in Ningxia.

Key words: soil and water conservation, soil and water resources coupling, coupling coordination degree, spatial relevance, small watersheds, Ningxia