Niu Ning, Fan Jihui, Yang Ziyan
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610299, China.
University of Chinese Academy of Sciences, Beijing, 100049, China.
Sci Rep. 2025 Jul 1;15(1):22413. doi: 10.1038/s41598-025-05080-3.
Guizhou Province, a typical karst region, experiences abundant rainfall but exhibits weak water conservation (WC) capacity. In this study, the InVEST water yield model was employed to quantify long-term WC dynamics (1983-2022). Spatiotemporal trends were analyzed using Mann-Kendall tests and Sen's slope estimator. Additionally, the response of WC to climate and land use drivers was further discussed. The results showed that the average annual WY and WC were 547.62 mm and 364.70 mm (in depth), respectively. The spatial distribution exhibited high in the east and low in the northwest. WC showed a decreased trend in the west and increased in the east from 1983 to 2022. The spatial analysis emphasized that high-WC areas should prioritize natural protection, while low-WC regions require artificial restoration, particularly significant decreasing trends that need urgent intervention. Variations in WC were driven by the combined effects of climate factors and land use types, with forest land and grassland demonstrating the highest WC capacity. This study clarifies the spatiotemporal evolution and driving mechanisms of WC, providing scientific support for maintaining and enhancing WC strategies in Guizhou Province.
贵州省是典型的喀斯特地区,降雨充沛,但保水能力较弱。本研究采用InVEST产水量模型量化长期保水动态(1983 - 2022年)。利用曼-肯德尔检验和森斜率估计器分析时空趋势。此外,还进一步探讨了保水对气候和土地利用驱动因素的响应。结果表明,年平均产水量和保水量分别为547.62毫米和364.70毫米(深度)。空间分布呈现东部高、西北部低的特点。1983年至2022年期间,西部地区保水呈下降趋势,东部地区则呈上升趋势。空间分析强调,高保水地区应优先进行自然保护,而低保水地区需要人工修复,特别是那些有显著下降趋势的地区需要紧急干预。保水的变化是由气候因素和土地利用类型的综合作用驱动的,其中林地和草地的保水能力最强。本研究阐明了保水的时空演变及其驱动机制,为贵州省维持和提高保水策略提供了科学支持。