钦江流域植被覆被变化及其水沙效应
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S157.1,P333

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广西自然科学基金项目“平陆运河建设背景下钦江河口咸潮入侵变化及其机制研究”(2025GXNSFHA069274); 国家自然科学基金项目“北部湾南流江三角洲潮滩响应热带气旋的动力地貌过程”(42366008)


Vegetation cover change and its water-sediment effects in Qinjiang River basin
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    [目的] 研究钦江流域植被覆被变化特征及其水沙效应,为流域治理和河流水沙调控提供科学依据。[方法] 基于2000—2021年逐月与逐年的水沙、NDVI和降水数据,以及2000—2024年逐年植被生长季的NDVI、降水与气温数据,通过相关分析、偏相关分析、多元线性回归模型分析等方法,分析钦江流域植被覆被年际和季节变化及其水沙效应。采用多元回归残差分析探讨植被覆被变化的驱动因素。[结果] ①2000—2021年钦江流域植被持续恢复,NDVI呈上升趋势,与输沙量形成显著负相关关系;植被与降水可有效解释输沙量变化。年降水量增加1 mm,年均NDVI增加0.1时,年输沙量减少3.05×104 t。②钦江流域NDVI的季节变化表现为:夏季>秋季>春季>冬季,植被对水沙过程的调节具有明显季节差异:夏季植被拦沙作用最强,输沙量与NDVI负相关;与春、冬季则呈正相关,体现出植被水土保持效应的季节非对称性。③气候变化与人类活动对植被变化的总贡献率均超过90%,气温升高和植树造林是促进植被恢复的主要因素。降水丰富和气温较高的中下游区域贡献率要高于上游,而城镇的扩张对植被覆被具有抑制作用。[结论] 钦江流域的植被恢复减沙效果明显。多元线性回归模型可以较好地模拟输沙量的变化,在北部湾河流流域具有一定的实用性。未来需重点关注城镇区域的生态建设。

    Abstract:

    [Objective] The vegetation cover change characteristics and their water-sediment effects in Qinjiang River basin were investigated in order to provide scientific support for river basin management and river watersediment regulation. [Methods] Based on the monthly and annual data of water and sediment, NDVI, and precipitation from 2000 to 2021, as well as the annual NDVI, precipitation, and temperature data during the vegetation growing season from 2000 to 2024, this study used correlation analysis, partial correlation analysis, and multiple linear regression model analysis to analyze the interannual and seasonal changes of vegetation cover and their water-sediment effects. In addition, multiple regression residual analysis was used to explore the driving factors of vegetation cover change. [Results] ① From 2000 to 2021, vegetation cover in the Qinjiang River basin showed continuous improvement, with NDVI exhibiting an increasing trend and a significant negative correlation with sediment load. The multiple linear regression results indicated that vegetation cover and precipitation effectively explained sediment load changes: an increase of 1 mm in annual precipitation combined with an increase of 0.1 in the annual mean NDVI was associated with a reduction of 3.05×104 t in annual sediment load.② Seasonal changes in NDVI in the Qinjiang River basin followed the order of summer > autumn > spring > winter. The regulation of water-sediment processes by vegetation exhibited pronounced seasonal differences. Vegetation showed the strongest sediment retention effect in summer, with a negative correlation between NDVI and sediment load, whereas positive correlations were observed in spring and winter, indicating the distinct seasonal asymmetry of soil and water conservation effects.③ Climate change and human activities jointly accounted for more than 90% of the total contribution to vegetation cover change. Temperature increase and afforestation were the main drivers of vegetation restoration. The middle and lower reaches, characterized by abundant precipitation and high temperature, showed greater contribution than the upper reaches. In contrast, urban expansion exerted an inhibitory effect on vegetation cover. [Conclusion] Vegetation restoration in Qinjiang River basin exhibits a significant sediment reduction effect. The multiple linear regression model can effectively simulate sediment load changes, demonstrating potential applicability in other river basins within the Beibu Gulf region. Future attention should be paid to ecological construction in urban areas. The findings can provide scientific support for watersediment regulation, ecological restoration, and river basin management under the background of the Pinglu Canal construction.

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李建明,黎树式,王梦竹,陈银薪.钦江流域植被覆被变化及其水沙效应[J].水土保持通报,2026,46(4):183-194

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  • 收稿日期:2025-09-29
  • 最后修改日期:2026-01-14
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  • 在线发布日期: 2026-08-25
  • 出版日期: 2026-08-15