喀斯特地区安顺市土壤侵蚀时空变化特征及驱动因素
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贵州师范大学喀斯特研究院

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S157.1

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国家自然科学基金青年科学基金项目(42201013);贵州省科技计划项目(黔科合基础-zk[2024]一般444号) ;贵州省教育厅高等学校科学研究项目(黔教技[2022]131号);贵州师范大学学术新苗基金项目(黔师新苗[2021]B01号)


Characteristics and drivers of spatial and temporal soil erosion in Anshun City, Karst region
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School of Karst Science,Guizhou Normal University

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    摘要:

    [目的]探索西南喀斯特地区安顺市土壤侵蚀时空演变规律、驱动因子以及驱动因子相互间交互作用,有助于该地区石漠化治理和水土资源管理。[方法]采用优化后的RUSLE模型估算2005-2020年安顺市土壤侵蚀,同时利用随机森林模型(RF) 揭示土壤侵蚀的驱动因子,并估算驱动因子相互作用对2005-2020年安顺市土壤侵蚀的影响。[结果] (1)2005-2020年安顺市土壤侵蚀总体上呈现低强度土壤侵蚀分布在中部、东南部和东部地区,而高强度土壤侵蚀分布在北部和西南部地区。从时间上来看,安顺市土壤侵蚀整体上呈现改善趋势,大部分地区土壤侵蚀等级主要由高向微强度侵蚀转移,但局部地区存在侵蚀加剧现象。(2)石漠化对于安顺市土壤侵蚀有较大的影响。安顺土壤侵蚀强度与石漠化呈正相关区域占总面积59.3%,具有高度相关性。土壤侵蚀随着石漠化强度增加呈现先增加后减少的趋势。(3)安顺市发生土壤侵蚀最主要的土地利用类型为林地、耕地和草地,总体上来看土壤侵蚀速率依次为林地<草地<耕地。(4)对土壤侵蚀驱动因子分析显示,植被覆盖与管理因子对研究区土壤侵蚀时空动态变化解释力最强,其次是水土保持措施因子、石漠化强度。驱动因子交互作用结果表明,植被覆盖与管理因子与水土保持措施因子交互作用为主导因素,而排名靠前的交互作用中均有植被覆盖与管理因子参与。[结论]2005-2020年安顺市土壤侵蚀强度整体呈好转趋势,但部分地区存在侵蚀加剧现象。植被、石漠化强度和土地利用对安顺市土壤侵蚀影响最强。因此,未来水土治理过程中需要重点关注植被覆盖、石漠化强度和土地利用变化。

    Abstract:

    [Objective] To explore the spatial and temporal evolution of soil erosion, driving factors and the interaction between driving factors in Anshun City, a karst area in southwest China, which can help the management of rock desertification and soil and water resources in the area. [Methods] The optimised RUSLE model was used to estimate soil erosion in Anshun City from 2005 to 2020, while the Random Forest Model (RF) was used to reveal the driving factors of soil erosion, and to estimate the effects of driving factor interactions on soil erosion in Anshun City from 2005 to 2020. [Results] (1) from 2005 to 2020, soil erosion in Anshun City generally shows that low-intensity soil erosion is distributed in the central, southeastern and eastern regions, while high-intensity soil erosion is distributed in the northern and southwestern regions. From the time point of view, soil erosion in Anshun City as a whole shows a trend of improvement, most of the areas of soil erosion grade mainly from high to micro-intensity erosion transfer, but there are local areas of erosion exacerbation phenomenon. (2) Rocky desertification has a greater impact on soil erosion in Anshun. The soil erosion intensity of Anshun is positively correlated with rocky desertification in the area accounting for 59.3% of the total area, which is highly correlated. Soil erosion with the increase of rocky desertification intensity shows the trend of increasing and then decreasing. (3) The most important land use types in Anshun City where soil erosion occurs are forest land, arable land and grassland, and the overall rate of soil erosion is in the order of forest land < grassland < arable land. (4) The analysis of the driving factors of soil erosion showed that the vegetation cover and management factor had the strongest explanatory power for the spatial and temporal dynamics of soil erosion in the study area, followed by the factor of soil and water conservation measures and the intensity of rock desertification. The results of driver interaction showed that the interaction between vegetation cover and management factor and soil and water conservation measures factor was the dominant factor, and the top ranked interactions all had the participation of vegetation cover and management factor. [Conclusion] Soil erosion intensity in Anshun City showed an overall trend of improvement from 2005 to 2020, but there was an increase in erosion in some areas. Vegetation cover, rock desertification intensity and land use have the strongest influence on soil erosion in Anshun City. Therefore, the future soil and water management process needs to focus on vegetation cover, rock desertification intensity and land use changes.

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  • 收稿日期:2024-07-09
  • 最后修改日期:2024-09-17
  • 录用日期:2024-09-18
  • 在线发布日期: 2025-01-09
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