漓江东岸冠岩地下河流域果园石漠化分布特征及其演变规律
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X171.1

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国家重点研发计划课题“峰丛洼地关键带水土资源生态调控技术”(2022YFF1300702); 桂林市重大专项计划“漓江核心区喀斯特石漠化修复及特色药业关键技术研究与示范”(20220102-1); 中国地质调查局项目(DD20190502,DD20230453); 2023年创新平台和人才计划“气候变化条件下典型岩溶区土壤固碳效率提升关键技术研究”(20230116-3)


Distribution and evolution of orchard rocky desertification in Guanyan underground river basin along eastern bank of Lijiang River
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    [目的] 分析漓江东岸冠岩地下河流域2010—2020年的土地利用以及果园石漠化演变过程,探究果园石漠化景观格局分布特征与内在演变规律,为该区乃至漓江流域生态保护修复与景观资源可持续利用提供地质依据与决策建议。[方法] 以冠岩地下河流域土地利用类型以及石漠化为研究对象,基于第二次、第三次全国土地调查数据以及遥感影像数据,运用GIS技术平台和面积转移矩阵模型分析研究区果园石漠化演变规律。[结果] ①冠岩地下河流域土地利用以耕地、果园、林地为主,其中耕地与草地面积呈现减少趋势,果园、林地、水域以及其他用地呈现增加趋势。②2010—2020年,冠岩地下河流域果园石漠化面积减少1.34 km2,减少比例为7.90%,果园石漠化状况整体表现出持续向好的良好态势,但中度石漠化与重度石漠化面积呈增加趋势,其中非石漠化转变为石漠化的面积1.51 km2。③结合冠岩地下河流域2010—2020年果园石漠化演变过程,10 a间果园石漠化改善面积为1.79 km2,恶化面积为1.78 km2。[结论] 流域内果园石漠化总体呈现出积极改善的趋势,但局部区域存在石漠化恶化扩张或新增石漠化现象,主要表现为果园本身以及部分林地发生石漠化蔓延。因而冠岩地下河流域后期生态环境恢复与保护的重点应是加强现有果园的科学种植与管理,逐步恢复灌木林等植被,大力发展林下复合经营种植模式,在现有石漠化治理措施基础之上防止果园石漠化进一步恶化。

    Abstract:

    [Objective] The land use and the evolution process of orchard rocky desertification in Guanyan underground river basin along the eastern bank of Lijiang River from 2010 to 2020 were analyzed, and the distribution characteristics and internal evolution law of orchard rocky desertification landscape pattern were explored, so as to provide geological basis and decision-making suggestions for ecological protection and restoration and sustainable utilization of landscape resources in this area and even in Lijiang River basin. [Methods] Taking the land use type and rocky desertification in Guanyan underground river basin as the research object, based on the second and third national land survey data and remote sensing image data, the GIS technology platform and area transfer matrix model were used to analyze the evolution law of orchard rocky desertification in the study area. [Results] ① Cultivated land, orchards, and forest land were the main land uses in the underground river basin. The areas of cultivated land and grassland decreased, while the areas of orchard, forest land, water, and other land increased. ② The area of rocky desertification in orchards in the Guanyan underground river basin decreased by 1.34 km2 from 2010 to 2020, a reduction of 7.90%. Overall, the rocky desertification was continuously decreasing in the orchards. However, the areas affected by moderate and severe rocky desertification increased. A total of 1.51 km2 of nonrocky desertification area transformed into rocky desertification. ③ In a 1.79 km2 area, the orchard rocky desertification decreased; however, the desertification worsened in a 1.78 km2 area from 2010 to 2020. [Conclusion] Overall, the rocky desertification in orchards within the watershed was decreases. However, rocky desertification was increasing and expanding to some new areas, which mainly manifested as the spread of rocky desertification in the orchard and in some forested areas. Therefore, the focus of ecological environmental restoration and protection in the underground Guanyan river basin should be on strengthening the scientific planting and management of existing orchards, gradually restoring shrubs and other vegetation, vigorously developing agroforestry planting methods, and preventing further increases in rocky desertification through the application of on existing rocky desertification control measures.

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李航,罗为群,张谭锋,涂纯.漓江东岸冠岩地下河流域果园石漠化分布特征及其演变规律[J].水土保持通报,2025,45(2):73-80,101

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  • 收稿日期:2024-08-29
  • 最后修改日期:2024-12-04
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  • 在线发布日期: 2025-05-16
  • 出版日期: 2025-04-15