高级检索

    极端暴雨下红壤丘陵区典型小流域重力侵蚀特征分析

    Analysis of Gravitational Erosion Characteristics in a Typical Small Watershed of the Red Soil Hilly Region Under Extreme Rainstorm Conditions

    • 摘要: 【目的】揭示极端暴雨后红壤丘陵小流域梯田损毁与重力侵蚀的数量、形态及空间组成,为灾后水土保持调查与修复提供依据。【方法】以武平县黄沙坑溪小流域为对象,2024年9月结合无人机航摄与实地核查,调查6块梯田和16处斑块,叠加DEM与土地利用数据统计,对流域内梯田损毁状况及重力侵蚀斑块进行解译、核查与统计分析。【结果】解译识别重力侵蚀斑块508处,总面积0.63 km²,占流域面积1.88%;实地核查16处均为浅层滑坡,平面形态多呈扇形或条形。重力侵蚀面积在5°~15°坡度带占66.40%(该带占流域面积59.24%),在有林地中占82.06%(有林地占流域面积83.57%)。梯田面积192.15 hm²,解译损毁面积0.21 hm²。6块典型梯田中,田坎总长798.5 m,损毁52.0 m,长度损毁率6.51%;有排水设施的4块梯田均未测量到田坎长度损毁,无排水设施的2块梯田均出现垮塌或滑坡。【结论】极端暴雨条件下,红壤丘陵小流域内梯田损毁与浅层滑坡等重力侵蚀现象并存,且受排水条件、坡度分布和土地利用格局共同影响,灾后水土保持工作应将梯田工程损毁与重力侵蚀斑块纳入协同调查体系并实施分类修复。

       

      Abstract: Objective This study aimed to reveal the quantity, morphology, and spatial composition of terrace damage and gravity erosion in a small watershed in the red soil hilly region after an extreme rainstorm, so as to provide a basis for post-disaster soil and water conservation investigation and restoration. Methods Taking the Huangshakengxi small watershed in Wuping County as the study area, UAV aerial photography and field verification were combined in September 2024 to investigate six terraced fields and 16 erosion patches. DEM and land-use data were overlaid for statistical analysis, and terrace damage and gravity erosion patches within the watershed were interpreted, verified, and statistically analyzed. Results A total of 508 gravity erosion patches were interpreted and identified, covering an area of 0.63 km² and accounting for 1.88% of the watershed area. Field verification showed that all 16 patches were shallow landslides, with planar shapes mostly fan-shaped or strip-shaped. The gravity erosion area distributed in the 5°~15° slope zone accounted for 66.40% of the total gravity erosion area, while this slope zone accounted for 59.24% of the watershed area. The gravity erosion area in forest land accounted for 82.06%, while forest land accounted for 83.57% of the watershed area. The terrace area was 192.15 ha, and the interpreted damaged area was 0.21 ha. Among the six typical terraces, the total length of terrace risers was 798.5 m, of which 52.0 m was damaged, with a length-based damage rate of 6.51%. No length-based damage was measured in the four terraces with drainage facilities, whereas collapse or landslide occurred in both terraces without drainage facilities. Conclusions Under extreme rainstorm conditions, terrace damage and gravity erosion such as shallow landslides coexisted in the red soil hilly small watershed, and were jointly influenced by drainage conditions, slope distribution, and land-use pattern. Therefore, post-disaster soil and water conservation work should incorporate both terrace engineering damage and gravity erosion patches into a coordinated investigation system and implement classified restoration measures.

       

    /

    返回文章
    返回