基于无人机摄影测量的平陆运河弃土场水土流失综合防控研究
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1.广西壮族自治区自然资源生态修复中心;2.广西大学 林学院

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S157.1

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广西科技重大专项(桂科AA23023016)


Comprehensive Research on the Prevention and Control of Soil and Water Loss in the Pinglu Canal Spoil Ground Based on UAV Photography Measurement
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This study was financed by Major Project of Guangxi Science and Technology (No. AA23023016)

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    摘要:

    [目的]评估平陆运河的弃土场在不同时期的土壤侵蚀量,并模拟其水土流失倾向,探讨坡度与侵蚀强度关系,为运河类线性工程弃土场水土流失综合防控提供科学参考。[方法]以广西平陆运河的4个弃土场为例,利用无人机低空正摄技术获取弃土场不同时期的高分辨率影像与地形数据;利用GIS技术分析弃土场的水土流失倾向;结合修正的通用土壤方程(RUSLE)对各侵蚀因子进行了量化和估算。[结果](1)4个弃土场不同时期的土壤侵蚀模数的范围为1977.55 ~ 5748.96 t/(km2·a),其中侵蚀强度从轻度到强度侵蚀。(2)土壤侵蚀模数随着坡度的增大而增大,特别是在坡度为8° ~ 25°的区域,土壤侵蚀占总侵蚀量的76.8% ~ 86.4%。(3)在丘间谷地型弃土场,涓流主要沿着边缘地势较高的区域流向低洼地带;在边坡型弃土场,涓流则集中在堆土区域的上坡部分,流向坡底。[结论] 本研究表明坡度对弃土场的土壤侵蚀有显著影响,8°~ 25°的坡度区域是水土流失防治的重点区域。对于丘间谷地型弃土场,削坡和布置外侧排水设施是有效防治措施;而边坡型弃土场则应加强坡底排水和沉砂池的建设。此外,植被覆盖在防治水土流失中起到关键作用,特别是在水热条件良好的地区,植被覆盖更能有效降低土壤侵蚀风险。

    Abstract:

    [Objective] The amount of soil erosion at the spoil ground of the linear project-Pinglu Canal at different periods were evaluated and their erosion tendency was simulated. The relationship between slope and erosion intensity was explored to provide scientific reference for soil erosion control in the spoil ground. [Methods] The four spoil grounds of Pinglu Canal in Guangxi were selected as an example. The high-resolution photographic and topographic data of the spoil ground in different periods were obtained by using UAV low-altitude photography technology. The soil erosion tendency of the spoil ground was analyzed using GIS technology. The erosion factors were quantified and estimated by combining with the Revised Universal Soil Equation (RUSLE). [Results] (1) The soil erosion modulus of the four spoil grounds across different time points ranged from 1977.55 to 5748.96 t/(km2·a), with erosion intensity ranging from gentle to strong erosion. (2) Soil erosion modulus increased with slope, especially in areas with slopes of 8° to 25°, where soil erosion accounted for 76.8 to 86.4 % of the total erosion. (3) In inter-mound valley spoil grounds, the trickle flow was mainly along the higher land areas at the edges to the lowland areas. In sloped spoil ground, trickle flows were concentrated in the upslope portion of the stockpile area, towards the bottom of the slope. [Conclude] This study shows that slope was significant to the soil erosion of the spoil ground, and the slope area of 8–25° is the key area for soil erosion control. For the inter-mound valley spoil grounds, cutting the slope and arranging external drainage facilities are effective control measures. For sloped spoil ground, the construction of slope bottom drainage and sand sedimentation ponds should be strengthened. In addition, vegetation cover was a key factor in preventing soil erosion, especially in areas with favorable hydrothermal conditions, where it was more effective in reducing the risk of soil erosion.

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  • 收稿日期:2024-11-30
  • 最后修改日期:2025-01-28
  • 录用日期:2025-02-07
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