不同降雨历时下采煤塌陷区土壤优先流特征研究
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东华理工大学

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中图分类号:

X132?????

基金项目:

国家自然科学基金“黄河中游采煤塌陷区裂缝优先流形成机制及运移过程”(42162021);东华理工大学博士基金“煤炭矿区流域径流过程分析及影响因素评价”(DHBK2019093);江西省水利科技重点项目“赣抚平原灌区抗旱保灌水资源配置技术研究”(202325ZDKT01);南昌市水文地质与优质地下水资源开发利用重点实验室开放基金“宁都蓝田地热田前缘晕元素特征与地热成因分析”(20242C21)


Soil Priority Flow Characteristics in Coal Mine Subsidence Area Under Different Rainfall Duration
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East China University of Technology

Fund Project:

Foundation item:The National Natural Science Fund

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    摘要:

    [目的]开展采煤塌陷区裂缝引发的优先流特征研究,可为科学合理的开展矿区水资源管理及生态治理实践工作提供支撑。[方法]本文在神府-东胜煤田采煤塌陷区选取3条同一宽度(3 cm)的裂缝,开展相同降雨强度、不同降雨历时的染色示踪试验。采用Adobe Photoshop 2020、Image Pro Plus 6.0、SketchUp Pro 2019、Auto CAD 2019等处理软件,分析不同降雨历时下的裂缝优先流特征。[结果](1)神府-东胜采煤塌陷区优先流发生区域的土壤体积含水量、孔隙度、饱和导水率大于非优先流区域,容重和田间持水量小于非优先流区域区;(2)降雨历时分别为10min、20min、30min 时,相应的基质流深度分别为5 cm、8 cm和10 cm;优先流发育深度分别为26.4 cm、47.7 cm和44.3 cm。降雨历时越长,基质流和优先流发育越深;(3)总体上,各试验点染色面积比均随着土层深度增加呈现减小趋势,形态上表现为S形状。当降雨历时短时,染色面积比随着土层深度变化的幅度较小;当降雨历时较长时,染色面积比曲线波动增大。(4)总体上,随着土壤深度的增加,宽染色路径的数量在减少,细小染色路径的数量增加,染色路径总数呈现出先增加后减小的趋势。且降雨历时越长,相同深度处土壤染色路径越宽,宽路径数量更多。[结论]研究成果可为煤炭矿区土地复垦和生态治理提供科学依据。

    Abstract:

    Abstract:[Objective] The research on the preferential flow characteristics triggered by cracks in the coal mining subsidence area can provide support for the scientific and rational development of water resource management and ecological management practice in the mining area. [Methods] Three cracks of the same width (3 cm) were selected in the coal mining subsidence area of Shenfu-Dongsheng Coal Field to carry out the staining tracer test with the same rainfall intensity and different rainfall durations. Processing software such as Adobe Photoshop 2020, Image Pro Plus 6.0, SketchUp Pro 2019, and Auto CAD 2019 were used to analyze the preferential flow characteristics of cracks under different rainfall calendars. [Results] (1) the soil volumetric water content, porosity, and saturated hydraulic conductivity in the priority flow occurrence area of the Shenfu-Dongsheng coal mining collapse area were greater than those in the non-priority flow area, and the volumetric weight and field water-holding capacity were less than those in the non-priority flow area zone; (2) When the rainfall duration was 10min, 20min and 30min, the corresponding depths of substrate flow were 5cm, 8cm and 10cm, respectively; and the depths of preferential flow were 26.4cm, 47.7cm and 44.3cm, respectively. the longer the rainfall duration, the deeper the development of substrate and preferential flow; (3) In general, the staining area ratio at each test site showed a decreasing trend with the increase of soil layer depth, and the morphology showed an S shape. When the rainfall duration was short, the magnitude of change in the coloring area ratio with soil layer depth was small; when the rainfall duration was long, the fluctuation of the coloring area ratio curve increased. (4) In general, with the increase of soil depth, the number of wide staining paths was decreasing, the number of fine staining paths was increasing, and the total number of staining paths showed a tendency of increasing and then decreasing. And the longer the rainfall duration, the wider the soil staining paths at the same depth, and the number of wide paths was more. [Conclusion] The f indings can provide scientific basis for land reclamation and ecological management in coal mining areas.

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  • 收稿日期:2024-08-04
  • 最后修改日期:2024-09-03
  • 录用日期:2024-09-19
  • 在线发布日期: 2025-01-09
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