• 中文核心期刊
  • 中国科技核心期刊
  • RCCSE中国核心学术期刊
  • Scopus, DOAJ, CA, AJ, JST收录期刊
高级检索

采煤沉陷盆地主断面上凹形黄土坡面形变特征及土壤侵蚀效应

Deformation characteristics and soil erosion effect of concave loess slope on main cross-section of coal mining subsidence basin

  • 摘要: 深刻理解坡面尺度下采煤沉陷的水土流失效应是实现黄河中游煤炭开采区水土流失精准防控的重要科学基础。以陕北典型黄土采煤沉陷盆地为研究区,通过FLAC3D数值模拟,从“坡位(边坡部位、中心部位、边缘部位)、自然坡度(5°、15°、25°、35°、45°)、坡向(顺坡、逆坡)”三元耦合的角度揭示采煤沉陷盆地主断面上凹形黄土坡面形变特征,基于CSLE模型和经验模型阐明凹形黄土沉陷坡面的土壤侵蚀效应。研究结果表明:在“坡位、自然坡度、坡向”三元耦合下,采煤沉陷会导致凹形黄土坡面的坡度增大,其中坡位是关键控制因子,坡度增幅随坡位由边缘向中心过渡呈“先升后降”的变化趋势,并在“边坡部位+自然坡度5°+顺坡”条件下达到最大,为11.85%。无论是在“年侵蚀降雨”尺度还是“典型场次侵蚀降雨”尺度下,采煤沉陷均会导致凹形黄土坡面的土壤侵蚀模数增大,增幅在“边坡部位+自然坡度5°+顺坡”条件下达到最大,分别为11.40%、10.14%,坡位仍是关键控制因子。建议将根据地表凹形黄土坡面在采煤沉陷区的相对位置关系调整优化地下采煤工作面的布置,作为黄河中游陕北黄土采煤沉陷区水土流失效应的采前精准防控策略。

     

    Abstract: A deep understanding of the erosion loss effect induced by coal mining subsidence on the slope scale is an important scientific basis for the accurate prevention and control of erosion loss in the coal mining area in the middle reaches of the Yellow River. Taking the typical loess mining subsidence basin in Northern Shaanxi as the research area, through FLAC3D numerical simulation, the deformation characteristics of concave loess slope on the main cross-section of the mining subsidence basin are revealed from the perspective of the triadic coupling of "slope position (slope edge, center, margin), natural slope gradient (5°, 15°, 25°, 35°, 45°), and slope aspect (downslope, upslope)". Based on the CSLE model and the empirical model, the soil erosion effect of the concave loess subsidence slope is clarified. The results show that under the triadic coupling of "slope position, natural slope gradient, and slope aspect", coal mining subsidence leads to an increase in the gradient of concave loess slopes, with slope position being the key controlling factor. The increase of slope gradient increases first and then decreases with the transition of slope position from margin to center, and reaches the maximum of 11.85% under the conditions of "slope edge position + natural slope gradient of 5° + downslope aspect". Whether in the scale of annual erosion rainfall or typical field erosion rainfall, coal mining subsidence will lead to the increase of soil erosion modulus of concave loess slope, and the increase will reach the maximum under the condition of "slope edge position + natural slope gradient of 5°+ downslope aspect", which is 11.40% and 10.14% respectively. Slope position is still the key control factor. It is suggested that the layout of underground coal mining face should be adjusted and optimized according to the relative position relationship of surface concave loess slope in coal mining subsidence area as the pre-mining precise prevention and control strategy of erosion loss effect in loess mining subsidence area of Northern Shaanxi in the middle reaches of the Yellow River.

     

/

返回文章
返回