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矿区地表形变对土壤湿度的影响

Spatial response relationship of soil moisture to surface deformation in mining areas

  • 摘要: 准确了解由开采活动导致的矿区地表形变对土壤湿度的影响,对干旱半干旱矿区煤炭资源绿色开采具有重要参考意义。以神东矿区内的7个矿区为研究对象,基于土壤湿度监测指数S-SMMI表征土壤湿度状况,利用PS-InSAR技术获取矿区地表形变状况,定量分析矿区地表形变与土壤湿度之间的关系。结果表明:地下矿地表沉陷呈中心沉陷最大、向四周逐渐减少的盆地状,S-SMMI均值变化规律为沉陷盆地>沉陷斜坡>沉陷边缘。其中,除4号地下矿沉陷盆地S-SMMI均值低于沉陷边缘外,其余地下矿沉陷盆地S-SMMI均值均高于沉陷边缘,说明沉陷越严重的区域土壤湿度越小,两者之间存在负相关关系;地下矿对周边土壤湿度的影响范围为3 000~5 000 m,距离越远,土壤湿度状况越趋于平稳。其中,地下矿土壤湿度影响区可分为3级:强影响区(0~500 m)、弱影响区(500~3 000 m)、无影响区(5 000 m以外)。对于露天矿,在复垦前,S-SMMI平均值较高,土壤湿度小;在复垦后,地表形变减缓,S-SMMI平均值逐渐降低,土壤湿度增大,说明复垦能够提升土壤湿度。在相同的地貌类型下,神东矿区土壤湿度以中强度开采区最高(S-SMMI=0.539),极高强度开采区最低(S-SMMI=0.653)。综上所述,地下矿地表沉陷对土壤湿度产生了负面影响,影响距离为3 000~5 000 m;露天矿复垦后,地表形变量显著减小。这不仅改善了矿区的植被覆盖状况,还有助于提高土壤湿度。因此,地下矿在开采过程中应该注重沉陷盆地处的土地修复,露天矿在开采过程中应边开采边修复,防止土壤湿度降低,导致地表生态环境进一步恶化。

     

    Abstract: Accurately understanding the impact of surface deformation on soil moisture caused by mining activities is of great reference significance for the green mining of coal resources in arid and semi-arid mining areas. In this study, seven mining areas in Shendong mining area were taken as the research objects, and the soil moisture status was characterized based on the soil moisture monitoring index S-SMMI, PS-InSAR technology was used to obtain the surface deformation of the mining area, and the relationship between the surface deformation and soil moisture in the mining area was quantitatively analyzed. The results show that: The surface subsidence of the well mine is a basin with the largest subsidence in the center and gradually decreasing to the surrounding area, and the overall change law of the S-SMMI mean is that the subsidence slope > subsidence edge of the subsidence basin >. Except for Well 4, the mean SMMI of the subsidence basin is lower than that of the subsidence edge, and the mean SMMI of the subsidence basin of the rest of the wells is higher than that of the subsidence edge, indicating that the soil moisture in the more severe the subsidence area is smaller, and there is a negative correlation between the two. The influence range of well mines on the surrounding soil moisture is about 3 000−5 000 m, and the farther the distance, the more stable the soil moisture condition becomes, among which the soil moisture influence area of well mines can be divided into three levels: strong influence area (0−500 m), weak influence area (500−3 000 m), and no influence area (beyond 5 000 m). For open-pit mines, before reclamation, the average S-SMMI is relatively high, and the soil moisture is low. Under the same geomorphological type, the soil moisture in the Shendong Mining Area was highest in the medium-intensity mining regions (S-SMMI=0.539) and lowest in the very high-intensity mining regions (S-SMMI=0.653). After reclamation, the surface deformation slows down, the average S-SMMI gradually decreases, and the soil moisture increases, indicating that reclamation can enhance soil moisture. In summary, the surface subsidence of underground mines has a negative impact on soil moisture, and the impact distance is about 3 000−5 000 m. After the reclamation of the open-pit mine, the surface deformation significantly decreased. This not only improved the vegetation coverage in the mining area but also helped increase soil moisture. Therefore, in the process of mining, underground mines should pay attention to the land restoration in the subsidence basin, and the open-pit mines should be repaired while mining in the process of mining, so as to prevent the further deterioration of the surface ecological environment caused by the reduction of soil moisture.

     

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