浅层煤层表面土壤的结构和水稳定性特征:空间变化和同惯性分析
Yingshun Li1, Junmeng Li1, Yanli Huang2
1School of Mines, China University of Mining & Technology, Xuzhou, 221116, China.
Journal of environmental management
|November 2, 2025
概括
矿产开采对土壤结构和水的稳定性产生重大影响,特别是在裂区域. 在非裂地区,损害传播更为明显,需要针对性的土壤保护策略.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 地质地质地质地质地质地
背景情况:
- 矿产开采导致环境退化,影响土壤结构和水的稳定性.
- 了解土壤结构和水稳定性特征之间的协惯性对于采矿区环境评估至关重要.
研究的目的:
- 分析煤矿区土壤结构和水稳定性特征之间的同惯性.
- 确定受采矿影响影响最严重的地区,并了解损害传播机制.
主要方法:
- 测量和测试土壤结构参数 (多孔度,孔径等). 和水稳定性参数 (含水量,散装密度等). 在不同的深度和区域.
- 建立了土壤裂发展的几何模型和水稳定性的空间分布模型.
- 分析了结构和水稳定性参数之间的同惯性.
主要成果:
- 在拉力沉降区的裂位置显示出水分含量,散装密度,纹理和聚合物的最显著恶化.
- 观察到的峰值下降:水分含量为51.8%,散装密度为12.8%,总销毁率为84.3%.
- 在非裂位置 (协惯性系数0.972) 中,从结构性特性转移到水稳定性特征的损伤传递比在裂位置 (0.933) 中更为显著.
结论:
- 采矿的影响创造了一个从土壤结构到水的稳定性链传输.
- 土壤类型从粘土转变为沙粘土和受影响地区的粘土沙.
- 这些发现为开发矿区土壤保护战略提供了理论基础.
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