在干旱地带开采的洛斯高原,多层次的土壤湿度动态源于裂演变和微观结构崩
Ting Ma1,2, Fuquan Tang3, Furong Zhang4
1Shaanxi Railway Institute, Weinan, 710054, China. 184740779@qq.com.
Scientific reports
|December 24, 2025
概括
煤矿的裂破坏了干旱地区的土壤水分. 裂的大小和演变影响水损失,影响土壤结构和保留,这对生态恢复至关重要.
科学领域:
- 土壤科学 土壤科学
- 环境科学 环境科学
- 地质地质地质地质地质地
背景情况:
- 煤炭开采导致沉降和裂,改变干旱环境中的土壤水分动态.
- 对于洛斯高原来说,了解采矿引起的土壤水分裂的多层次机制至关重要.
研究的目的:
- 调查采矿引起的裂如何影响土壤水分在不同尺度上的再分配.
- 分析裂的演变特征及其对土壤微观结构和液压性能的影响.
主要方法:
- 综合现场监测,土壤实验,物理模拟和数值建模 (Hydrus-2D双域模型).
- 动态裂监测,扫描电子显微镜 (SEM) 和土壤水特性曲线分析.
- 对裂纹尺度 (微,小,中,大) 和它们的稳定期进行比较分析.
主要成果:
- 裂演变因规模而异:微/小裂缓慢稳定 (20天),中/大裂迅速 (8-10天).
- 裂的宽度和近距离确定了土壤水分损失率.
- 裂改变了的微观结构,增加了孔隙性和连接性,加速了蒸发/透,降低了水的保留能力,微裂的影响最大.
结论:
- 采矿诱导的裂通过裂演变和微观结构崩协同影响土壤的液压特性.
- 调查结果为采矿受影响的洛斯地区的生态恢复战略提供了关键的见解.
- 在裂附近的优选流动模式得到了有效的建模,并通过现场数据进行了验证.
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