水力性能变化与深度在泥泥石滑坡的滑坡
Wei Liu1, Gaochao Lin2, Qingpeng Liu1
1Institute of Transportation, Inner Mongolia University, Hohhot, 010070, Inner Mongolia, China.
Scientific reports
|May 14, 2024
概括
调查岩-泥石滑坡揭示了岩和泥石的独特土壤水特性曲线 (SWCC). 滑坡中的SWCC显示了由土壤类型和泥石含量影响的模式,这对于了解滑坡触发因素至关重要.
科学领域:
- 地质技术工程 地质技术工程
- 地球科学 地球科学 地球科学
- 土壤力学 土壤力学
背景情况:
- 滑坡,特别是石泥石滑坡,在石分布的地区是显著的地质危险.
- 湿度是引发这些滑坡的关键因素,影响土壤的稳定性和安全性.
研究的目的:
- 为了研究活跃的岩泥石滑坡中的土壤的液压特性.
- 分析土壤水特性曲线 (SWCC) 和它们与滑坡动态的关系.
主要方法:
- 土壤水特性曲线 (SWCC) 用van Genuchten模型确定和拟合.
- 实验分析包括X射线衍射 (XRD),扫描电子显微镜 (SEM),粒子大小分布 (PSD) 和地质技术测试.
- 研究了,泥石及其混合物的液压性能.
主要成果:
- 对于和泥石,观察到明显的SWCC分布.
- 由于山体滑坡活动,Loess SWCC在不同深度显示了类似的模式.
- 石-泥石混合物表现出过渡性SWCC,与较高的泥石含量相关的水留量增加.
结论:
- 这项研究提供了关于岩泥石滑坡内土壤的液压行为的见解.
- 这些发现与地质观测相一致,提高了对山体滑坡机制的理解.
- 结果对于预测和减轻河流地区的山体滑坡风险非常有价值.
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