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复杂性的起源在软土悬浮体的重质学中
Shravan Pradeep1,2, Paulo E Arratia2, Douglas J Jerolmack3,4
1Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA, 19104, USA.
Nature communications
|August 28, 2024
概括
这项研究揭示了水,沙和粘土的简单混合物如何复制复杂的碎片流动行为. 了解这些土壤悬浮物有助于预测灾难性的土壤流化事件.
科学领域:
- 地质物理学 地质物理学
- 材料科学 是一种材料科学.
- 土壤力学 土壤力学
背景情况:
- 强烈降雨或地震期间土壤液化带来了重大风险.
- 富含沙子的泥表现为颗粒状悬浮物,故障与解堵过渡有关.
- 泥流被模拟为凝,由于粒子间的力量而表现出屈服和剪切稀薄.
研究的目的:
- 使用简单的组件,复制自然垃圾流的复杂流动行为.
- 为了研究从富含沙子的悬浮剂到富含粘土的悬浮剂的产量行为的过渡.
- 为土壤悬浮物提出一个一般的构成关系.
主要方法:
- 使用水,砂和高粘土对碎片流动行为的实验复制.
- 从脆性过渡到柔性过渡的观察,产生不同的沙粘土比率.
- 基于实验数据和无形固体模型的构成关系的开发.
主要成果:
- 使用三元混合物成功复制了自然碎片流动行为的全谱.
- 观察到从脆性 (库伦型) 持续过渡到柔性 (塑料) 产量.
- 提出了土壤悬浮的一般构成关系,将粒子重新排列时间与产生应力和阻塞距离联系起来.
结论:
- 这项研究表明,复杂的土壤悬浮行为可以通过简单的成分来理解.
- 这些发现表明,非平衡相位过渡为预测软土材料行为提供了一个框架.
- 这项研究提供了对灾难性土壤流化控制的基本机制的见解.
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