对含有藻微化石的细粒度土壤的爬行行为进行实验性探索,并洞察微观结构进化
Yue Zhang1, Hongjie Lin2,3, Jianyu Li1,4
1School of Civil Engineering, Sun Yat-sen University, Guangzhou, 510275, Guangdong, China.
Scientific reports
|November 19, 2025
概括
这项研究揭示了二氧化土表现出独特的水力机械和爬行行为,这是由于它们的空洞多孔结构. 这些土壤表现出衰减爬行,随着时间的推移具有稳定的应变,并具有高的巩固系数.
科学领域:
- 地质技术工程 地质技术工程
- 土壤力学 土壤力学
- 材料科学 材料科学 材料科学
背景情况:
- 含有藻微化石的海洋土壤具有不寻常的特性.
- 有限的研究存在于藻土的爬行特征.
- 了解这些土壤中的爬行变形机制至关重要.
研究的目的:
- 为了研究人工二氧化石的水力机械和爬行特性.
- 分析在压力下二氧化的微观结构演变.
- 评估爬行组件模型对二氧化的适用性.
主要方法:
- 使用藻粉,高,蒙莫里隆和伊利特制备人工藻石.
- 进行三轴整合无排水的剪切和爬行测试.
- 利用激光粒子大小分析,扫描电子显微镜和侵入孔径学进行微观结构分析.
主要成果:
- 亚亚土壤表现出高的巩固系数 (1.0 × 10-5 m2 / s) 独立于限制压力.
- 在统一的无排水试验中失败显示出桶式和应变硬化.
- 所有测试的二氧化土壤都显示了衰减爬行,具有稳定的应变率和最终的应变稳定.
- 分数麦克斯韦尔模型证明了用于描述观察到的爬行行为的高适用性.
结论:
- 独特的藻结构,其空洞的毛孔,显著影响水力机械性能,如巩固.
- 藻颗粒之间的摩擦和相互锁定效应有助于未排水的剪切强度与限制压力成正比.
- 观察到的减弱爬行行为归因于藻的结构特征.
- 微观结构完整性在500kPa以下的限制压力下保持.
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