关于孔隙结构的实验研究 砂岩在盐水下的演化 侵蚀
1School of Resources and Safety Engineering, Central South University, Changsha 410083, China.
Materials (Basel, Switzerland)
|August 14, 2025
概括
盐水侵蚀显著改变了红色砂岩的微观结构,减少了水的吸收,改变了孔隙结构. 这影响了沿海地区地下结构的稳定性.
科学领域:
- 地质技术工程 地质技术工程
- 材料科学 材料科学 材料科学
- 环境科学 环境科学
背景情况:
- 中国沿海地区的地下水化影响了地下结构.
- 岩石微观结构因盐水侵蚀而改变,影响机械性能.
研究的目的:
- 为了研究红色砂岩在盐水侵蚀下孔的演变.
- 分析盐水对砂岩微观结构和多孔性的影响.
主要方法:
- 核磁共振 (NMR) 技术用于毛孔进化.
- 用于矿物成分分析的X射线衍射 (XRD).
主要成果:
- 砂岩在盐水中表现出最低的吸水率.
- 盐水侵蚀导致红色砂岩毛孔发生显著变化,改变了迷你和中等毛孔.
- 盐水成分和浸泡时间影响砂岩的多孔性.
结论:
- 盐水侵蚀从根本上改变了红色砂岩的微观结构和多孔性.
- 了解这些变化对于盐的沿海地区地下结构稳定性至关重要.
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