在水力动力学作用下研究碳酸岩的酸性侵蚀特性
Jiaxin Zhang1, Xuewei Chu1, Hai Fu1
1College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, Guizhou, China.
ACS omega
|May 6, 2024
概括
酸性过物加速碳酸盐岩的溶解,影响工程项目. 溶解模式在很大程度上取决于岩石组成,酸度和流速,形成复杂的通道.
科学领域:
- 地质化学 地质化学
- 工程地质工程地质学
- 材料科学 材料科学 材料科学
背景情况:
- 碳酸盐岩石通过酸性过物的溶解对工程结构构成了挑战.
- 在酸性环境中加速溶解的确切机制尚不清楚.
研究的目的:
- 在酸性条件下研究碳酸盐岩的溶解模式.
- 分析各种因素对溶解过程的影响.
主要方法:
- 实验室溶解实验使用自制旋转反应装置在碳酸盐芯上进行.
- 监测质量损失,pH值变化,Ca2+和Mg2+度以及形态变化.
- 相关性分析以确定溶解特征和实验参数之间的关系.
主要成果:
- 溶解与溶解时间,岩石组成 (CaO/MgO比率),液体流速和酸度有显著的关系.
- CaO/MgO比率影响化学溶解速率,并观察到细分特征.
- 液体流速与溶解速率呈正相关,影响多洛米特比石灰岩更大.
- 在五种碳酸盐构成中确定了不同的质量损失率,表明了不同的溶解行为.
结论:
- 碳酸盐岩中的酸性流体诱导的溶解导致复杂的通道形成.
- 了解这些溶解模式对于减轻碳酸盐地形中的工程风险至关重要.
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