在多洛米特石灰岩中的迁移机制
Xinyu Zhang1, Wei Li1, Xiaojun Huang1
1College of Materials Science and Engineering, Nanjing Tech University, Nanjing 211816, China.
Materials (Basel, Switzerland)
|September 27, 2025
概括
-多洛米特反应 (ADR) 涉及离子通过混凝土孔迁移. 这种迁移驱动了脱化,这是混凝土裂和恶化的关键过程.
科学领域:
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
- 土木工程 土木工程是指土木工程.
背景情况:
- -多洛米特反应 (ADR) 通过脱多洛米化导致混凝土的恶化.
- 关于ADR机制和产品的现有研究是广泛的,但对反应进展和控制因素的理解是有限的.
研究的目的:
- 为了研究在多洛米特石灰岩中的离子迁移.
- 了解离子和多洛米特晶体之间的反应过程.
主要方法:
- 在多洛米特石灰岩样本上进行实验.
- 对 (Na+) 离子迁移的量化.
- 使用X射线衍射 (XRD) 测量去化度.
- 通过场辐射扫描电子显微镜 (FESEM) 进行微结构评估.
主要成果:
- 孔隙网络作为离子迁移的物理途径.
- 度梯度是离子迁移的主要驱动因素.
- 离子相互作用影响迁移的效率.
结论:
- 获得了除化洞察力,突出了孔隙结构和离子迁移动态的作用.
- 了解离子迁移对于预测和减轻混凝土结构中的ADR至关重要.
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