道化是复杂的多孔介质中一种独特的溶解类
Hannah P Menke1, Julien Maes2, Sebastian Geiger3
1Institute of GeoEnergy Engineering, Heriot-Watt University, Edinburgh, UK. h.menke@hw.ac.uk.
Scientific reports
|July 14, 2023
概括
在多孔介质中发现了一种新的道溶解制度,改变了传统的模型. 这一发现对于预测地热能和碳储存等应用中的溶解至关重要.
科学领域:
- 地质化学 地质化学
- 地质地质地质地质地质地
- 的媒体科学 的媒体科学
背景情况:
- 传统上,在多孔介质中的固体溶解遵循统一,紧或虫洞的模式.
- 这些机制取决于反应速率,流量和扩散之间的平衡.
- 现有的模型可能无法完全捕捉复杂的溶解模式.
研究的目的:
- 用数值模拟来研究在酸注射过程中孔隙结构的演变.
- 确定已知的溶解制度之间的界限.
- 为了描述一个潜在的新解体制度:道化.
主要方法:
- 在两个越来越复杂的模型中进行酸注射的数值模拟.
- 孔隙结构演变和溶解模式的分析.
- 研究流通路径及其对溶解的影响.
主要成果:
- 确定了第四种解散制度,称为道化.
- 当流通道由于毛孔喉大小分布而表现出数量级的流速差异时,就会发生道化.
- 这种模式导致透度变化显著,透度变化最小,创建一个独特的透度-透度关系.
结论:
- 在多孔介质中固体溶解的传统模型需要更新,以包括道化制度.
- 在地热能生产和地质碳储存等应用中精确预测溶解需要将这种新制度纳入.
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