碳酸盐酸化:对低流速下虫洞传播的新见解
Jair R Neyra1,2, Daniel N N da Silva1, Cláudio R S Lucas1
1Petroleum Science and Engineering Laboratory (LCPETRO), Federal University of Pará (UFPA), Salinópolis, Pará 68721-000, Brazil.
ACS omega
|November 24, 2025
概括
在低流速下碳酸盐岩中形成虫洞的理解很少. 这项研究表明,传统模型高估了突破时间,虫洞的增长在特定的极限稳定,而不是无限增加.
科学领域:
- 地质化学 地质化学
- 石油工程是石油工程中的一个.
- 地质二氧化碳储存地质二氧化碳储存
背景情况:
- 虫洞是由碳酸岩的酸性溶解形成的,对于石油工程和二氧化碳储存中的流体流动至关重要.
- 低流速时的虫洞形成尚未得到充分探索,尽管它在现场作业中发生.
- 现有的模型不准确地预测了缩酸的低流速虫洞行为.
研究的目的:
- 在低流速下研究虫洞的形成和形态.
- 在这些条件下确定孔积到突破 (PVBt).
- 解决目前模型在预测虫洞行为方面的局限性.
主要方法:
- 在低流速下进行了酸化实验.
- 由于最小的压力下降,采用了部分酸化.
- 利用微型CT成像分析虫洞形态并估计PVBt.
主要成果:
- 传统模型高估了PVBt在低流速;突破比预测更早发生.
- 在较低的流速下观察到PVBt稳定趋势.
- 这种稳定发生在经经经测量推导的极限时,与无限增长预测相矛盾.
结论:
- 目前的模型需要修订,以准确预测低流速的虫洞突破.
- 这些发现提高了对碳酸盐系统中反应性流动力学的理解.
- 这项研究为优化酸化处理和二氧化碳储存提供了关键数据.
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