对模拟合物-盐水-矿物系统中的水化学相互作用的洞察力
Hamed M Kermani1, María Bonto1, Hamidreza M Nick1
1Danish Offshore Technology Centre (DTU Offshore), Technical University of Denmark, Kgs, Lyngby 2800, Denmark.
Journal of contaminant hydrology
|August 12, 2025
概括
与碳酸盐岩的结合体相互作用受盐度,pH值和温度的影响. 高盐度促进合物沉积,而较低的盐度和较高的pH/温度减少了它,影响了地下水管理.
科学领域:
- 地质化学和环境科学
- 石油工程是石油工程中的一个.
- 合体和表面科学科学
背景情况:
- 了解合物 - 盐水 - 岩石相互作用对于地下流体流动至关重要,特别是在碳酸盐水库中.
- 生产的水再注入和水泛滥场景是管理合体运输的关键应用.
- 由于合体沉积而造成的形成损伤可以显著影响水库的生产力.
研究的目的:
- 为了研究有机-无机合物在多孔碳酸盐介质中的保留潜力.
- 评估物理化学和水力动力学条件对合体沉积的影响.
- 开发一个整合表面复杂化,DLVO理论和流体水力学模型.
主要方法:
- 利用表面复杂化模型来捕捉静电力变化.
- 应用了扩展的DLVO理论来分析合体-表面相互作用.
- 纳入流体液态动力学来建模合体流动力学.
- 模拟场景使用产生的水 (高盐度) 和稀释的产生的水 (低盐度).
主要成果:
- 在研究pH值和温度的高盐度条件下,体沉积更受欢迎.
- 在低盐度的水中,增加的pH值和温度减少了合物附着.
- 在典型的地下流速下,化学因素主导着合物岩石相互作用,而高速率则强调水力动力学.
结论:
- 碳酸盐储中的合体保留对液体的盐度,pH值和温度高度敏感.
- 水力动力学只有在非常高的液体注入速度时才变得重要.
- 该研究为减轻形成损害和优化水淹水操作提供了关键的见解.
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