一个有效的介质模型,用于评估有机丰富的泥岩中的可湿性
Isa Silveira de Araujo1, Zoya Heidari1
1Hildebrand Department of Petroleum and Geosystems Engineering, The University of Texas at Austin, 200 E. Dean Keeton St., Stop C0300, Austin, Texas 78712-1585, United States1.
Langmuir : the ACS journal of surfaces and colloids
|December 9, 2025
概括
一种新方法使用吸附水和建模来评估有机丰富的泥岩 (ORM) 的可湿性. 这种方法可以准确地预测岩石的湿度,而无需进行广泛的实验室测试,从而改善了水库评估.
科学领域:
- 地质化学 地质化学
- 石油地质学 石油地质学
- 材料科学 材料科学 材料科学
背景情况:
- 有机丰富的泥岩 (ORM) 的浸透性对于碳化合物生产至关重要.
- 传统的方法与ORM复杂的组成和孔状结构作斗争.
研究的目的:
- 开发一种新的工作流程,用于分析估计ORM湿度评估的水吸附异热体.
- 为了克服复杂岩层中的传统湿度评估的局限性.
主要方法:
- 结合用前向模型和反转算法进行水吸附测量.
- 通过岩石组成和实验数据,推导出特定组件的吸附特性.
- 对ORM样本的分析估计的水吸附同热量.
主要成果:
- 拟议的方法准确地估计了水吸附等温度,与实验数据相比,平均相对差异低于14%.
- 已确定的吸附参数使得新的样品可靠地评估了可湿性,而不需要进一步的实验.
- 通过钻井地质物理测量,证明了实时湿度评估的潜力.
结论:
- 新的工作流提供了一种可靠的方法来评估复杂成分岩石的可湿性.
- 这种技术增强了水库特征和碳化合物产量评估.
- 未来的应用可能包括任何深度的实时形成湿度评估.
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