关于由页岩水化形成的二次断层扩张机制的实验研究 在断层开发中
Kai Liu1,2,3, Wenli Ding1, Mingguo Peng1,2,3
1School of Petroleum Engineering, Changzhou University, Changzhou, Jiangsu 213164, PR China.
ACS omega
|April 21, 2025
概括
这项研究揭示了裂纹液体,如滑水和瓜尔如何影响页岩水库. 滑水导致早期扩张,而瓜尔导致更大的长期断裂孔隙,以有效地开发页岩油气.
科学领域:
- 石油工程是石油工程中的一个.
- 地质力学 地质力学
- 材料科学 材料科学 材料科学
背景情况:
- 页岩水库需要水力压裂来实现经济可行性.
- 裂变液诱导了页岩中的水化和二次裂变扩张.
- 关于页岩中不同裂变流体的具体水化特征的研究有限.
研究的目的:
- 为了澄清不同裂变流体的页岩水库的水分特性.
- 为了阐明由于页岩水化而导致的二次裂变扩张的机制.
- 量化描述受裂流体影响的断裂参数.
主要方法:
- 最初和长期的孔隙压力实验.
- 微观实验包括声波发射,在线核磁共振 (NMR) 和CT扫描.
- 液化特征和二次断裂扩张的分析.
主要成果:
- 早期水合:滑水显示出更大的膨胀和多孔性 (0.0882%) 与孔隙压力下降到4 MPa.
- 早期水化:瓜尔的扩张和孔隙性较小 (0.0515%),孔隙压力降至2MPa.
- 长期补水:与滑水相比,瓜尔导致骨折孔径显著增加 (280.6%) 和最终孔径更高 (0.196%).
结论:
- 滑水的早期有效性是由于表面活性剂和粘土膨胀,但分布有限.
- 瓜尔的延迟但更广泛的分布导致更大的晚期二次骨折扩张.
- 这些发现为优化页岩油气开采提供了关键的物理参数和理论见解.
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