在石灰岩泥岩中注射酸盐盐水时,骨折表面的演变
Hasan Javed Khan1, Ridha Al-Abdrabalnabi1, Murtada Saleh Al-Jawad1
1Department of Petroleum Engineering, King Fahd University of Petroleum and Minerals, Dhahran, Eastern Province, Saudi Arabia 34464.
ACS omega
|June 5, 2023
概括
酸盐注射改变了富含石的页岩裂,通过矿物溶解增加了孔径. 这一过程产生了细,降低了压力压力下的断裂导电性.
科学领域:
- 地质地质地质地质地质地
- 石油工程是石油工程中的一个.
- 材料科学 材料科学 材料科学
背景情况:
- 液压压裂流体改变岩石断裂表面,创造了反应改变的区域.
- 物理化学变化主要发生在页岩表面,反应透深度有限.
研究的目的:
- 在注射酸盐水中调查富含酸盐的骨折表面的物理化学演变.
- 分析压力压力下的断裂孔径增长和表面性能变化.
主要方法:
- 在富含酸盐的沃尔夫坎普页岩裂中注入酸盐水.
- 高分辨率计算机断层扫描用于光圈测量.
- 表面粗度分析,X射线光和质谱检测物理化学变化.
主要成果:
- 断裂孔径增加了大约8.3微米.
- 骨折地形在注射后变得更加光滑.
- 通过表面剥离和废水分析证实了石溶解.
结论:
- 矿物溶解是骨折孔径增长的主要机制.
- 表面减弱和压力应力促进了细菌的产生,减少了断裂导电性.
- 岩石矿物学显著影响断裂进化机制.
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