基于J函数和碎形理论的透性计算方法研究
Guangteng Lu1,2, Fengpeng Lai1,2, Bince Li1,2
1School of Energy Resources, China University of Geosciences, Beijing, China.
Ground water
|July 1, 2023
概括
使用碎形理论的新方法计算了砂岩水库的透度,克服了低透度构成的实验挑战. 这种方法为地质研究提供了准确可靠的透率估计.
科学领域:
- 地质地质地质地质地质地
- 水文地质学 水文地质学
- 地质物理学 地质物理学
背景情况:
- 透性对于含水层的表征至关重要.
- 对于具有低透性的砂岩含水层来说,直接测量透性是具有挑战性的.
- 现有的方法在特定的地质环境中可能缺乏准确性.
研究的目的:
- 开发和验证一种用于计算砂岩含水层透性的新方法.
- 为了利用碎形理论和J函数来改进透率估计.
- 分析地质参数对计算透性的影响.
主要方法:
- 根据分数理论和J函数推导出一种新的透性计算方法.
- 在变化的水和下解决J函数.
- 拟合J函数和水和度曲线,使用注入数据来确定碎形尺寸和扭曲度.
- 使用来自Ordos盆地Chang 7群的岩石样本计算和验证透性.
主要成果:
- 拟议的方法准确计算了砂岩含水层的透性.
- 对15个岩石样本的验证显示,大多数样本的相对误差不到20%.
- 分析揭示了碎形尺寸,扭曲度和多孔度对透性的显著影响.
结论:
- 新的基于碎形的方法提供了一个准确和可靠的方法来确定砂岩含水层的透性,特别是在低透性的情况下.
- 该方法有效地整合了注射数据和碎形参数.
- 这项研究增强了对水表水力特性孔隙结构控制的理解.
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