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陆上非常规气靶区断层封闭性分析——以北珀斯盆地为例。

Fault Seal Analysis in an Onshore Unconventional Gas Target, North Perth Basin.

机构信息

The University of Auckland, Private Bag 92019 Auckland Mail Centre, Auckland, 1142, New Zealand.

Badleys Geoscience North Beck House/North Beck Lane, Spilsby, E23 5NB, United Kingdom.

出版信息

Ground Water. 2021 Jan;59(1):131-145. doi: 10.1111/gwat.13026. Epub 2020 Jul 23.

Abstract

During the 1980s, hydrocarbons were logged in aquifers during drilling of conventional gas wells in the Woodada gasfield. The gasfield is located in the North Perth Basin in Western Australia. Using Fault Seal Analysis Technology, our goal was to test the hypothesis that faults in the Kockatea Shale that are currently being reactivated may be leak prone. Wells proximal to faults with a fracture stability of greater than 5 MPa logged only methane. Wells proximal to faults with a fracture stability ≤5 MPa logged both methane and condensate in aquifers confirming that hydrocarbon leakage is correlated with critically stressed faults. This assessment assumes that fault rocks in the Kockatea Shale, which is a regional source rock and seal, comprise uncemented phyllosilicate rock. For the normal stress case, faults oriented west-north-west with moderate dip have the lowest integrity. For the strike slip stress case, faults oriented north-west and west-south-west, with moderate to steep dip have the lowest integrity. If the Kockatea Shale fault rock is assumed to be a cemented phyllosilicate, then the fracture stability increases to 14 MPa for both the normal and strike slip case. In this case, Jurassic-Permian fault intersections may be contributing to hydrocarbon leakage, however, this would require numerical modeling for confirmation. Based on leak off tests, the increase in pressure required to hydraulically fracture the formation varies between 10.7 and 13.8 MPa. The treatment pressures used during hydraulic fracturing may potentially exacerbate leakage in areas such as the Woodada gasfield.

摘要

在 20 世纪 80 年代,在西澳大利亚州北珀斯盆地的伍德达气田钻探常规天然气井时,烃类物质被记录在含水层中。利用断层密封分析技术,我们的目标是验证这样一个假设,即在目前正在重新活动的科卡泰莎页岩中的断层可能容易发生泄漏。裂缝稳定性大于 5MPa 的近断层井仅记录甲烷。裂缝稳定性小于或等于 5MPa 的近断层井在含水层中记录了甲烷和凝析油,证实了烃类泄漏与临界应力断层有关。该评估假设,作为区域源岩和封盖的科卡泰莎页岩中的断层岩由未胶结的层状硅酸盐岩组成。对于正常应力情况,具有中等倾角的向西-北西向定向的断层具有最低的完整性。对于走滑应力情况,具有中等至陡峭倾角的西北向和西南-西向的断层具有最低的完整性。如果假设科卡泰莎页岩断层岩是胶结的层状硅酸盐,则正常和走滑情况下的断裂稳定性分别增加到 14MPa。在这种情况下,侏罗纪-二叠纪断层交点可能导致烃类泄漏,但这需要数值模拟来确认。基于泄漏测试,水力压裂地层所需的压力增加在 10.7 和 13.8MPa 之间。在水力压裂过程中使用的处理压力可能会加剧伍德达气田等地区的泄漏。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c1d9/7891673/8de6c2d3feb4/GWAT-59-131-g001.jpg

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