Hydraulic fracturing in unconventional gas reservoirs: risks in the geological system, part 2

被引:106
|
作者
Kissinger, Alexander [1 ]
Helmig, Rainer [1 ]
Ebigbo, Anozie [2 ]
Class, Holger [1 ]
Lange, Torsten [3 ]
Sauter, Martin [3 ]
Heitfeld, Michael [4 ]
Kluenker, Johannes [4 ]
Jahnke, Wiebke [3 ]
机构
[1] Univ Stuttgart, Inst Modelling Hydraul & Environm Syst, Dept Hydromech & Modelling Hydrosyst, D-70569 Stuttgart, Germany
[2] Rhein Westfal TH Aachen, EON Energy Res Ctr EON ERC, D-52074 Aachen, Germany
[3] Univ Gottingen, Geosci Ctr Gottingen, Dept Appl Geol, D-37077 Gottingen, Germany
[4] Ingenieurburo Heitfeld Schetelig GmbH, D-52074 Aachen, Germany
关键词
Fracturing fluids; Methane; Modelling; EQUATION-OF-STATE; CH4-CO2-H2O SYSTEM; 1000-DEGREES-C; SCALE; FLOW;
D O I
10.1007/s12665-013-2578-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Hydraulic fracturing is a method used for the production of unconventional gas resources. Huge amounts of so-called fracturing fluid (10,000-20,000 m(3)) are injected into a gas reservoir to create fractures in solid rock formations, upon which mobilised methane fills the pore space and the fracturing fluid is withdrawn. Hydraulic fracturing may pose a threat to groundwater resources if fracturing fluid or brine can migrate through fault zones into shallow aquifers. Diffuse methane emissions from the gas reservoir may not only contaminate shallow groundwater aquifers, but also escape into the atmosphere where methane acts as a greenhouse gas. The working group "Risks in the Geological System" as part of ExxonMobil's hydrofracking dialogue and information dissemination processes was tasked with the assessment of possible hazards posed by migrating fluids as a result of hydraulic fracturing activities. In this work, several flow paths for fracturing fluid, brine and methane are identified and scenarios are set up to qualitatively estimate under what circumstances these fluids would leak into shallower layers. The parametrisation for potential hydraulic fracturing sites in North Rhine-Westphalia and Lower Saxony (both in Germany) is derived from literature using upper and lower bounds of hydraulic parameters. The results show that a significant fluid migration is only possible if a combination of several conservative assumptions is met by a scenario.
引用
收藏
页码:3855 / 3873
页数:19
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