Most fugitive emissions are the result of loss of well integrity through poorly sealed well casings due to geochemically unstable cement.[3] This allows gas to escape through the well itself (known as surface casing vent flow) or via lateral migration along adjacent geological formations (known as gas migration).[3] Approximately 1-3% of methane leakage cases in unconventionaloil and gas wells are caused by imperfect seals and deteriorating cement in wellbores.[3] Some leaks are also the result of leaks in equipment, intentional pressure release practices, or accidental releases during normal transportation, storage, and distribution activities.[4][5][6]
Emissions can be measured using either ground-based or airborne techniques.[3][4][7] In Canada, the oil and gas industry is thought to be the largest source of greenhouse gas and methane emissions,[8] and approximately 40% of Canada's emissions originate from Alberta.[5] Emissions are largely self-reported by companies. The Alberta Energy Regulator keeps a database on wells releasing fugitive gas emissions in Alberta,[9] and the British Columbia Oil and Gas Commission keeps a database of leaky wells in British Columbia. Testing wells at the time of drilling was not required in British Columbia until 2010, and since then 19% of new wells have reported leakage problems. This number may be a low estimate, as suggested by fieldwork completed by the David Suzuki Foundation.[1] Some studies have shown a range of 6-30% of wells suffer gas leakage.[7][9][10][11]
Canada and Alberta have plans for policies to reduce emissions, which may help combat climate change.[12][13] Costs related to reducing emissions are very location-dependent and can vary widely.[14] Methane has a greater global warming impact than carbon dioxide, as its radiative force is 120, 86 and 34 times that of carbon dioxide, when considering a 1, 20 and 100 year time frame (including Climate Carbon Feedback [15][16][9] Additionally, it leads to increases in carbon dioxide concentration through its oxidation by water vapor.[17]
^ abcdCahill, Aaron G.; Steelman, Colby M.; Forde, Olenka; Kuloyo, Olukayode; Ruff, S. Emil; Mayer, Bernhard; Mayer, K. Ulrich; Strous, Marc; Ryan, M. Cathryn (27 March 2017). "Mobility and persistence of methane in groundwater in a controlled-release field experiment". Nature Geoscience. 10 (4): 289–294. Bibcode:2017NatGe..10..289C. doi:10.1038/ngeo2919. hdl:1880/115891. ISSN1752-0908.
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^ abcBachu, Stefan (2017). "Analysis of gas leakage occurrence along wells in Alberta, Canada, from a GHG perspective – Gas migration outside well casing". International Journal of Greenhouse Gas Control. 61: 146–154. doi:10.1016/j.ijggc.2017.04.003.
^Myhre; Shindell; Bréon; Collins; Fuglestvedt; Huang; Koch; Lamarque; Lee; Mendoza; Nakajima; Robock; Stephens; Takemura; Zhang (2013). "Anthropogenic and Natural Radiative Forcing". In Stocker; Qin; Plattner; Tignor; Allen; Boschung; Nauels; Xia; Bex; Midgley (eds.). Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press.