Abstract
Human underground activity related to oil & gas production can result in unintended connections between shallow
groundwater and deep reservoirs, causing upward gas leakage. This may impair groundwater quality, contribute
to anthropogenic greenhouse gas emissions, and can cause explosion hazard. Typically, leakage is detected by
measuring methane emissions at the soil surface, or methane concentrations in shallow groundwater. The extent to
which such leaks may result in elevated methane concentrations in groundwater and methane emissions at surface
level is expected to depend on a range of factors. Besides the gas leakage rate, it is also affected by the degree of
dissolution of the gas and dispersion in intermediate aquifers during its upward migration. Such losses may be
particularly large in thick unconsolidated sedimentary systems, under the influence of lateral groundwater flow.
To investigate how these various factors affect subsurface methane gas leaks, a 3D numerical model was
constructed using DuMux, to simulate two-phase (liquid & gas) and two-component (H2O & CH4) behaviour for
variations of typical sedimentary aquifer conditions. Then, a sensitivity analysis was carried out to determine the
most influential parameters by varying porous medium properties, two-phase flow parameters, regional groundwater flow velocities and leakage flux. The results show that for typically observed leakage fluxes significant
proportions of gas may be dissolved and/or dispersed laterally during upward migration, making it effectively
undetectable at surface level or only after long time periods (decades to centuries). Under such conditions,
measurements at surface are inadequate for determining subsurface gas leakage rates.
Original language | English |
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Article number | EGU2019-12954 |
Journal | Geophysical Research Abstracts |
Volume | 21 |
Publication status | Published - 2019 |
Event | EGU General Assembly 2019 - Vienna, Austria Duration: 7 Apr 2019 → 12 Apr 2019 |