Estimating the upper limit of gas production from Class 2 hydrate accumulations in the permafrost: 2. Alternative well designs and sensitivity analysis

• Published in: Journal of Petroleum Science and Engineering
• Main Authors: Moridis, G., Reagan, M.T.
• Language: unknown
• Published: 2011
• Subjects: 54; 58; CONFIGURATION; DESIGN; FLUID WITHDRAWAL; HEATING; HYDRATES; PERFORMANCE; PERMAFROST; PERMEABILITY; PRODUCTION; SATURATION; SENSITIVITY ANALYSIS; WATER; permafrost
• Online Access: http://www.osti.gov/servlets/purl/1007197; https://www.osti.gov/biblio/1007197; https://doi.org/10.1016/j.petrol.2010.12.001

In the second paper of this series, we evaluate two additional well designs for production from permafrost-associated (PA) hydrate deposits. Both designs are within the capabilities of conventional technology. We determine that large volumes of gas can be produced at high rates (several MMSCFD) for long times using either well design. The production approach involves initial fluid withdrawal from the water zone underneath the hydrate-bearing layer (HBL). The production process follows a cyclical pattern, with each cycle composed of two stages: a long stage (months to years) of increasing gas production and decreasing water production, and a short stage (days to weeks) that involves destruction of the secondary hydrate (mainly through warm water injection) that evolves during the first stage, and is followed by a reduction in the fluid withdrawal rate. A well configuration with completion throughout the HBL leads to high production rates, but also the creation of a secondary hydrate barrier around the well that needs to be destroyed regularly by water injection. However, a configuration that initially involves heating of the outer surface of the wellbore and later continuous injection of warm water at low rates (Case C) appears to deliver optimum performance over the period it takes for the exhaustion of the hydrate deposit. Using Case C as the standard, we determine that gas production from PA hydrate deposits increases with the fluid withdrawal rate, the initial hydrate saturation and temperature, and with the formation permeability.