Capillary Wicking in Gas Wells

TitleCapillary Wicking in Gas Wells
Publication TypeConference Paper
Year of Publication2006
AuthorsMahadevan, J., M. M. Sharma, and Y. C. Yortsos
Conference NameSPE Annual Technical Conference and Exhibition
Date Published09/2006
PublisherSociety of Petroleum Engineers
Conference LocationSan Antonio, Texas, U.S.A., September 24-27, 2006
ISBN Number978-1-55563-149-9
Other NumbersSPE 103229-MS
KeywordsFormation Damage, Fracture modeling, Shale-fluid interactions, Water Blocking in Low Permeability Gas Sands
Abstract

Gas expansion near the wellbore during production causes the evaporation of connate water. When the reservoir permeability is low, capillarity is controlling, causing liquid movement to the near-wellbore region where drying rates are higher. In tight gas sands or in shale gas formations, where capillarity is high, the gas production itself can cause depletion of the water saturation below residual values, due to such evaporation.

In this work we present a study of the fundamental processes involved during the flow of a gas in a liquid- saturated porous medium. We have modeled evaporation by accounting for the capillary driven film flow or ‘wicking' of saline liquid to the wellbore or the near-fracture region and the effect of gas expansion. It is shown that, for gas reservoirs with connate water saturation, large pressure drawdowns lead to a drying front that develops at the formation face and propagates into the reservoir. When pressure drops are lower, water rapidly redistributes due to capillarity-induced movement of liquid from high-to low-saturation regions. This phase redistribution causes higher drying rates near the wellbore.

The results show, for the first time, the effect of both capillarity- induced film flow and gas compressibility on the rate of drying in gas wells. The model can be used to help maximize gas production under conditions such as waterblocking by optimizing the operating conditions. Additionally it can be used to obtain a better understanding of the impact of capillarity on evaporation and consequent processes, such as salt precipitation.

DOI10.2118/103229-MS