SPE Journal
Volume 17,
Number 1,
March 2012,
pp. 230-242
Summary
Shales and some tight-gas reservoirs have complex, multimodal pore-size
distributions, including pore sizes in the nanopore range, causing gas to be
transported by multiple flow mechanisms through the pore structure. Ertekin et
al. (1986) developed a method to account for dual-mechanism (pressure- and
concentration-driven) flow for tight formations that incorporated an apparent
Klinkenberg gas-slippage factor that is not a constant, which is commonly
assumed for tight gas reservoirs. In this work, we extend the dynamic-slippage
concept to shale-gas reservoirs, for which it is postulated that multimechanism
flow can occur. Inspired by recent studies that have demonstrated the complex
pore structure of shale-gas reservoirs, which may include nanoporosity in
kerogen, we first develop a numerical model that accounts for multimechanism
flow in the inorganic- and organic-matter framework using the dynamic-slippage
concept. In this formulation, unsteady-state desorption of gas from the kerogen
is accounted for. We then generate a series of production forecasts using the
numerical model to demonstrate the consequences of not rigorously accounting
for multimechanism flow in tight formations. Finally, we modify modern
rate-transient methods by altering pseudovariables to include dynamic-slippage
and desorption effects and demonstrate the utility of this approach with
simulated and field cases. The primary contribution of this work is therefore
the demonstration of the use of modern rate-transient methods for reservoirs
exhibiting multimechanism (non-Darcy) flow. The approach is considered to be
useful for analysis of production data from shale-gas and tight-gas formations
because it captures the physics of flow in such formations realistically.
© 2012. Society of Petroleum Engineers
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History
- Original manuscript received:
14 March 2011
- Meeting paper published:
12 June 2011
- Revised manuscript received:
28 June 2011
- Manuscript approved:
7 July 2011
- Published online:
8 February 2012
- Version of record:
13 March 2012