@misc{fb6b2757a7f94fb283a61f4baabca3da,
title = "Influence of Reservoir Heterogeneity on Geothermal Fluid and Methane Recovery from a Geopressured Geothermal Reservoir (Presentation): NREL (National Renewable Energy Laboratory)",
abstract = "Geopressured geothermal reservoirs are characterized by high temperatures and high pressures with correspondingly large quantities of dissolved methane. Two methods utilizing reservoir simulation techniques have been used to estimate recoverability factors of geothermal brine and methane based on well log data from a specific reservoir in Texas. The first assumes a simplified reservoir that hasthree layers: upper shale, sandstone, and lower shale with the sandstone layer thickness equal to the net sandstone in the reservoir interval. The second method uses a detailed reservoir model that accounts for multiple sandstone and shale layering. This method includes 12 layers of sandstone or shale with the layer depths determined from a well log. These two methods are used to answer thequestion on the sensitivity of the results to the level of detail that is included in the reservoir model. It was found that incorporating multiple thin layers of lower permeability sandstone can noticeably impact the results of the reservoir simulation. The heterogeneous model resulted in greater flow rates of both geothermal brine and total methane. Both models demonstrate that thegeopressured geothermal reservoir is capable of producing hot geothermal fluid at flow rates over a long duration that are sufficient for electricity production from binary power plants. The results indicate that simplified models of geopressured geothermal reservoirs that approximate actual reservoir details can be applied to give a reasonable, albeit conservative, estimate of the recoverableresource over broad areas using generalized data sets.",
keywords = "geopressured geothermal reservoirs, geothermal, geothermal models",
author = "Chad Augustine and Ariel Esposito",
year = "2012",
language = "American English",
series = "Presented at the Stanford Geothermal Workshop, 31 January - 1 February 2012, Stanford, California",
type = "Other",
}