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Coal reservoir saturation:Impact of temperature and pressure

June 14, 2008 By: admin Category: Earth and Space Science, Physical Sciences and Engineering

Methane adsorption isotherms measured for a series of coals with varying rank at a wide range of temperatures and pressures allows the prediction of the change in sorption capacity as a function of tectonic history. Changes in sorption capacity in response to declining pressure and temperature associated with uplift may increase or decrease the capacity of the coal and, if the coal is initially saturated, result in excess gas or a deficiency of gas (undersaturation). Assuming reasonable geothermal and pressure gradients, our data indicate that the sorption capacity will generally decrease with uplift and associated exhumation, (more…)

Petroleum generation and migration in the Ghadames Basin, north Africa:A two-dimensional basin-modeling study

June 14, 2008 By: admin Category: Earth and Space Science, Physical Sciences and Engineering

The Ghadames Basin contains important oil- and gas-producing reservoirs distributed across Algeria, Tunisia, and Libya. Regional two-dimensional (2-D) modeling, using data from more than 30 wells, has been undertaken to assess the timing and distribution of hydrocarbon generation in the basin. Four potential petroleum systems have been identified: (1) a Middle-Upper Devonian (Frasnian) and Triassic (Triassic Argilo Greseux Inferieur [TAG-I]) system in the central-western basin; (2) a Lower Silurian (more…)

A new technology for the characterization of microfractured reservoirs

June 14, 2008 By: admin Category: Earth and Space Science, Physical Sciences and Engineering

This article presents a test case of a new technology using artificially enhanced anisotropy of magnetic susceptibility (referred to here as EAMS) for the characterization of microfractured reservoirs. These are reservoirs in which microfractures are essential to porosity and/or permeability. A conventional geological characterization is costly, time consuming, and difficult to quantify in terms of assessing fracture impact on porosity and permeability. (more…)

Electronic Submission Guidelines For AAPG Bulletin

June 14, 2008 By: admin Category: Earth and Space Science, Physical Sciences and Engineering

Authors are asked to submit new manuscripts online through Rapid Review (www.rapidreview.com), where they can track their manuscripts from submission through acceptance. Preparing computer files in one of the preferred computer applications increases the likelihood that graphics will be rendered correctly. (more…)

Impacts of volumetric strain on CO2 sequestration in coals and enhanced CH4 recovery

June 14, 2008 By: admin Category: Earth and Space Science, Physical Sciences and Engineering

Sequestration of CO2 into deep, unminable coal seams is an attractive option to reduce atmospheric emissions. However, coal seams commonly have low initial permeability, and CO2 adsorption causes the coal matrix to swell, which further reduces the permeability and may result in inefficient injection. We investigate numerically the impacts of coal swelling on coal permeability and, thus, CO2 injection efficiency with constraints determined by experimental adsorption-associated volumetric strain measurements on three western Canadian coals. Our results show that injecting pure CO2 markedly reduces permeability through time to the extent that it is not a feasible sequestration technology for almost all coals. (more…)

Regional overview of deep sedimentary thermal gradients of the geopressured zone of the Texas-Louisiana continental shelf

June 14, 2008 By: admin Category: Earth and Space Science, Physical Sciences and Engineering

Nearly 600 bottom-hole temperature data from the northern continental shelf of the Gulf of Mexico, each corrected for drilling disturbance, yielded a regional map of geothermal gradient down to approximately 6 km (3.7 mi) sub-sea floor. Two geographic trends can be seen on the map. First, from east to west, the geothermal gradient changes from values between 0.025 and 0.03 K/m (0.014 and 0.016 degreeF/ft) off the Alabama-Mississippi shore to lower values of 0.015-0.025 K/m (0.008-0.014 degreeF/ft) off eastern Louisiana and to higher values of 0.03-0.06 K/m (0.016-0.033degreeF/ft) off western Louisiana through Texas. Second, thermal gradients tend to be lower toward the outer continental shelf (less than 0.02 K/m [0.0112 degree F/ft]). We believe that the observed variations are primarily attributable to the thermal effect of rapid and regionally variable sediment accumulation during the Cenozoic era, which resulted in the occurrence of the geopressured zone in the Texas -Louisiana shelf. (more…)