Geopressured-Geothermal Research Program: An Overview Metadata

Title

• Main Title Geopressured-Geothermal Research Program: An Overview

Creator

• Author: Fortuna, Raymond
  Creator Type: Personal
• Author: Jelacic, Allan
  Creator Type: Personal

Contributor

• Sponsor: United States. Office of Fossil Energy.
  Contributor Type: Organization
  Contributor Info: USDOE - Office of Fossil Energy (FE)

Publisher

• Name: United States. Department of Energy.
  Place of Publication: United States
  Additional Info: USDOE

Date

• Creation: 1989-04

Language

• English

Description

• Content Description: The geopressured-geothermal resource consists of deeply buried reservoirs of hot brine, under abnormally high pressures, that contain dissolved methane. Geopressured brine reservoirs with pressures approaching the lithostatic load are known to occur both onshore and offshore beneath the Gulf of Mexico coast, along the Pacific west coast, in Appalachia, as well as in deep sedimentary basins elsewhere in the United States. The Department of Energy (DOE) has concentrated its research on the northern Gulf of Mexico sedimentary basin (Figure 1) which consists largely of Tertiary interbedded sandstones and shales deposited in alternating deltaic, fluvial, and marine environments. Thorsen (1964) and Norwood and Holland (1974) describe three generalized depositional facies in sedimentary beds of the Gulf Coast Geosyncline (Figure 2 ): (1) a massive sandstone facies in which sandstone constitutes 50 percent o r more of the sedimentary volume; (2) an alternating sandstone and shale facies in which sandstone constitutes 15 to 35 percent of the sedimentary volume. (3) a massive shale facies in which sandstone constitutes 15 percent or less of the sedimentary volume. In general, at any given location the volume of sandstone decreases with increasing depth. The datum of higher-than-normal fluid pressures is associated with the alternating sandstone and shale facies and the massive shale facies. Faulting and salt tectonics have complicated the depositional patterns and influenced the distribution of geopressured reservoirs (Wallace et a1 1978). The sandstones in the alternating sandstone and shale facies have the greatest potential for geopressured-geothermal energy development. Due to the insulating effect of surrounding shales, temperatures of the geopressured-geothermal brines typically range from 250 F to over 350 F, and under prevailing temperature, pressure, and salinity conditions, the brine contains 20 or more cubic feet of methane per barrel. Wallace et al (1978) estimated the geopressured-geothermal energy in Gulf Coast sandstone pore fluids to a depth of 22,500 feet to be 5,700 TCF of methane and 11,000 quads of thermal energy.
• Physical Description: vp

Subject

• Keyword: Natural Gas
• Keyword: Methane
• Keyword: Us Gulf Coast
• Keyword: Sandstones
• Keyword: Appalachian Mountains
• Keyword: Salinity
• Keyword: Contractors
• Keyword: Research Programs
• Keyword: Tectonics
• Keyword: Shales
• Keyword: Brines
• Keyword: Gulf Of Mexico
• STI Subject Categories: 03 Natural Gas
• Keyword: Sedimentary Basins
• Keyword: Distribution

Source

• Conference: Proceedings of the Natural Gas R&D Contractors Review Meeting, April 1989

Collection

• Name: Office of Scientific & Technical Information Technical Reports
  Code: OSTI

Institution

• Name: UNT Libraries Government Documents Department
  Code: UNTGD

Resource Type

• Article

Format

• Text

Identifier

• Report No.: DOE/METC-89/6103
• Office of Scientific & Technical Information Report Number: 896394
• Archival Resource Key: ark:/67531/metadc877391