Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates
Gas hydrates are crystalline, ice-like compounds of gas and water molecules that are formed under certain thermodynamic conditions. Hydrate deposits occur naturally within ocean sediments just below the sea floor at temperatures and pressures existing below about 500 meters water depth. Gas hydrate...
Main Authors: | , , , , , , |
---|---|
Other Authors: | |
Format: | Report |
Language: | English |
Published: |
Westport Technology Center
2006
|
Subjects: | |
Online Access: | https://doi.org/10.2172/920371 https://digital.library.unt.edu/ark:/67531/metadc898195/ |
id |
ftunivnotexas:info:ark/67531/metadc898195 |
---|---|
record_format |
openpolar |
spelling |
ftunivnotexas:info:ark/67531/metadc898195 2023-05-15T15:14:15+02:00 Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates Mohanty, Kishore Cook, Bill Hakimuddin, Mustafa Pitchumani, Ramanan Ogunlana, Damiola Burger, Jon Shillinglaw, John United States. Department of Energy. 2006-06-30 Text https://doi.org/10.2172/920371 https://digital.library.unt.edu/ark:/67531/metadc898195/ English eng Westport Technology Center grantno: FC26-02NT41327 doi:10.2172/920371 osti: 920371 https://digital.library.unt.edu/ark:/67531/metadc898195/ ark: ark:/67531/metadc898195 Methane Thermodynamics Dissociation Sodium Iodides Sediments Acoustics Hydrates 29 Energy Planning Policy And Economy Temperature Gradients Boundary Conditions Production Gas Hydrates Water Fluid Withdrawal Simulators Gulf Of Mexico Depressurization 03 Natural Gas Fossil Fuels Permafrost Report 2006 ftunivnotexas https://doi.org/10.2172/920371 2019-05-18T22:08:18Z Gas hydrates are crystalline, ice-like compounds of gas and water molecules that are formed under certain thermodynamic conditions. Hydrate deposits occur naturally within ocean sediments just below the sea floor at temperatures and pressures existing below about 500 meters water depth. Gas hydrate is also stable in conjunction with the permafrost in the Arctic. Most marine gas hydrate is formed of microbially generated gas. It binds huge amounts of methane into the sediments. Estimates of the amounts of methane sequestered in gas hydrates worldwide are speculative and range from about 100,000 to 270,000,000 trillion cubic feet (modified from Kvenvolden, 1993). Gas hydrate is one of the fossil fuel resources that is yet untapped, but may play a major role in meeting the energy challenge of this century. In this project novel techniques were developed to form and dissociate methane hydrates in porous media, to measure acoustic properties and CT properties during hydrate dissociation in the presence of a porous medium. Hydrate depressurization experiments in cores were simulated with the use of TOUGHFx/HYDRATE simulator. Input/output software was developed to simulate variable pressure boundary condition and improve the ease of use of the simulator. A series of simulations needed to be run to mimic the variable pressure condition at the production well. The experiments can be matched qualitatively by the hydrate simulator. The temperature of the core falls during hydrate dissociation; the temperature drop is higher if the fluid withdrawal rate is higher. The pressure and temperature gradients are small within the core. The sodium iodide concentration affects the dissociation pressure and rate. This procedure and data will be useful in designing future hydrate studies. Report Arctic Ice permafrost University of North Texas: UNT Digital Library Arctic |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Methane Thermodynamics Dissociation Sodium Iodides Sediments Acoustics Hydrates 29 Energy Planning Policy And Economy Temperature Gradients Boundary Conditions Production Gas Hydrates Water Fluid Withdrawal Simulators Gulf Of Mexico Depressurization 03 Natural Gas Fossil Fuels Permafrost |
spellingShingle |
Methane Thermodynamics Dissociation Sodium Iodides Sediments Acoustics Hydrates 29 Energy Planning Policy And Economy Temperature Gradients Boundary Conditions Production Gas Hydrates Water Fluid Withdrawal Simulators Gulf Of Mexico Depressurization 03 Natural Gas Fossil Fuels Permafrost Mohanty, Kishore Cook, Bill Hakimuddin, Mustafa Pitchumani, Ramanan Ogunlana, Damiola Burger, Jon Shillinglaw, John Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates |
topic_facet |
Methane Thermodynamics Dissociation Sodium Iodides Sediments Acoustics Hydrates 29 Energy Planning Policy And Economy Temperature Gradients Boundary Conditions Production Gas Hydrates Water Fluid Withdrawal Simulators Gulf Of Mexico Depressurization 03 Natural Gas Fossil Fuels Permafrost |
description |
Gas hydrates are crystalline, ice-like compounds of gas and water molecules that are formed under certain thermodynamic conditions. Hydrate deposits occur naturally within ocean sediments just below the sea floor at temperatures and pressures existing below about 500 meters water depth. Gas hydrate is also stable in conjunction with the permafrost in the Arctic. Most marine gas hydrate is formed of microbially generated gas. It binds huge amounts of methane into the sediments. Estimates of the amounts of methane sequestered in gas hydrates worldwide are speculative and range from about 100,000 to 270,000,000 trillion cubic feet (modified from Kvenvolden, 1993). Gas hydrate is one of the fossil fuel resources that is yet untapped, but may play a major role in meeting the energy challenge of this century. In this project novel techniques were developed to form and dissociate methane hydrates in porous media, to measure acoustic properties and CT properties during hydrate dissociation in the presence of a porous medium. Hydrate depressurization experiments in cores were simulated with the use of TOUGHFx/HYDRATE simulator. Input/output software was developed to simulate variable pressure boundary condition and improve the ease of use of the simulator. A series of simulations needed to be run to mimic the variable pressure condition at the production well. The experiments can be matched qualitatively by the hydrate simulator. The temperature of the core falls during hydrate dissociation; the temperature drop is higher if the fluid withdrawal rate is higher. The pressure and temperature gradients are small within the core. The sodium iodide concentration affects the dissociation pressure and rate. This procedure and data will be useful in designing future hydrate studies. |
author2 |
United States. Department of Energy. |
format |
Report |
author |
Mohanty, Kishore Cook, Bill Hakimuddin, Mustafa Pitchumani, Ramanan Ogunlana, Damiola Burger, Jon Shillinglaw, John |
author_facet |
Mohanty, Kishore Cook, Bill Hakimuddin, Mustafa Pitchumani, Ramanan Ogunlana, Damiola Burger, Jon Shillinglaw, John |
author_sort |
Mohanty, Kishore |
title |
Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates |
title_short |
Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates |
title_full |
Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates |
title_fullStr |
Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates |
title_full_unstemmed |
Petrophysical Characterization and Reservoir Simulator for Methane Gas Production from Gulf of Mexico Hydrates |
title_sort |
petrophysical characterization and reservoir simulator for methane gas production from gulf of mexico hydrates |
publisher |
Westport Technology Center |
publishDate |
2006 |
url |
https://doi.org/10.2172/920371 https://digital.library.unt.edu/ark:/67531/metadc898195/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ice permafrost |
genre_facet |
Arctic Ice permafrost |
op_relation |
grantno: FC26-02NT41327 doi:10.2172/920371 osti: 920371 https://digital.library.unt.edu/ark:/67531/metadc898195/ ark: ark:/67531/metadc898195 |
op_doi |
https://doi.org/10.2172/920371 |
_version_ |
1766344714484711424 |