Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993

The grantee will evaluate the influence of hydrate production on ground subsidence near the wellbore and the surface. The objective of this research will be achieved by using computer simulations of what is expected in a hydrate reservoir during the production stage as reported by hydrate production...

Full description

Bibliographic Details
Main Author: Siriwardane, H.J.
Language:unknown
Published: 2008
Subjects:
Online Access:http://www.osti.gov/servlets/purl/10175491
https://www.osti.gov/biblio/10175491
https://doi.org/10.2172/10175491
id ftosti:oai:osti.gov:10175491
record_format openpolar
spelling ftosti:oai:osti.gov:10175491 2023-07-30T04:06:17+02:00 Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993 Siriwardane, H.J. 2008-02-12 application/pdf http://www.osti.gov/servlets/purl/10175491 https://www.osti.gov/biblio/10175491 https://doi.org/10.2172/10175491 unknown http://www.osti.gov/servlets/purl/10175491 https://www.osti.gov/biblio/10175491 https://doi.org/10.2172/10175491 doi:10.2172/10175491 03 NATURAL GAS 58 GEOSCIENCES GAS HYDRATES PRODUCTION GROUND SUBSIDENCE MATHEMATICAL MODELS PROGRESS REPORT PERMAFROST NATURAL GAS HYDRATE DEPOSITS EXPLOITATION GROUND MOTION ROCK MECHANICS PARAMETRIC ANALYSIS COMPUTERIZED SIMULATION FINITE ELEMENT METHOD MECHANICAL PROPERTIES 2008 ftosti https://doi.org/10.2172/10175491 2023-07-11T11:00:59Z The grantee will evaluate the influence of hydrate production on ground subsidence near the wellbore and the surface. The objective of this research will be achieved by using computer simulations of what is expected in a hydrate reservoir during the production stage as reported by hydrate production models and available data. The model will be based on theories of continuum mechanics, thermomechnanics of hydrate production, principles of rock mechanics and geomechanics, and special features of geomaterials under cold temperatures such as those found in permafrost regions. The research work involved in the proposed investigation will be divided into three major tasks: mechanics of subsidence in permafrost regions; modeling of subsidence; and parametric studies. Under task 1, the literature survey was completed, and following factors were identified influencing subsidence: overburden depth; extent of dissociated (or depleted) hydrate reservoir; rock/frozen soil mechanical properties and strength; and reservoir compaction characteristics. Under task 2, technical progress is reported for studies on: mechanical properties; simulation of reservoir compression; and computer modeling effort. Other/Unknown Material permafrost SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 03 NATURAL GAS
58 GEOSCIENCES
GAS HYDRATES
PRODUCTION
GROUND SUBSIDENCE
MATHEMATICAL MODELS
PROGRESS REPORT
PERMAFROST
NATURAL GAS HYDRATE DEPOSITS
EXPLOITATION
GROUND MOTION
ROCK MECHANICS
PARAMETRIC ANALYSIS
COMPUTERIZED SIMULATION
FINITE ELEMENT METHOD
MECHANICAL PROPERTIES
spellingShingle 03 NATURAL GAS
58 GEOSCIENCES
GAS HYDRATES
PRODUCTION
GROUND SUBSIDENCE
MATHEMATICAL MODELS
PROGRESS REPORT
PERMAFROST
NATURAL GAS HYDRATE DEPOSITS
EXPLOITATION
GROUND MOTION
ROCK MECHANICS
PARAMETRIC ANALYSIS
COMPUTERIZED SIMULATION
FINITE ELEMENT METHOD
MECHANICAL PROPERTIES
Siriwardane, H.J.
Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993
topic_facet 03 NATURAL GAS
58 GEOSCIENCES
GAS HYDRATES
PRODUCTION
GROUND SUBSIDENCE
MATHEMATICAL MODELS
PROGRESS REPORT
PERMAFROST
NATURAL GAS HYDRATE DEPOSITS
EXPLOITATION
GROUND MOTION
ROCK MECHANICS
PARAMETRIC ANALYSIS
COMPUTERIZED SIMULATION
FINITE ELEMENT METHOD
MECHANICAL PROPERTIES
description The grantee will evaluate the influence of hydrate production on ground subsidence near the wellbore and the surface. The objective of this research will be achieved by using computer simulations of what is expected in a hydrate reservoir during the production stage as reported by hydrate production models and available data. The model will be based on theories of continuum mechanics, thermomechnanics of hydrate production, principles of rock mechanics and geomechanics, and special features of geomaterials under cold temperatures such as those found in permafrost regions. The research work involved in the proposed investigation will be divided into three major tasks: mechanics of subsidence in permafrost regions; modeling of subsidence; and parametric studies. Under task 1, the literature survey was completed, and following factors were identified influencing subsidence: overburden depth; extent of dissociated (or depleted) hydrate reservoir; rock/frozen soil mechanical properties and strength; and reservoir compaction characteristics. Under task 2, technical progress is reported for studies on: mechanical properties; simulation of reservoir compression; and computer modeling effort.
author Siriwardane, H.J.
author_facet Siriwardane, H.J.
author_sort Siriwardane, H.J.
title Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993
title_short Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993
title_full Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993
title_fullStr Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993
title_full_unstemmed Ground movements associated with gas hydrate production. Progress report, January 1--March 31, 1993
title_sort ground movements associated with gas hydrate production. progress report, january 1--march 31, 1993
publishDate 2008
url http://www.osti.gov/servlets/purl/10175491
https://www.osti.gov/biblio/10175491
https://doi.org/10.2172/10175491
genre permafrost
genre_facet permafrost
op_relation http://www.osti.gov/servlets/purl/10175491
https://www.osti.gov/biblio/10175491
https://doi.org/10.2172/10175491
doi:10.2172/10175491
op_doi https://doi.org/10.2172/10175491
_version_ 1772818788719263744