Numerical Studies on Two-Way Coupled Fluid Flow and Geomechanics in Hydrate Deposits (Record no. 187538)

MARC details
000 -LEADER
fixed length control field 03032nab a2200229 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2012 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Numerical Studies on Two-Way Coupled Fluid Flow and Geomechanics in Hydrate Deposits
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. jun. 2012
270 ## - FECHA DE CARGA
Fecha de carga 22/01/2013 ; 22/01/2013
300 ## - DESCRIPCION FISICA
Otra extensión 16 p. ; 485-501
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: Coupled flow and geomechanics play an important role in the analysis of gas-hydrate reservoirs under production. The stiffness of the rock skeleton and the deformation of the reservoir, as well as porosity and permeability, are directly influenced by (and interrelated with) changes in pressure and temperature and in fluid- (water and gas) and solid- (hydrate and ice) phase saturations. Fluid and solid phases may coexist, which, coupled with steep temperature and pressure gradients, results in strong nonlinearities in the coupled flow and mechanics processes, making the description of system behavior in dissociating hydrate deposits exceptionally complicated. In previous studies, the geological stability of hydrate-bearing sediments was investigated using one-way coupled analysis, in which the changes in fluid properties affect mechanics within the gas-hydrate reservoirs, but with no feedback from geomechanics to fluid flow. In this paper, we develop and test a rigorous two-way coupling between fluid flow and geomechanics, in which the solutions from mechanics are reflected in the solution of the flow problem through the adjustment of affected hydraulic properties. We employ the fixed-stress split method, which results in a convergent sequential implicit scheme. In this study of several hydrate-reservoir cases, we find noticeable differences between the results from one- and two-way couplings. The nature of the elliptic boundary value problem of quasistatic mechanics results in instantaneous compaction or dilation over the domain through loading from reservoir-fluid production. This induces a pressure rise or drop at early times (low-pressure diffusion), and consequently changes the effective stress instantaneously, possibly causing geological instability. Additionally, the pressure and temperature regime affects the various phase saturations, the rock stiffness, porosity, and permeability, thus affecting the fluid-flow regime. These changes are not captured accurately by the simpler one-way coupling. The tightly coupled sequential approach we propose provides a rigorous, two-way coupling model that captures the interrelationship between geomechanical and flow properties and processes, accurately describes the system behavior, and can be readily applied to large-scale problems of hydrate behavior in geologic media.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 2
773 0# - CORRECCIÓN
Título SPE Journal
Partes relacionadas 17
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Kim, J.
9 (RLIN) 52924
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Moridis, G.J.
9 (RLIN) 42539
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Yang, D.
9 (RLIN) 21331
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Rutqvist, J.
9 (RLIN) 42538
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 06/03/2026 200059661   200059661 06/03/2026 Artículo de Revista


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