Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano

Detalhes bibliográficos
Autor(a) principal: Castro, Eduardo da Silva
Data de Publicação: 2021
Tipo de documento: Tese
Idioma: por
Título da fonte: Biblioteca Digital de Teses e Dissertações do LNCC
Texto Completo: https://tede.lncc.br/handle/tede/345
Resumo: In the context of canonical finite volume discretizations, the predictive capacity of hydrody- namic simulators in complex reservoirs, containing geological fault zones, strongly depends on the quality of the values assigned to hydraulic transmissibility multipliers, whose magnitude tends to reduce the values of intact rock due to the presence of discontinuities. In the context of two-point stencil approximations, the linear dependence with the tailings extension is commonly postulated for transmissibility, with values calculated via harmonic mean between the permeabilities of adjacent cells and that of the fault. In order to build the behavior of transmissibility multipliers in a more rigorous way, based on information from hydrodynamics at the finest scales, in this work we propose an alternative methodology to the purely macroscopic approach, built from an innovative three-scale model. Such model exhibits the ability to describe the complex microstructure of the failure zone, encompassing the nucleus and multiple adjacent damage regions, characterized by the presence of deformation bands, fractures and joints. On the finer scale of the problem, the proposed new approach describes geological structures occupying disjoint three-dimensional subdomains, and gives rise to the model called high-fidelity. In the first process of upscaling (micro-meso) we build strictly reduced models, where the fault zone is now treated as a (n − 1) dimensional (n = 2, 3) variety embedded in the matrix porous, giving rise to the presence of jumps in the fields of pressure and speed. The finite element discretization of the governing equations of the single-phase flow of the reduced model is built based on the addition of additional degrees of freedom to approximate the potential in the discontinuity. Subsequently, we proceed in the context of a flow-based upscaling process to propagate information from the reduced model to the scale of reservoir simulation cells (macroscopic). The wealth of information inherent to this procedure generates innovative constitutive laws for transmissibilities, incorporating the effects of the microstructure of the fault zone, which are commonly neglected by approaches of a purely macroscopic nature based on the approximation of two points. The methodology proposed in this work shows an enormous potential for the development of transmissibility preprocessors, more accurate to be used in commercial simulators. The information enrichment inherent to the model is illustrated in several computer simulations.
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spelling Murad, Marcio ArabBarroso, Josué dos SantosGuerreiro, João Nisan CorreiaMurad, Marcio ArabLoula, Abimael Fernando DouradoBorges, Marcio RentesManzolio, Osvaldo LuisGomes, Igor Fernandeshttp://lattes.cnpq.br/7483132144832976Castro, Eduardo da Silva2023-04-05T18:29:55Z2021-12-17CASTRO, E. S. Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano. 2021. 108 f. Tese (Programa de Pós-Graduação em Modelagem Computacional) - Laboratório Nacional de Computação Científica, Petrópolis, 2021.https://tede.lncc.br/handle/tede/345In the context of canonical finite volume discretizations, the predictive capacity of hydrody- namic simulators in complex reservoirs, containing geological fault zones, strongly depends on the quality of the values assigned to hydraulic transmissibility multipliers, whose magnitude tends to reduce the values of intact rock due to the presence of discontinuities. In the context of two-point stencil approximations, the linear dependence with the tailings extension is commonly postulated for transmissibility, with values calculated via harmonic mean between the permeabilities of adjacent cells and that of the fault. In order to build the behavior of transmissibility multipliers in a more rigorous way, based on information from hydrodynamics at the finest scales, in this work we propose an alternative methodology to the purely macroscopic approach, built from an innovative three-scale model. Such model exhibits the ability to describe the complex microstructure of the failure zone, encompassing the nucleus and multiple adjacent damage regions, characterized by the presence of deformation bands, fractures and joints. On the finer scale of the problem, the proposed new approach describes geological structures occupying disjoint three-dimensional subdomains, and gives rise to the model called high-fidelity. In the first process of upscaling (micro-meso) we build strictly reduced models, where the fault zone is now treated as a (n − 1) dimensional (n = 2, 3) variety embedded in the matrix porous, giving rise to the presence of jumps in the fields of pressure and speed. The finite element discretization of the governing equations of the single-phase flow of the reduced model is built based on the addition of additional degrees of freedom to approximate the potential in the discontinuity. Subsequently, we proceed in the context of a flow-based upscaling process to propagate information from the reduced model to the scale of reservoir simulation cells (macroscopic). The wealth of information inherent to this procedure generates innovative constitutive laws for transmissibilities, incorporating the effects of the microstructure of the fault zone, which are commonly neglected by approaches of a purely macroscopic nature based on the approximation of two points. The methodology proposed in this work shows an enormous potential for the development of transmissibility preprocessors, more accurate to be used in commercial simulators. The information enrichment inherent to the model is illustrated in several computer simulations.No contexto de discretizações canônicas de volumes finitos, a capacidade de predição dos simuladores hidrodinâmicos em reservatórios complexos, contendo zonas de falhas geológicas, depende fortemente da qualidade dos valores atribuídos aos multiplicadores de transmissibilidade hidráulica, cuja magnitude, tende a reduzir os valores da rocha intacta devido a presença de descontinuidades. No contexto das aproximações caracterizadas por estêncil de dois pontos, a dependência linear com a extensão do rejeito é comumente postuladas para a transmissibilidade, com valores calculados via média harmônica entre as permeabilidades das células adjacentes e a da falha. Com o objetivo de construir o comportamento dos multiplicadores de transmissibilidade de uma forma mais rigorosa, baseado na informação proveniente da hidrodinâmica nas escalas mais finas, neste trabalho propomos uma metodologia alternativa à abordagem puramente macroscópica, construída a partir de um modelo inovador posto em três escalas. Tal modelo exibe capacidade de descrever a microestrutura complexa da zona de falha, englobando núcleo e múltiplas regiões de dano adjacentes, caracterizadas pela presença de bandas de deformação, fraturas e juntas. Na escala mais fina do problema, a nova abordagem descreve estruturas geológicas ocupantes de subdomínios tridimensionais disjuntos, e dá origem ao modelo denominado de alta-fidelidade. No primeiro processo de upscaling (micro-meso) construímos rigoro- samente modelos reduzidos, onde a zona da falha é agora tratada como uma variedade (n − 1) dimensional (n = 2, 3) embebida na matriz porosa, dando origem à presença de saltos nos campos das pressão e velocidade. A discretização por elementos finitos das equações governantes do escoamento monofásico do modelo reduzido é construída baseada na adição de graus de liberdade adicionais para a aproximação do potencial na descontinuidade. Subsequentemente, procedemos no contexto de um processo de flow-based upscaling para propagar a informações proveniente do modelo reduzido para a escala das células de simulação de reservatório (macroscópica). A riqueza de informação inerente a este procedimento exibe potencial para geração de leis constitutivas inovadoras para as transmissibilidades, incorporando os efeitos da microestrutura da zona de falhas, os quais são comumente negligenciados pela aproximação de natureza puramente macroscópica, baseada na aproximação de dois pontos. A metodologia proposta neste trabalho exibe um enorme potencial para o desenvolvimento de pré-processadores de transmissibilidade, mais acurados para serem utilizados em simuladores comerciais. 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dc.title.por.fl_str_mv Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
title Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
spellingShingle Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
Castro, Eduardo da Silva
Reservatórios
Modelos hidrodinâmicos
Fraturas (Geologia)
Método dos elementos finitos
Aprendizado por computador
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL::ENGENHARIA HIDRAULICA
title_short Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
title_full Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
title_fullStr Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
title_full_unstemmed Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
title_sort Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano
author Castro, Eduardo da Silva
author_facet Castro, Eduardo da Silva
author_role author
dc.contributor.advisor1.fl_str_mv Murad, Marcio Arab
dc.contributor.advisor2.fl_str_mv Barroso, Josué dos Santos
dc.contributor.advisor-co1.fl_str_mv Guerreiro, João Nisan Correia
dc.contributor.referee1.fl_str_mv Murad, Marcio Arab
dc.contributor.referee2.fl_str_mv Loula, Abimael Fernando Dourado
dc.contributor.referee3.fl_str_mv Borges, Marcio Rentes
dc.contributor.referee4.fl_str_mv Manzolio, Osvaldo Luis
dc.contributor.referee5.fl_str_mv Gomes, Igor Fernandes
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/7483132144832976
dc.contributor.author.fl_str_mv Castro, Eduardo da Silva
contributor_str_mv Murad, Marcio Arab
Barroso, Josué dos Santos
Guerreiro, João Nisan Correia
Murad, Marcio Arab
Loula, Abimael Fernando Dourado
Borges, Marcio Rentes
Manzolio, Osvaldo Luis
Gomes, Igor Fernandes
dc.subject.por.fl_str_mv Reservatórios
Modelos hidrodinâmicos
Fraturas (Geologia)
Método dos elementos finitos
Aprendizado por computador
topic Reservatórios
Modelos hidrodinâmicos
Fraturas (Geologia)
Método dos elementos finitos
Aprendizado por computador
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL::ENGENHARIA HIDRAULICA
dc.subject.cnpq.fl_str_mv CNPQ::ENGENHARIAS::ENGENHARIA CIVIL::ENGENHARIA HIDRAULICA
description In the context of canonical finite volume discretizations, the predictive capacity of hydrody- namic simulators in complex reservoirs, containing geological fault zones, strongly depends on the quality of the values assigned to hydraulic transmissibility multipliers, whose magnitude tends to reduce the values of intact rock due to the presence of discontinuities. In the context of two-point stencil approximations, the linear dependence with the tailings extension is commonly postulated for transmissibility, with values calculated via harmonic mean between the permeabilities of adjacent cells and that of the fault. In order to build the behavior of transmissibility multipliers in a more rigorous way, based on information from hydrodynamics at the finest scales, in this work we propose an alternative methodology to the purely macroscopic approach, built from an innovative three-scale model. Such model exhibits the ability to describe the complex microstructure of the failure zone, encompassing the nucleus and multiple adjacent damage regions, characterized by the presence of deformation bands, fractures and joints. On the finer scale of the problem, the proposed new approach describes geological structures occupying disjoint three-dimensional subdomains, and gives rise to the model called high-fidelity. In the first process of upscaling (micro-meso) we build strictly reduced models, where the fault zone is now treated as a (n − 1) dimensional (n = 2, 3) variety embedded in the matrix porous, giving rise to the presence of jumps in the fields of pressure and speed. The finite element discretization of the governing equations of the single-phase flow of the reduced model is built based on the addition of additional degrees of freedom to approximate the potential in the discontinuity. Subsequently, we proceed in the context of a flow-based upscaling process to propagate information from the reduced model to the scale of reservoir simulation cells (macroscopic). The wealth of information inherent to this procedure generates innovative constitutive laws for transmissibilities, incorporating the effects of the microstructure of the fault zone, which are commonly neglected by approaches of a purely macroscopic nature based on the approximation of two points. The methodology proposed in this work shows an enormous potential for the development of transmissibility preprocessors, more accurate to be used in commercial simulators. The information enrichment inherent to the model is illustrated in several computer simulations.
publishDate 2021
dc.date.issued.fl_str_mv 2021-12-17
dc.date.accessioned.fl_str_mv 2023-04-05T18:29:55Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/doctoralThesis
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dc.identifier.citation.fl_str_mv CASTRO, E. S. Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano. 2021. 108 f. Tese (Programa de Pós-Graduação em Modelagem Computacional) - Laboratório Nacional de Computação Científica, Petrópolis, 2021.
dc.identifier.uri.fl_str_mv https://tede.lncc.br/handle/tede/345
identifier_str_mv CASTRO, E. S. Nova família de modelos hidrodinâmicos reduzidos aplicados a rochas contendo falhas com múltiplas zonas de dano. 2021. 108 f. Tese (Programa de Pós-Graduação em Modelagem Computacional) - Laboratório Nacional de Computação Científica, Petrópolis, 2021.
url https://tede.lncc.br/handle/tede/345
dc.language.iso.fl_str_mv por
language por
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dc.publisher.none.fl_str_mv Laboratório Nacional de Computação Científica
dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Modelagem Computacional
dc.publisher.initials.fl_str_mv LNCC
dc.publisher.country.fl_str_mv Brasil
dc.publisher.department.fl_str_mv Coordenação de Pós-Graduação e Aperfeiçoamento (COPGA)
publisher.none.fl_str_mv Laboratório Nacional de Computação Científica
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repository.name.fl_str_mv Biblioteca Digital de Teses e Dissertações do LNCC - Laboratório Nacional de Computação Científica (LNCC)
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