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Computational topology-based characterization of pore space changes due to chemical dissolution of rocks. / Lisitsa, Vadim; Bazaikin, Yaroslav; Khachkova, Tatyana.
в: Applied Mathematical Modelling, Том 88, 01.12.2020, стр. 21-37.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Computational topology-based characterization of pore space changes due to chemical dissolution of rocks
AU - Lisitsa, Vadim
AU - Bazaikin, Yaroslav
AU - Khachkova, Tatyana
N1 - Publisher Copyright: © 2020 Elsevier Inc. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/12/1
Y1 - 2020/12/1
N2 - In this paper, we present an algorithm for the numerical simulation of reactive transport at the pore scale to facilitate observation of pore space and rock matrix evolution. Moreover, simulation at the pore scale opens up the possibility of estimating changes in the transport properties of rocks, such as permeability and tortuosity. To quantitatively analyze pore space evolution, we developed a numerical algorithm that can be used to construct persistence diagrams of the connectivity components for pore space and the rock matrix, which characterize the topology evolution during rock matrix dissolution. Introducing the “bottle-neck” metric in the space of the persistence diagrams, we cluster the numerical experiments in terms of similarities in topology evolution. We demonstrate that the application of this metric to the persistence diagrams allowed us to distinguish topologically different dissolution scenarios, for instance, the formation of a dissolution front near the inlet, homogeneous dissolution of the matrix inside the core sample, and formation of wormholes. We illustrate that the differences in topology evolution lead to cross-correlations among the transport properties of rocks (porosity-permeability-tortuosity).
AB - In this paper, we present an algorithm for the numerical simulation of reactive transport at the pore scale to facilitate observation of pore space and rock matrix evolution. Moreover, simulation at the pore scale opens up the possibility of estimating changes in the transport properties of rocks, such as permeability and tortuosity. To quantitatively analyze pore space evolution, we developed a numerical algorithm that can be used to construct persistence diagrams of the connectivity components for pore space and the rock matrix, which characterize the topology evolution during rock matrix dissolution. Introducing the “bottle-neck” metric in the space of the persistence diagrams, we cluster the numerical experiments in terms of similarities in topology evolution. We demonstrate that the application of this metric to the persistence diagrams allowed us to distinguish topologically different dissolution scenarios, for instance, the formation of a dissolution front near the inlet, homogeneous dissolution of the matrix inside the core sample, and formation of wormholes. We illustrate that the differences in topology evolution lead to cross-correlations among the transport properties of rocks (porosity-permeability-tortuosity).
KW - Betti numbers
KW - Computational topology
KW - Finite-differences
KW - Level-set
KW - Persistence diagram,
KW - Rock dissolution
KW - Persistence diagram
KW - POROUS-MEDIA
KW - MECHANISMS
KW - SCALE
KW - LEVEL-SET METHODS
KW - FLOW
UR - http://www.scopus.com/inward/record.url?scp=85087591561&partnerID=8YFLogxK
U2 - 10.1016/j.apm.2020.06.037
DO - 10.1016/j.apm.2020.06.037
M3 - Article
AN - SCOPUS:85087591561
VL - 88
SP - 21
EP - 37
JO - Applied Mathematical Modelling
JF - Applied Mathematical Modelling
SN - 0307-904X
ER -
ID: 24721636