Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings

The footprints of petroleum microseepage can be associated with chemical and microbial processes in initially homogeneous strata and/or with the fluid transport properties of the rocks through which oil and gas migrate. This work examines the role of such driving factors in two contrasting geologica...

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Main Authors: Vincenzo Costanzo-Álvarez, Jorge Mendoza, Milagrosa Aldana, Maria Jacome, Marisel Díaz, Keyla Ramirez, Cristina H. Amon
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-08-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.940799/full
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author Vincenzo Costanzo-Álvarez
Vincenzo Costanzo-Álvarez
Jorge Mendoza
Milagrosa Aldana
Maria Jacome
Marisel Díaz
Keyla Ramirez
Cristina H. Amon
Cristina H. Amon
author_facet Vincenzo Costanzo-Álvarez
Vincenzo Costanzo-Álvarez
Jorge Mendoza
Milagrosa Aldana
Maria Jacome
Marisel Díaz
Keyla Ramirez
Cristina H. Amon
Cristina H. Amon
author_sort Vincenzo Costanzo-Álvarez
collection DOAJ
description The footprints of petroleum microseepage can be associated with chemical and microbial processes in initially homogeneous strata and/or with the fluid transport properties of the rocks through which oil and gas migrate. This work examines the role of such driving factors in two contrasting geological settings by comparing numerical modeling predictions for upward methane microseepage with some field evidence for hydrocarbons transport and accumulation. The two case studies are a monitoring borehole (BH8) from a landfill in southern Ontario, Canada, and an oil well (Saltarin 1A) from the Eastern Llanos Basin in Colombia. Profiles of relative methane concentrations versus depth were generated using a time-dependent, one-dimensional, simulation of the advection-diffusion equation applied to multiple strata of soils, and sediments. The model employs the layered sequences of these two geological settings. The results obtained hinge on the standard permeability values for the rock types involved and their corresponding flow velocities and diffusion coefficients. Resistivity logs were utilized as direct proxies of hydrocarbon concentrations. As additional evidence for petroleum microseepage, experiments of electron paramagnetic resonance (EPR) were carried out in drilling cuts of Saltarin 1A to measure traces of organic matter free radicals concentrations (OMFRC). Extractable organic matter (EOM) and magnetic susceptibility data were also considered in interpreting the EPR results. Qualitative comparisons between modeled methane profiles and their corresponding resistivity logs suggest that microseepage and hydrocarbon accumulations are conditioned by the fluid transport properties of the rocks contained by BH8 and Saltarin 1A. Moreover, in most of the Saltarin 1A sequence, the OMFRC profiles follow the trends displayed by the resistivity and modeled methane logs. Thus, the EPR data also indicates that hydrocarbon microseepage and accumulation are largely controlled by lithology. Conversely, EOM and magnetic susceptibility appear to be evidence for hydrocarbon-mediated near-surface chemical processes.
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spelling doaj.art-f1d18bff910042e8ba99e303e067d7472022-12-22T02:51:52ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632022-08-011010.3389/feart.2022.940799940799Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological SettingsVincenzo Costanzo-Álvarez0Vincenzo Costanzo-Álvarez1Jorge Mendoza2Milagrosa Aldana3Maria Jacome4Marisel Díaz5Keyla Ramirez6Cristina H. Amon7Cristina H. Amon8Department of Mechanical and Industrial Engineering, University of Toronto, Toronto, ON, CanadaDepartamento de Ciencias de la Tierra, Universidad Simón Bolívar, Caracas, VenezuelaFacultad de Ingeniería en Ciencias de la Tierra, Escuela Superior Politécnica del Litoral ESPOL, Guayaquil, EcuadorDepartamento de Ciencias de la Tierra, Universidad Simón Bolívar, Caracas, VenezuelaFaculty of Applied Sciences and Technology, Humber Institute of Technology and Advanced Learning, Toronto, ON, CanadaCentro de Física, Instituto Venezolano de Investigaciones Científicas, Miranda, VenezuelaFUNVISIS Fundación Venezolana de Investigaciones Sismológicas, Caracas, VenezuelaDepartment of Mechanical and Industrial Engineering, University of Toronto, Toronto, ON, CanadaDepartment of Chemical Engineering and Applied Chemistry University of Toronto, Toronto, ON, CanadaThe footprints of petroleum microseepage can be associated with chemical and microbial processes in initially homogeneous strata and/or with the fluid transport properties of the rocks through which oil and gas migrate. This work examines the role of such driving factors in two contrasting geological settings by comparing numerical modeling predictions for upward methane microseepage with some field evidence for hydrocarbons transport and accumulation. The two case studies are a monitoring borehole (BH8) from a landfill in southern Ontario, Canada, and an oil well (Saltarin 1A) from the Eastern Llanos Basin in Colombia. Profiles of relative methane concentrations versus depth were generated using a time-dependent, one-dimensional, simulation of the advection-diffusion equation applied to multiple strata of soils, and sediments. The model employs the layered sequences of these two geological settings. The results obtained hinge on the standard permeability values for the rock types involved and their corresponding flow velocities and diffusion coefficients. Resistivity logs were utilized as direct proxies of hydrocarbon concentrations. As additional evidence for petroleum microseepage, experiments of electron paramagnetic resonance (EPR) were carried out in drilling cuts of Saltarin 1A to measure traces of organic matter free radicals concentrations (OMFRC). Extractable organic matter (EOM) and magnetic susceptibility data were also considered in interpreting the EPR results. Qualitative comparisons between modeled methane profiles and their corresponding resistivity logs suggest that microseepage and hydrocarbon accumulations are conditioned by the fluid transport properties of the rocks contained by BH8 and Saltarin 1A. Moreover, in most of the Saltarin 1A sequence, the OMFRC profiles follow the trends displayed by the resistivity and modeled methane logs. Thus, the EPR data also indicates that hydrocarbon microseepage and accumulation are largely controlled by lithology. Conversely, EOM and magnetic susceptibility appear to be evidence for hydrocarbon-mediated near-surface chemical processes.https://www.frontiersin.org/articles/10.3389/feart.2022.940799/fullmethane microseepageadvection-diffusion equationhydrocarbon-induced diagenesiselectron paramagnetic resonanceresistivity logorganic matter free radical
spellingShingle Vincenzo Costanzo-Álvarez
Vincenzo Costanzo-Álvarez
Jorge Mendoza
Milagrosa Aldana
Maria Jacome
Marisel Díaz
Keyla Ramirez
Cristina H. Amon
Cristina H. Amon
Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings
Frontiers in Earth Science
methane microseepage
advection-diffusion equation
hydrocarbon-induced diagenesis
electron paramagnetic resonance
resistivity log
organic matter free radical
title Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings
title_full Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings
title_fullStr Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings
title_full_unstemmed Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings
title_short Comparing Direct Numerical Modeling Predictions With Field Evidence for Methane Vertical Microseepage in Two Geological Settings
title_sort comparing direct numerical modeling predictions with field evidence for methane vertical microseepage in two geological settings
topic methane microseepage
advection-diffusion equation
hydrocarbon-induced diagenesis
electron paramagnetic resonance
resistivity log
organic matter free radical
url https://www.frontiersin.org/articles/10.3389/feart.2022.940799/full
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