Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium

Abstract One important unresolved question in reactive transport is how pore-scale processes can be upscaled and how predictions can be made on the mutual effect of chemical processes and fluid flow in the porous medium. It is paramount to predict the location of mineral precipitation besides their...

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Main Authors: Mohammad Nooraiepour, Mohammad Masoudi, Helge Hellevang
Format: Article
Language:English
Published: Nature Publishing Group 2021-08-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-95237-7
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spelling doaj-13431192bb0844fbb9b399128a7c7d712021-08-15T11:26:01ZengNature Publishing GroupScientific Reports2045-23222021-08-0111111710.1038/s41598-021-95237-7Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous mediumMohammad Nooraiepour0Mohammad Masoudi1Helge Hellevang2CO2 Storage Research Group, Department of Geosciences, University of OsloCO2 Storage Research Group, Department of Geosciences, University of OsloCO2 Storage Research Group, Department of Geosciences, University of OsloAbstract One important unresolved question in reactive transport is how pore-scale processes can be upscaled and how predictions can be made on the mutual effect of chemical processes and fluid flow in the porous medium. It is paramount to predict the location of mineral precipitation besides their amount for understanding the fate of transport properties. However, current models and simulation approaches fail to predict precisely where crystals will nucleate and grow in the spatiotemporal domain. We present a new mathematical model for probabilistic mineral nucleation and precipitation. A Lattice Boltzmann implementation of the two-dimensional mineral surface was developed to evaluate geometry evolution when probabilistic nucleation criterion is incorporated. To provide high-resolution surface information on mineral precipitation, growth, and distribution, we conducted a total of 27 calcium carbonate synthesis experiments in the laboratory. The results indicate that nucleation events as precursors determine the location and timing of crystal precipitation. It is shown that reaction rate has primary control over covering the substrate with nuclei and, subsequently, solid-phase accumulation. The work provides insight into the spatiotemporal evolution of porous media by suggesting probabilistic and deterministic domains for studying reactive transport processes. We indicate in which length- and time-scales it is essential to incorporate probabilistic nucleation for valid predictions.https://doi.org/10.1038/s41598-021-95237-7
collection DOAJ
language English
format Article
sources DOAJ
author Mohammad Nooraiepour
Mohammad Masoudi
Helge Hellevang
spellingShingle Mohammad Nooraiepour
Mohammad Masoudi
Helge Hellevang
Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
Scientific Reports
author_facet Mohammad Nooraiepour
Mohammad Masoudi
Helge Hellevang
author_sort Mohammad Nooraiepour
title Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
title_short Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
title_full Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
title_fullStr Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
title_full_unstemmed Probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
title_sort probabilistic nucleation governs time, amount, and location of mineral precipitation and geometry evolution in the porous medium
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-08-01
description Abstract One important unresolved question in reactive transport is how pore-scale processes can be upscaled and how predictions can be made on the mutual effect of chemical processes and fluid flow in the porous medium. It is paramount to predict the location of mineral precipitation besides their amount for understanding the fate of transport properties. However, current models and simulation approaches fail to predict precisely where crystals will nucleate and grow in the spatiotemporal domain. We present a new mathematical model for probabilistic mineral nucleation and precipitation. A Lattice Boltzmann implementation of the two-dimensional mineral surface was developed to evaluate geometry evolution when probabilistic nucleation criterion is incorporated. To provide high-resolution surface information on mineral precipitation, growth, and distribution, we conducted a total of 27 calcium carbonate synthesis experiments in the laboratory. The results indicate that nucleation events as precursors determine the location and timing of crystal precipitation. It is shown that reaction rate has primary control over covering the substrate with nuclei and, subsequently, solid-phase accumulation. The work provides insight into the spatiotemporal evolution of porous media by suggesting probabilistic and deterministic domains for studying reactive transport processes. We indicate in which length- and time-scales it is essential to incorporate probabilistic nucleation for valid predictions.
url https://doi.org/10.1038/s41598-021-95237-7
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