Linear Stability Analysis of Double-Diffusive Convection in Porous Media, with Application to Geological Storage of CO.

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Title: Linear Stability Analysis of Double-Diffusive Convection in Porous Media, with Application to Geological Storage of CO.
Authors: Javaheri, Mohammad1, Abedi, Jalal1 jabedi@ucalgary.ca, Hassanzadeh, Hassan1
Source: Transport in Porous Media. Sep2010, Vol. 84 Issue 2, p441-456. 16p.
Subjects: Natural heat convection, Diffusion, Fluid dynamics, Porous materials, Carbon sequestration, Stability (Mechanics), Wavelengths
Abstract: Onset of double-diffusive buoyancy-driven flow resulted from vertical temperature and concentration gradients in a horizontal layer of a saturated and homogenous porous medium is investigated using amplification factor theory. After injection of CO into a deep saline aquifer, the density of the brine saturated with CO increases slightly. This increase in density induces natural convection. The effect of geothermal gradient is also considered in this work as a second incentive for convection and the double-diffusion convection was studied. Linear stability analysis is used to predict the inception of instabilities and initial wavelength of the convective instabilities. The analysis presented is applied to acid gas injection (as an analogue for CO storage) into saline aquifers in the Alberta basin. It is found that the geothermal gradient does not have significant effect on the onset of convection for these aquifers. It is shown that the geothermal effects on the onset of natural convection are negligible as compared to the solutal effects induced by dissolution and diffusion of CO in deep saline aquifers. Therefore, the linear stability analysis and the long-term numerical simulation of CO sequestration into such saline aquifers may be assumed to be isothermal in terms of natural convection occurrence. [ABSTRACT FROM AUTHOR]
Copyright of Transport in Porous Media is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: <searchLink fieldCode="JN" term="%22Transport+in+Porous+Media%22">Transport in Porous Media</searchLink>. Sep2010, Vol. 84 Issue 2, p441-456. 16p.
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  Data: <searchLink fieldCode="DE" term="%22Natural+heat+convection%22">Natural heat convection</searchLink><br /><searchLink fieldCode="DE" term="%22Diffusion%22">Diffusion</searchLink><br /><searchLink fieldCode="DE" term="%22Fluid+dynamics%22">Fluid dynamics</searchLink><br /><searchLink fieldCode="DE" term="%22Porous+materials%22">Porous materials</searchLink><br /><searchLink fieldCode="DE" term="%22Carbon+sequestration%22">Carbon sequestration</searchLink><br /><searchLink fieldCode="DE" term="%22Stability+%28Mechanics%29%22">Stability (Mechanics)</searchLink><br /><searchLink fieldCode="DE" term="%22Wavelengths%22">Wavelengths</searchLink>
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  Data: Onset of double-diffusive buoyancy-driven flow resulted from vertical temperature and concentration gradients in a horizontal layer of a saturated and homogenous porous medium is investigated using amplification factor theory. After injection of CO into a deep saline aquifer, the density of the brine saturated with CO increases slightly. This increase in density induces natural convection. The effect of geothermal gradient is also considered in this work as a second incentive for convection and the double-diffusion convection was studied. Linear stability analysis is used to predict the inception of instabilities and initial wavelength of the convective instabilities. The analysis presented is applied to acid gas injection (as an analogue for CO storage) into saline aquifers in the Alberta basin. It is found that the geothermal gradient does not have significant effect on the onset of convection for these aquifers. It is shown that the geothermal effects on the onset of natural convection are negligible as compared to the solutal effects induced by dissolution and diffusion of CO in deep saline aquifers. Therefore, the linear stability analysis and the long-term numerical simulation of CO sequestration into such saline aquifers may be assumed to be isothermal in terms of natural convection occurrence. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Transport in Porous Media is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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        Value: 10.1007/s11242-009-9513-z
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        Text: English
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      – SubjectFull: Natural heat convection
        Type: general
      – SubjectFull: Diffusion
        Type: general
      – SubjectFull: Fluid dynamics
        Type: general
      – SubjectFull: Porous materials
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      – SubjectFull: Carbon sequestration
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      – SubjectFull: Stability (Mechanics)
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      – TitleFull: Linear Stability Analysis of Double-Diffusive Convection in Porous Media, with Application to Geological Storage of CO.
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              M: 09
              Text: Sep2010
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