Title:
Numerical investigation of multiphase Darcy-Forchheimer flow and contaminant transport during SO₂ co-injection with CO₂ in deep saline aquifers

dc.contributor.advisor Aral, Mustafa M.
dc.contributor.author Zhang, Andi
dc.contributor.committeeMember Stieglitz, Marc
dc.contributor.committeeMember Luo, Jian
dc.contributor.committeeMember Guan, Jiabao
dc.contributor.committeeMember Stieglitz, Marc
dc.contributor.committeeMember Luo, Jian
dc.contributor.committeeMember Uzer, Turgay
dc.contributor.department Civil and Environmental Engineering
dc.date.accessioned 2013-09-20T13:26:05Z
dc.date.available 2013-09-20T13:26:05Z
dc.date.created 2013-08
dc.date.issued 2013-06-24
dc.date.submitted August 2013
dc.date.updated 2013-09-20T13:26:05Z
dc.description.abstract Of all the strategies to reduce carbon emissions, carbon dioxide (CO₂) geological sequestration is an immediately available option for removing large amounts of the gas from the atmosphere. However, our understanding of the transition behavior between Forchheimer and Darcy flow through porous media during CO₂ injection is currently very limited. In addition, the kinetic mass transfer of SO₂ and CO₂ from CO₂ stream to the saline and the fully coupling between the changes of porosity and permeability and multiphase flow are two significant dimensions to investigate the brine acidification and the induced porosity and permeability changes due to SO₂ co-injection with CO₂. Therefore, this dissertation develops a multiphase flow, contaminant transport and geochemical model which includes the kinetic mass transfer of SO₂ into deep saline aquifers and obtains the critical Forchheimer number for both water and CO₂ by using the experimental data in the literature. The critical Forchheimer numbers and the multiphase flow model are first applied to analyze the application problem involving the injection of CO₂ into deep saline aquifers. The results show that the Forchheimer effect would result in higher displacement efficiency with a magnitude of more than 50% in the Forchheimer regime than that for Darcy flow, which could increase the storage capacity for the same injection rate and volume of a site. Another merit for the incorporation of Forchheimer effect is that more CO₂ would be accumulated in the lower half of the domain and lower pressure would be imposed on the lower boundary of the cap-rock. However, as a price for the advantages mentioned above, the injection pressure required in Forchheimer flow would be higher than that for Darcy flow. The fluid flow and contaminant transport and geochemical model is then applied to analyze the brine acidification and induced porosity and permeability changes due to SO₂ co-injection. The results show that the co-injection of SO₂ with CO₂ would lead to a substantially acid zone near the injecting well and it is important to include the kinetic dissolution of SO₂ from the CO₂ stream to the water phase into the simulation models, otherwise considerable errors would be introduced for the equilibrium assumption. This study provides a useful tool for future analysis and comprehension of multiphase Darcy-Forchheimer flow and brine acidification of CO₂ injection into deep saline aquifers. Results from this dissertation have practical use for scientists and engineers concerned with the description of flow behavior, and transport and fate of SO₂ during SO₂ co-injection with CO₂ in deep saline aquifers.
dc.description.degree Ph.D.
dc.format.mimetype application/pdf
dc.identifier.uri http://hdl.handle.net/1853/49065
dc.language.iso en_US
dc.publisher Georgia Institute of Technology
dc.subject Darcy-Forchheimer flow
dc.subject Multiphase flow
dc.subject Critical Forchheimer number
dc.subject Deep saline aquifers
dc.subject Contaminant transport
dc.subject CO₂ sequestration
dc.subject SO₂ co-injection
dc.subject.lcsh Darcy's law
dc.subject.lcsh Aquifers
dc.subject.lcsh Saline waters
dc.subject.lcsh Carbon dioxide
dc.subject.lcsh Carbon dioxide Environmental aspects
dc.subject.lcsh Carbon dioxide mitigation
dc.subject.lcsh Carbon sequestration
dc.subject.lcsh Geochemistry
dc.title Numerical investigation of multiphase Darcy-Forchheimer flow and contaminant transport during SO₂ co-injection with CO₂ in deep saline aquifers
dc.type Text
dc.type.genre Dissertation
dspace.entity.type Publication
local.contributor.corporatename School of Civil and Environmental Engineering
local.contributor.corporatename College of Engineering
relation.isOrgUnitOfPublication 88639fad-d3ae-4867-9e7a-7c9e6d2ecc7c
relation.isOrgUnitOfPublication 7c022d60-21d5-497c-b552-95e489a06569
thesis.degree.level Doctoral
Files
Original bundle
Now showing 1 - 3 of 3
Thumbnail Image
Name:
ZHANG-DISSERTATION-2013.pdf
Size:
1.32 MB
Format:
Adobe Portable Document Format
Description:
No Thumbnail Available
Name:
Thesis_from_Andi_Zhang_final_reformatted.doc
Size:
2.12 MB
Format:
Microsoft Word
Description:
No Thumbnail Available
Name:
Thesis_from_Andi_Zhang_final.doc
Size:
2.09 MB
Format:
Microsoft Word
Description:
License bundle
Now showing 1 - 1 of 1
No Thumbnail Available
Name:
LICENSE.txt
Size:
3.86 KB
Format:
Plain Text
Description: