Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
An Analytical Algorithm of Porosity-Permeability for Porous and Fractured Media: Extension to Reactive Transport Conditions and Fitting via Flow-Through Experiments Within Limestone and Dolomite
Date
2019-08-01
Author
Erol, Selçuk
Fowler, Sarah Jane
Nehler, Mathias
De Boever, Eva
Harcouet-Menou, Virginie
Laenen, Ben
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
11
views
0
downloads
Cite This
Accurate prediction of permeability evolution is essential for forecasting the long-term performance and lifetime of hydrothermal reservoirs, an important goal in the geothermal, ore, and petroleum industries. Erol et al. (Transp Porous Media 120(2):327-358, 2017. 10.1007/s11242-017-0923-z) introduced a general (non-empirical) analytical Kozeny-Carman type equation for predicting matrix and fracture permeability during single-phase, non-reactive flow. Here we incorporate the equation into an algorithm for addressing the influence on porous and fractured media permeability of the transient reactive processes of mineral dissolution and precipitation. Analytical algorithm predictions are identical to permeability values measured during fluid circulation through limestone and dolomite core samples from the Campine Basin deep geothermal system in Belgium. Benchmarking used identical values for initial hydraulic aperture dimension and porosity, measured during fluid circulation based on nondestructive micro-CT imaging. Analytical algorithm predictions of reactive surface area and fracture porosity are similar to results based on the TOUGHREACT reactive transport code. TOUGHREACT implements several well-established power-law models for predicting permeability, notably Civan (AIChE J 47(2):1167-1197, 2001. 10.1002/aic.690470206) and Verma and Pruess (J Geophys Res Solid Earth 93:1159-1173, 1988. 10.1029/jb093ib02p01159). However, these models rely on specification of empirical exponents, which are not straightforward to measure. Our results suggest that a more general, computationally inexpensive analytical method can lead to accurate permeability calculation.
URI
https://hdl.handle.net/11511/116940
Journal
TRANSPORT IN POROUS MEDIA
DOI
https://doi.org/10.1007/s11242-019-01293-z
Collections
Department of Petroleum and Natural Gas Engineering, Article
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
S. Erol, S. J. Fowler, M. Nehler, E. De Boever, V. Harcouet-Menou, and B. Laenen, “An Analytical Algorithm of Porosity-Permeability for Porous and Fractured Media: Extension to Reactive Transport Conditions and Fitting via Flow-Through Experiments Within Limestone and Dolomite,”
TRANSPORT IN POROUS MEDIA
, vol. 129, no. 1, pp. 343–383, 2019, Accessed: 00, 2025. [Online]. Available: https://hdl.handle.net/11511/116940.