ATTENTION: The software behind KU ScholarWorks is being upgraded to a new version. Starting July 15th, users will not be able to log in to the system, add items, nor make any changes until the new version is in place at the end of July. Searching for articles and opening files will continue to work while the system is being updated. If you have any questions, please contact Marianne Reed at mreed@ku.edu .

Show simple item record

dc.contributor.authorNie, Xin
dc.contributor.authorZhang, Chi
dc.contributor.authorWang, Chenchen
dc.contributor.authorNie, Shichang
dc.contributor.authorZhang, Jie
dc.contributor.authorZhang, Chaomo
dc.date.accessioned2021-02-23T21:55:06Z
dc.date.available2021-02-23T21:55:06Z
dc.date.issued2019
dc.identifier.citationNie, Xin, Zhang, Chi, Wang, Chenchen, Nie, Shichang, Zhang, Jie and Zhang, Chaomo. "Variable secondary porosity modeling of carbonate rocks based on μ-CT images" Open Geosciences, vol. 11, no. 1, 2019, pp. 617-626. https://doi.org/10.1515/geo-2019-0049en_US
dc.identifier.urihttp://hdl.handle.net/1808/31461
dc.description.abstractAs an essential carbonate reservoir parameter, porosity is closely related to rock properties. Digital rock physics (DRP) technology can help us to build forward models and find out the relationship between porosity and physical properties. In order to prepare models for the rock physical simulations of carbonate rocks, digital rock models with different porosities and fractures are needed. Based on a three-dimensional carbonate digital rock image obtained by X-ray microtomography (μ-CT), we used erosion and dilation in mathematical morphology to modify the pores, and fractional Brownian motion model (FBM) to create fractures with different width and angles. The pores become larger after the erosion operation and become smaller after the dilation operation. Therefore, a series of models with different porosities are obtained. From the analysis of the rock models, we found out that the erosion operation is similar to the corrosion process in carbonate rocks. The dilation operation can be used to restore the matrix of the late stages. In both processes, the pore numbers decrease because of the pore surface area decreases. The porosity-permeability relation of the models is a power exponential function similar to the experimental results. The structuring element B’s radius can affect the operation results. The FBM fracturing method has been proved reliable in sandstones, and because it is based on mathematics, the usage of it can also be workable in carbonate rocks. We can also use the processes and workflows introduced in this paper in carbonate digital rocks reconstructed in other ways. The models we built in this research lay the foundation of the next step physical simulations.en_US
dc.rights© 2019 X. Nie et al., published by De Gruyter. This work is licensed under a Creative Commons Attribution 4.0 International License.en_US
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_US
dc.subjectCarbonateen_US
dc.subjectDigital rock physicsen_US
dc.subjectSecondary porosityen_US
dc.subjectFractureen_US
dc.subjectMathematical morphologyen_US
dc.subjectFractional Brownian motionen_US
dc.titleVariable secondary porosity modeling of carbonate rocks based on μ-CT imagesen_US
dc.typeArticleen_US
kusw.kuauthorZhang, Chi
kusw.kudepartmentGeologyen_US
dc.identifier.doi10.1515/geo-2019-0049en_US
kusw.oaversionScholarly/refereed, publisher versionen_US
kusw.oapolicyThis item meets KU Open Access policy criteria.en_US
dc.rights.accessrightsopenAccessen_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

© 2019 X. Nie et al., published by De Gruyter. This work is licensed under a Creative Commons Attribution 4.0 International License.
Except where otherwise noted, this item's license is described as: © 2019 X. Nie et al., published by De Gruyter. This work is licensed under a Creative Commons Attribution 4.0 International License.