scholarly journals Brine Transport Experiments in Granular Salt

2016 ◽  
Author(s):  
Amy B. Jordan ◽  
Hakim Boukhalfa ◽  
Florie Andre Caporuscio ◽  
Philip H. Stauffer
Keyword(s):  
Brine Transport

Multiphase CO2-brine Transport Properties of Synthetic Fault Gouge

2021 ◽  
pp. 105054
Author(s):  
Xiaojin Zheng ◽  
D. Nicolas Espinoza
Keyword(s):  
Transport Properties ◽  
Fault Gouge ◽  
Brine Transport

scholarly journals Brine transport in porous media: self-similar solutions

1998 ◽  
Vol 22 (3) ◽  
pp. 285-297 ◽  
Author(s):  
C.J van Duijn ◽  
L.A Peletier ◽  
R.J Schotting
Keyword(s):  
Porous Media ◽  
Transport In Porous Media ◽  
Brine Transport ◽  
Self Similar ◽  
Similar Solutions

Experimental and numerical study on supercritical CO2/brine transport in a fractured rock: Implications of mass transfer, capillary pressure and storage capacity

2013 ◽  
Vol 62 ◽  
pp. 442-453 ◽  
Author(s):  
Junho Oh ◽  
Kue-Young Kim ◽  
Weon Shik Han ◽  
Taehee Kim ◽  
Jeong-Chan Kim ◽  
...  
Keyword(s):  
Mass Transfer ◽  
Capillary Pressure ◽  
Supercritical Co2 ◽  
Storage Capacity ◽  
Numerical Study ◽  
Fractured Rock ◽  
Brine Transport ◽  
And Storage

On the modeling of brine transport in porous media

1988 ◽  
Vol 24 (3) ◽  
pp. 321-330 ◽  
Author(s):  
S. Majid Hassanizadeh ◽  
Toon Leijnse
Keyword(s):  
Porous Media ◽  
Transport In Porous Media ◽  
Brine Transport

Brine Transport in the Bedded Salt of the Waste Isolation Pilot Plant (wipp): Field Measurements and a Darcy Flow Model

1987 ◽  
Vol 112 ◽  
Author(s):  
David F. Mctigue ◽  
E. James Nowak
Keyword(s):  
Field Experiments ◽  
Flow Model ◽  
Radial Flow ◽  
Field Measurements ◽  
Darcy Flow ◽  
Waste Isolation Pilot Plant ◽  
One Dimensional ◽  
Brine Transport ◽  
Order Of Magnitude ◽  
Linearized Model

AbstractBrine flow has been measured to unheated boreholes for periods of a few days and to heated holes for two years in the WIPP facility. It is proposed that Darcy flow may dominate the observed influx of brine. Exact solutions to a linearized model for one-dimensional, radial flow are evaluated for conditions approximating the field experiments. Flow rates of the correct order of magnitude are calculated for permeabilities in the range 10−21–1020 m2 (1–10 nanodarcy) for both the unheated and heated cases.

Modeling Horizontal Salt Cavern Leaching in Bedded Salt Formations

SPE Journal ◽  
2022 ◽  
pp. 1-12
Author(s):  
Quanshu Zeng ◽  
Zhiming Wang ◽  
Jinchao Wang ◽  
Qiqi Wanyan ◽  
Guosheng Ding ◽  
...  
Keyword(s):  
Concentration Distribution ◽  
Coupled Model ◽  
Flow Region ◽  
Cavity Expansion ◽  
Injection Point ◽  
Salt Cavern ◽  
Transport Dynamics ◽  
Brine Transport ◽  
Relative Errors ◽  
And Diffusion

Summary The leaching of a salt cavern will trigger a series of rock-fluid interactions, including salt rock dissolution, cavity expansion, and brine transport caused by convection, turbulence, and diffusion effects. These interactions have influences on one another. The primary objectives of this study include developing a 3D multiphysical coupled model for horizontal salt cavern leaching and quantifying these interactions. The species transport equation and standard κ-ε equation were combined to describe the brine transport dynamics within the cavity. Based on the velocity and concentration distribution characteristics predicted, the interface movement equation implemented with mesh deformation techniques was applied to describe the cavity expansion. Next, the Volgograd cavern monitored data were collected for model validation. The predicted results are consistent with the field data. The average relative errors are 11.0% for brine displacing concentration and 4.5% for cavity volume. The results suggest that the cavity can be divided into three regions, including the main flow region, circulation region, and reflux region. The results also suggest that the brine concentration distribution is relatively uniform. With the dissolution threshold angle and anisotropic dissolution rates considered, the resultant cavity cross section is crown top and cone bottom. The results also show that the cavity can be divided into dissolution and erosion sections according to its position relative to the injection point.

Ground ice recharge via brine transport in frozen soils of Victoria Valley, Antarctica: Insights from modeling δ18O and δD profiles

2010 ◽  
Vol 74 (2) ◽  
pp. 435-448 ◽  
Author(s):  
Birgit Hagedorn ◽  
Ronald S. Sletten ◽  
Bernard Hallet ◽  
David F. McTigue ◽  
Eric J. Steig
Keyword(s):  
Ground Ice ◽  
Frozen Soils ◽  
Brine Transport ◽  
Δ18o And Δd
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