The mixing of two miscible fluids in motion in a saturated isotropic porous medium and the stability of the density interface between them has been studied. The density interface was formed by a line source introducing a denser fluid into a uniform confined horizontal flow. It was shown that the half-body thus formed may be approximated to within the density difference by the shape when the densities are equal. The mixing of the two fluids by lateral dispersion along such an interface was investigated experimentally and it was found that up to density differences of at least 1 per cent there was no observable effect on the lateral dispersion coefficient. A theoretical investigation has been made of the stability of the uniform two-dimens...
A vertically moving boundary in a stratified fluid can create and maintain a horizontal density grad...
A vertically moving boundary in a stratified fluid can create and maintain a horizontal density grad...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...
We investigate the stability of slowly smearing phase boundary that appears at the contact of two mi...
The stability of a mixing layer made up of two miscible fluids, with a viscosity-stratified layer be...
The stability of a mixing layer made up of two miscible fluids, with a viscosity-stratified layer be...
The combined effects of the double-diffusion and of the viscous dissipation on the convective instab...
The combined effects of the double-diffusion and of the viscous dissipation on the convective instab...
The combined effects of the double-diffusion and of the viscous dissipation on the convective instab...
A miscible horizontal interface separating two solutions of different solutes in the gravity field c...
Double-diffusive density stratified systems are well studied and have been shown to display a rich v...
This study investigates lateral mixing of tracer fluids in turbulent open-channel flows when the tra...
The pressure-driven miscible displacement of a less viscous fluid by a more viscous one in a horizon...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...
A vertically moving boundary in a stratified fluid can create and maintain a horizontal density grad...
A vertically moving boundary in a stratified fluid can create and maintain a horizontal density grad...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...
We investigate the stability of slowly smearing phase boundary that appears at the contact of two mi...
The stability of a mixing layer made up of two miscible fluids, with a viscosity-stratified layer be...
The stability of a mixing layer made up of two miscible fluids, with a viscosity-stratified layer be...
The combined effects of the double-diffusion and of the viscous dissipation on the convective instab...
The combined effects of the double-diffusion and of the viscous dissipation on the convective instab...
The combined effects of the double-diffusion and of the viscous dissipation on the convective instab...
A miscible horizontal interface separating two solutions of different solutes in the gravity field c...
Double-diffusive density stratified systems are well studied and have been shown to display a rich v...
This study investigates lateral mixing of tracer fluids in turbulent open-channel flows when the tra...
The pressure-driven miscible displacement of a less viscous fluid by a more viscous one in a horizon...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...
A vertically moving boundary in a stratified fluid can create and maintain a horizontal density grad...
A vertically moving boundary in a stratified fluid can create and maintain a horizontal density grad...
Flooding of coastal areas with seawater often leads to density stratification. The stability of the ...