Uniform mean flow takes place in a 3-D heterogeneous formation of normal hydraulic logconductivity Y=lnK. The aim of the study is to derive the dependence of the horizontal Kefhand vertical Kefveffective conductivities on the structural parameters of hydraulic conductivity and investigate the impact of departure from multi-Gaussianity on Kef, by numerical simulations of flow in formations that share the same pdf and covariance of Y but differ in the connectivity of classes of Y. The main result is that for the extreme models of connected and disconnected high Y zones the ratio between the effective conductivities in isotropic media is much smaller than in 2-D. The dependence of Kefh and Kefvupon the logconductivity variance and the anisotro...
Aquifer hydraulic properties such as hydraulic conductivity (K) are ubiquitously heterogeneous and t...
At regional scale, it is common to model groundwater flow as 2-D in the x, y, horizontal plane, by i...
Solute transport takes place in heterogeneous porous formations, with the log conductivity, Y = ln K...
Uniform mean flow takes place in a 3-D heterogeneous formation of normal hydraulic logconductivity Y...
Water flow in partially saturated heterogeneous porous formations is modelled by regarding the hydra...
Abstract. We develop analytical expressions for the effective hydraulic conductivity Ke of a three-d...
Connectivity has been a target of investigation for subsurface hydrology for decades. We apply seven...
In large scale heterogeneous aquifer simulations, determining the appropriate coarsening scale λ to ...
"\"The paper deals with the effective conductivity tensor K(ef) of anisotropic random media subject ...
The equivalent hydraulic conductivity (Keq) relates the spatial averages of flux and head gradient i...
International audienceThe equivalent hydraulic conductivity () relates the spatial averages of flux ...
Natural gradient steady flow of mean velocity U takes place in heterogeneous aquifers of random logc...
The effect of a periodic spatial behaviour of the mean log-conductivity (logK) in random heterogeneo...
We explore the concept of effective hydraulic conductivity for a bounded randomly heterogeneous form...
The study, a continuation of that of Indelman et at. [1996], aims at deriving the second-order momen...
Aquifer hydraulic properties such as hydraulic conductivity (K) are ubiquitously heterogeneous and t...
At regional scale, it is common to model groundwater flow as 2-D in the x, y, horizontal plane, by i...
Solute transport takes place in heterogeneous porous formations, with the log conductivity, Y = ln K...
Uniform mean flow takes place in a 3-D heterogeneous formation of normal hydraulic logconductivity Y...
Water flow in partially saturated heterogeneous porous formations is modelled by regarding the hydra...
Abstract. We develop analytical expressions for the effective hydraulic conductivity Ke of a three-d...
Connectivity has been a target of investigation for subsurface hydrology for decades. We apply seven...
In large scale heterogeneous aquifer simulations, determining the appropriate coarsening scale λ to ...
"\"The paper deals with the effective conductivity tensor K(ef) of anisotropic random media subject ...
The equivalent hydraulic conductivity (Keq) relates the spatial averages of flux and head gradient i...
International audienceThe equivalent hydraulic conductivity () relates the spatial averages of flux ...
Natural gradient steady flow of mean velocity U takes place in heterogeneous aquifers of random logc...
The effect of a periodic spatial behaviour of the mean log-conductivity (logK) in random heterogeneo...
We explore the concept of effective hydraulic conductivity for a bounded randomly heterogeneous form...
The study, a continuation of that of Indelman et at. [1996], aims at deriving the second-order momen...
Aquifer hydraulic properties such as hydraulic conductivity (K) are ubiquitously heterogeneous and t...
At regional scale, it is common to model groundwater flow as 2-D in the x, y, horizontal plane, by i...
Solute transport takes place in heterogeneous porous formations, with the log conductivity, Y = ln K...