Solute transport takes place in heterogeneous porous formations, with the log conductivity, Y = ln K, modeled as a stationary random space function of given univariate normal probability density function (pdf) with mean , variance sigma(2)(Y), and integral scale I-Y. For weak heterogeneity, the above mentioned quantities completely define the first-order approximation of the longitudinal macrodispersivity sigma(L) = sigma I-2(Y)Y. However, in highly heterogeneous formations, nonlinear effects which depend on the multipoint joint pdf of Y, impact alpha(L). Most of the past numerical simulations assumed a multivariate normal distribution (MVN) of Y values. The main aim of this study is to investigate the impact of deviations from the MVN stru...
The paper deals with non-Fickian dispersion of inert solutes in random permeability fields. Attentio...
A pulse of a passive tracer is injected in a porous medium via a point-like source. The hydraulic co...
Subsurface flow and transport settings are typically characterized by spatial variability of the und...
Solute transport takes place in heterogeneous porous formations, with the log conductivity, Y = ln K...
Solute transport takes place in heterogeneous porous formations, with the log-conductivity Y modell...
Heterogeneity of the hydraulic properties is one of the main causes of the seemingly random distribu...
This study presents numerical simulation of conservative solute transport in randomly heterogeneous...
We consider here the Lagrangian approach for stochastic modeling of the transport of inert solutes i...
Solute transport in natural formations at the regional scale is influenced by several scales of hete...
Solute transport in natural formations at the regional scale is influenced by several scales of hete...
A stochastic analysis of macrodispersion for conservative solute transport in three-dimension (3D) h...
We study the upscaling and prediction of large-scale solute dispersion in heterogeneous porous media...
The paper deals with the transport of nonreactive solute in heterogeneous formations with prescribed...
The concept of block-effective dispersivity represents the difference between the classic macrodispe...
The purpose of this research is twofold. First, a tool is developed to assist in the reproduction of...
The paper deals with non-Fickian dispersion of inert solutes in random permeability fields. Attentio...
A pulse of a passive tracer is injected in a porous medium via a point-like source. The hydraulic co...
Subsurface flow and transport settings are typically characterized by spatial variability of the und...
Solute transport takes place in heterogeneous porous formations, with the log conductivity, Y = ln K...
Solute transport takes place in heterogeneous porous formations, with the log-conductivity Y modell...
Heterogeneity of the hydraulic properties is one of the main causes of the seemingly random distribu...
This study presents numerical simulation of conservative solute transport in randomly heterogeneous...
We consider here the Lagrangian approach for stochastic modeling of the transport of inert solutes i...
Solute transport in natural formations at the regional scale is influenced by several scales of hete...
Solute transport in natural formations at the regional scale is influenced by several scales of hete...
A stochastic analysis of macrodispersion for conservative solute transport in three-dimension (3D) h...
We study the upscaling and prediction of large-scale solute dispersion in heterogeneous porous media...
The paper deals with the transport of nonreactive solute in heterogeneous formations with prescribed...
The concept of block-effective dispersivity represents the difference between the classic macrodispe...
The purpose of this research is twofold. First, a tool is developed to assist in the reproduction of...
The paper deals with non-Fickian dispersion of inert solutes in random permeability fields. Attentio...
A pulse of a passive tracer is injected in a porous medium via a point-like source. The hydraulic co...
Subsurface flow and transport settings are typically characterized by spatial variability of the und...