Heterogeneity is the single most salient feature of hydrogeology. An enormous amount of
work has been devoted during the last 30 years to addressing this issue. Our objective is to …

Geology is ubiquitously heterogeneous, exhibiting both discrete and continuous spatial
variations on a multiplicity of scales. It is therefore natural to expect that hydrogeologic and …

Numerical Monte Carlo simulation is considered to be one of the main tools to be used in
groundwater hydrology (1) to quantify the uncertainty in the flow predictions due to imperfect …

We consider heterogeneous media whose properties vary in space and particularly aquifers
whose hydraulic conductivity K may change by orders of magnitude in the same formation …

The conventional analysis of pumping tests by type‐curve methods is based on the
assumption of a homogeneous aquifer. Applying these techniques to pumping test data from …

Steady flow toward a fully penetrating well takes place in a natural porous formation, where
the erratic spatial variations, and the raising uncertainty, of the hydraulic conductivity K are …

The spatiotemporal patterns of injection‐induced seismicity (IIS) are commonly interpreted
with the concept of a triggering front, which propagates in a diffusion‐like manner with an …

Equations governing flow and transport in randomly heterogeneous porous media are
stochastic and scale dependent. In the moment equation (ME) method, exact deterministic …

Well‐type flow takes place in a heterogeneous porous formation where the transmissivity is
modeled as a stationary random space function (RSF). General expressions for the …

Tracer tests have been performed on a 3D tank of dimensions 560× 100× 100 cm3. These
experiments at laboratory scale are used to define effective hydraulic conductivity and …