Trends, prospects and challenges in quantifying flow and transport through fractured rocks

SP Neuman - Hydrogeology Journal, 2005 - Springer
Among the current problems that hydrogeologists face, perhaps there is none as
challenging as the characterization of fractured rock (Faybishenko and Benson 2000). This …

Representative hydraulic conductivities in saturated groundwater flow

X Sanchez‐Vila, A Guadagnini… - Reviews of …, 2006 - Wiley Online Library
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 …

GSTools v1. 3: a toolbox for geostatistical modelling in Python

S Müller, L Schüler, A Zech… - Geoscientific Model …, 2022 - gmd.copernicus.org
Geostatistics as a subfield of statistics accounts for the spatial correlations encountered in
many applications of, for example, earth sciences. Valuable information can be extracted …

The fractional‐order governing equation of Lévy motion

DA Benson, SW Wheatcraft… - Water resources …, 2000 - Wiley Online Library
A governing equation of stable random walks is developed in one dimension. This Fokker‐
Planck equation is similar to, and contains as a subset, the second‐order advection …

[图书][B] Percolation theory for flow in porous media

A Hunt, R Ewing, B Ghanbarian - 2014 - books.google.com
This monograph presents, for the first time, a unified and comprehensive introduction to
some of the basic transport properties of porous media, such as electrical and hydraulic …

Stochastic methods for flow in porous media: coping with uncertainties

YK Zhang - 2006 - pubs.geoscienceworld.org
Hydrogeological variables of a groundwater system, for example, the hydraulic head and
contaminant concentration, vary with space and time. The variability is due to spatial …

Scaling issues in snow hydrology

G Blöschl - Hydrological processes, 1999 - Wiley Online Library
The concept of scale can be used to quantify characteristic lengths of (a) a natural process
(such as the correlation length of the spatial snow water equivalent (SWE) variability);(b) a …

A dual‐domain mass transfer approach for modeling solute transport in heterogeneous aquifers: Application to the Macrodispersion Experiment (MADE) site

CE Feehley, C Zheng, FJ Molz - Water Resources Research, 2000 - Wiley Online Library
A large‐scale natural‐gradient tracer test in a highly heterogeneous aquifer at the
Macrodispersion Experiment (MADE) site on the Columbus Air Force Base in Mississippi is …

Advances in the use of observed spatial patterns of catchment hydrological response

RB Grayson, G Blöschl, AW Western… - Advances in water …, 2002 - Elsevier
Over the past two decades there have been repeated calls for the collection of new data for
use in developing hydrological science. The last few years have begun to bear fruit from the …

Multifaceted nature of hydrogeologic scaling and its interpretation

SP Neuman, V Di Federico - Reviews of Geophysics, 2003 - Wiley Online Library
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 …