Journal ArticleDOI
Analysis of solute transport in a heterogeneous aquifer: the Krauthausen field experiment
Harry Vereecken,U Döring,H. Hardelauf,Uwe Jaekel,Uwe Hashagen,O. Neuendorf,Holger Schwarze,R Seidemann +7 more
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TLDR
In this paper, a field-scale natural gradient tracer experiment with bromide, uranin and lithium was conducted in a heterogeneous aquifer at Krauthausen, Germany.About:
This article is published in Journal of Contaminant Hydrology.The article was published on 2000-10-01. It has received 95 citations till now. The article focuses on the topics: Aquifer & Hydraulic conductivity.read more
Citations
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Journal ArticleDOI
Imaging and characterisation of subsurface solute transport using electrical resistivity tomography (ERT) and equivalent transport models
TL;DR: In this article, the authors assess the usefulness of electrical resistivity tomography (ERT) in imaging and characterising subsurface solute transport in heterogeneous unconfined aquifers.
Journal ArticleDOI
Tracer tests for the investigation of heterogeneous porous media and stochastic modelling of flow and transport—a review of some recent developments
TL;DR: Tracer tests can be performed at laboratory and field-scales with depth integrated (two-dimensional) or multilevel (threedimensional) set-ups, and under natural or forced hydraulic gradient conditions.
Journal ArticleDOI
Two-dimensional characterization of hydraulic heterogeneity by multiple pumping tests
TL;DR: In this article, the authors compare the results obtained by geostatistical inverse modeling and type-curve analysis to pseudo-local values of transmissivity and storativity, which can be interpolated by kriging.
Journal ArticleDOI
Imaging and characterization of solute transport during two tracer tests in a shallow aquifer using electrical resistivity tomography and multilevel groundwater samplers
K Müller,K Müller,Jan Vanderborght,Andreas Englert,Andreas Englert,Andreas Kemna,Andreas Kemna,Johan Alexander Huisman,J. Rings,Harry Vereecken +9 more
TL;DR: In this article, the breakthroughs of an electrically conductive and a resistive tracer were monitored with ERT and local multilevel groundwater samplers (MLS) along two cross sections perpendicular to the mean flow direction.
Journal ArticleDOI
Hydraulic conductivity estimation from induced polarisation data at the field scale — the Krauthausen case history
TL;DR: In this paper, an IP survey at the Krauthausen hydrogeological test site in Germany was carried out and multifrequency data were recorded along two profiles with a dipole-dipole configuration and 2 m electrode spacing.
References
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Book
GSLIB: Geostatistical Software Library and User's Guide
TL;DR: In this paper, the authors present a set of programs that summarize data with histograms and other graphics, calculate measures of spatial continuity, provide smooth least-squares-type maps, and perform stochastic spatial simulation.
Book
Flow and Transport in Porous Formations
TL;DR: In this article, the authors presented a systematic and comprehensive approach to analyze the large scale heterogeneity of aquifers and its effect on the transport of contaminant in subsurface hydrology.
Journal ArticleDOI
Three‐dimensional stochastic analysis of macrodispersion in aquifers
Lynn W. Gelhar,Carl L. Axness +1 more
TL;DR: In this article, the dispersive mixing resulting from complex flow in three-dimensionalally heterogeneous porous media is analyzed using stochastic continuum theory, which is consistent with controlled field experiments and Monte Carlo simulations.
Book
Stochastic subsurface hydrology
TL;DR: Stohastic description temporally variable subsurface flow spatially variable sub-surface flow transport processes in heterogeneous media geostatistical methods and parameter estimation as mentioned in this paper, and
Journal ArticleDOI
A natural gradient experiment on solute transport in a sand aquifer: Spatial variability of hydraulic conductivity and its role in the dispersion process
TL;DR: The Borden aquifer was examined in great detail by conducting permeability measurements on a series of cores taken along two cross sections, one along and the other transverse to the mean flow direction as discussed by the authors.