Jan Vanderborght
Jan Vanderborght
Agrosphere Institute, IBG-3, Forschungszentrum Jülich
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On the value of soil moisture measurements in vadose zone hydrology: A review
H Vereecken, JA Huisman, H Bogena, J Vanderborght, JA Vrugt, ...
Water resources research 44 (4), 2008
Modeling soil processes: Review, key challenges, and new perspectives
H Vereecken, A Schnepf, JW Hopmans, M Javaux, D Or, T Roose, ...
Vadose zone journal 15 (5), 2016
Imaging and characterisation of subsurface solute transport using electrical resistivity tomography (ERT) and equivalent transport models
A Kemna, J Vanderborght, B Kulessa, H Vereecken
Journal of hydrology 267 (3-4), 125-146, 2002
On the spatio-temporal dynamics of soil moisture at the field scale
H Vereecken, JA Huisman, Y Pachepsky, C Montzka, J Van Der Kruk, ...
Journal of Hydrology 516, 76-96, 2014
Use of a three-dimensional detailed modeling approach for predicting root water uptake
M Javaux, T Schröder, J Vanderborght, H Vereecken
Vadose Zone Journal 7 (3), 1079-1088, 2008
Review of dispersivities for transport modeling in soils
J Vanderborght, H Vereecken
Vadose Zone Journal 6 (1), 29-52, 2007
Pedotransfer functions in Earth system science: Challenges and perspectives
K Van Looy, J Bouma, M Herbst, J Koestel, B Minasny, U Mishra, ...
Reviews of Geophysics 55 (4), 1199-1256, 2017
Upscaling hydraulic properties and soil water flow processes in heterogeneous soils: A review
H Vereecken, R Kasteel, J Vanderborght, T Harter
Vadose Zone Journal 6 (1), 1-28, 2007
Nutrient acquisition from arable subsoils in temperate climates: a review
T Kautz, W Amelung, F Ewert, T Gaiser, R Horn, R Jahn, M Javaux, ...
Soil Biology and Biochemistry 57, 1003-1022, 2013
Proof of concept of regional scale hydrologic simulations at hydrologic resolution utilizing massively parallel computer resources
SJ Kollet, RM Maxwell, CS Woodward, S Smith, J Vanderborght, ...
Water resources research 46 (4), 2010
Explaining soil moisture variability as a function of mean soil moisture: A stochastic unsaturated flow perspective
H Vereecken, T Kamai, T Harter, R Kasteel, J Hopmans, J Vanderborght
Geophysical Research Letters 34 (22), 2007
A simple three-dimensional macroscopic root water uptake model based on the hydraulic architecture approach
V Couvreur, J Vanderborght, M Javaux
Hydrology and earth system sciences 16 (8), 2957-2971, 2012
Modelling water flow and solute transport in heterogeneous soils: A review of recent approaches
J Feyen, D Jacques, A Timmerman, J Vanderborght
Journal of Agricultural Engineering Research 70 (3), 231-256, 1998
Soil hydrology: Recent methodological advances, challenges, and perspectives
H Vereecken, JA Huisman, HJ Hendricks Franssen, N Brüggemann, ...
Water resources research 51 (4), 2616-2633, 2015
20 years of long-term atrazine monitoring in a shallow aquifer in western Germany
D Vonberg, J Vanderborght, N Cremer, T Pütz, M Herbst, H Vereecken
Water research 50, 294-306, 2014
Root water uptake: from three-dimensional biophysical processes to macroscopic modeling approaches
M Javaux, V Couvreur, J Vanderborght, H Vereecken
Vadose Zone Journal 12 (4), 2013
Comparison of three methods to calibrate TDR for monitoring solute movement in undisturbed soil
D Mallants, M Vanclooster, J Vanderborght, J Feyen, N Toride, ...
Soil Science Society of America Journal 60 (3), 747-754, 1996
Potential of electrical resistivity tomography to infer aquifer transport characteristics from tracer studies: A synthetic case study
J Vanderborght, A Kemna, H Hardelauf, H Vereecken
Water Resources Research 41 (6), 2005
Imaging and characterization of solute transport during two tracer tests in a shallow aquifer using electrical resistivity tomography and multilevel groundwater samplers
K Müller, J Vanderborght, A Englert, A Kemna, JA Huisman, J Rings, ...
Water Resources Research 46 (3), 2010
Monitoring solute transport in a multi‐layered sandy lysimeter using time domain reflectometry
M Vanclooster, D Mallants, J Vanderborght, J Diels, J Van Orshoven, ...
Soil Science Society of America Journal 59 (2), 337-344, 1995
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