- Articles & preprints
- Submission
- Policies
- Peer review
- Editorial board
- About
- EGU publications
- Manuscript tracking
Journal cover
Journal topic
Hydrology and Earth System Sciences
An interactive open-access journal of the European Geosciences Union
Journal topic
- Articles & preprints
- Submission
- Policies
- Peer review
- Editorial board
- About
- EGU publications
- Manuscript tracking
Journal metrics
IF5.153
IF 5-year
5.460
5.460
CiteScore
7.8
7.8
SNIP1.623
IPP4.91
SJR2.092
Scimago H
index123
index123
h5-index65
Abstracted/indexed
Abstracted/indexed
HESS | Articles | Volume 22, issue 4
Hydrol. Earth Syst. Sci., 22, 2449–2470, 2018
https://doi.org/10.5194/hess-22-2449-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-22-2449-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Hydrol. Earth Syst. Sci., 22, 2449–2470, 2018
https://doi.org/10.5194/hess-22-2449-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-22-2449-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Research article 23 Apr 2018
Research article | 23 Apr 2018
Root growth, water uptake, and sap flow of winter wheat in response to different soil water conditions
Gaochao Cai et al.
Related authors
No articles found.
Youri Rothfuss, Maria Quade, Nicolas Brüggemann, Alexander Graf, Harry Vereecken, and Maren Dubbert
Biogeosciences Discuss., https://doi.org/10.5194/bg-2020-414, https://doi.org/10.5194/bg-2020-414, 2020
Preprint under review for BG
Short summary
Short summary
The partitioning of evapotranspiration into evaporation from soil and transpiration from plants is crucial for a wide range of parties, from farmers to policy makers.
In this work, we focus on a particular partitioning method, based on the stable isotopic analysis of water. In particular, we aim at highlighting the challenges that this method is currently facing and, in light of recent methodological developments, propose ways forward for the isotopic partitioning community.
Thuy Huu Nguyen, Matthias Langensiepen, Jan Vanderborght, Hubert Hüging, Cho Miltin Mboh, and Frank Ewert
Hydrol. Earth Syst. Sci., 24, 4943–4969, https://doi.org/10.5194/hess-24-4943-2020, https://doi.org/10.5194/hess-24-4943-2020, 2020
Short summary
Short summary
The mechanistic Couvreur root water uptake (RWU) model that is based on plant hydraulics and links root system properties to RWU, water stress, and crop development can evaluate the impact of certain crop properties on crop performance in different environments and soils, while the Feddes RWU approach does not possess such flexibility. This study also shows the importance of modeling root development and how it responds to water deficiency to predict the impact of water stress on crop growth.
Jordi Vilà-Guerau de Arellano, Patrizia Ney, Oscar Hartogensis, Hugo de Boer, Kevin van Diepen, Dzhaner Emin, Geiske de Groot, Anne Klosterhalfen, Matthias Langensiepen, Maria Matveeva, Gabriela Miranda-García, Arnold F. Moene, Uwe Rascher, Thomas Röckmann, Getachew Adnew, Nicolas Brüggemann, Youri Rothfuss, and Alexander Graf
Biogeosciences, 17, 4375–4404, https://doi.org/10.5194/bg-17-4375-2020, https://doi.org/10.5194/bg-17-4375-2020, 2020
Short summary
Short summary
The CloudRoots field experiment has obtained an open comprehensive observational data set that includes soil, plant, and atmospheric variables to investigate the interactions between a heterogeneous land surface and its overlying atmospheric boundary layer, including the rapid perturbations of clouds in evapotranspiration. Our findings demonstrate that in order to understand and represent diurnal variability, we need to measure and model processes from the leaf to the landscape scales.
Theresa Boas, Heye Bogena, Thomas Grünwald, Bernard Heinesch, Dongryeol Ryu, Marius Schmidt, Harry Vereecken, Andrew Western, and Harrie-Jan Hendricks-Franssen
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2020-241, https://doi.org/10.5194/gmd-2020-241, 2020
Revised manuscript under review for GMD
Short summary
Short summary
In this study we were able to significantly improve the CLM5 model performance for European cropland sites by adding a winter wheat representation, specific plant parameters for important cash crops and a cover cropping subroutine to its crop module. We anticipate that our findings and modifications can help to improve regional scale yield predictions, and offer the possibility to study the effects of large-scale cover cropping on energy fluxes, CN pools and the terrestrial water cycle.
Bernd Schalge, Gabriele Baroni, Barbara Haese, Daniel Erdal, Gernot Geppert, Pablo Saavedra, Vincent Haefliger, Harry Vereecken, Sabine Attinger, Harald Kunstmann, Olaf A. Cirpka, Felix Ament, Stefan Kollet, Insa Neuweiler, Harrie-Jan Hendricks Franssen, and Clemens Simmer
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2020-24, https://doi.org/10.5194/essd-2020-24, 2020
Preprint under review for ESSD
Short summary
Short summary
In this study a nine year simulation of complete model output of a coupled atmosphere-land surface-subsurface model on the catchment scale is discussed. We used the Neckar catchment in SW-Germany as the basis of this simulation. Since the dataset includes the full model output it is not only possible to investigate model behaviour and interactions between the component models but also use it as a virtual truth for comparison of for example data assimilation experiments.
Jannis Groh, Jan Vanderborght, Thomas Pütz, Hans-Jörg Vogel, Ralf Gründling, Holger Rupp, Mehdi Rahmati, Michael Sommer, Harry Vereecken, and Horst H. Gerke
Hydrol. Earth Syst. Sci., 24, 1211–1225, https://doi.org/10.5194/hess-24-1211-2020, https://doi.org/10.5194/hess-24-1211-2020, 2020
Michael Paul Stockinger, Heye Reemt Bogena, Andreas Lücke, Christine Stumpp, and Harry Vereecken
Hydrol. Earth Syst. Sci., 23, 4333–4347, https://doi.org/10.5194/hess-23-4333-2019, https://doi.org/10.5194/hess-23-4333-2019, 2019
Short summary
Short summary
Precipitation moves through the soil to become stream water. The fraction of precipitation that becomes stream water after 3 months (Fyw) can be calculated with the stable isotopes of water. Previously, this was done for all the isotope data available, e.g., for several years. We used 1 year of data to calculate Fyw and moved this calculation time window over the time series. Results highlight that Fyw varies in time. Comparison studies of different regions should take this into account.
Anne Klosterhalfen, Alexander Graf, Nicolas Brüggemann, Clemens Drüe, Odilia Esser, María P. González-Dugo, Günther Heinemann, Cor M. J. Jacobs, Matthias Mauder, Arnold F. Moene, Patrizia Ney, Thomas Pütz, Corinna Rebmann, Mario Ramos Rodríguez, Todd M. Scanlon, Marius Schmidt, Rainer Steinbrecher, Christoph K. Thomas, Veronika Valler, Matthias J. Zeeman, and Harry Vereecken
Biogeosciences, 16, 1111–1132, https://doi.org/10.5194/bg-16-1111-2019, https://doi.org/10.5194/bg-16-1111-2019, 2019
Short summary
Short summary
To obtain magnitudes of flux components of H2O and CO2 (e.g., transpiration, soil respiration), we applied source partitioning approaches after Scanlon and Kustas (2010) and after Thomas et al. (2008) to high-frequency eddy covariance measurements of 12 study sites covering various ecosystems (croplands, grasslands, and forests) in different climatic regions. We analyzed the interrelations among turbulence, site characteristics, and the performance of both partitioning methods.
Nevil Quinn, Günter Blöschl, András Bárdossy, Attilio Castellarin, Martyn Clark, Christophe Cudennec, Demetris Koutsoyiannis, Upmanu Lall, Lubomir Lichner, Juraj Parajka, Christa D. Peters-Lidard, Graham Sander, Hubert Savenije, Keith Smettem, Harry Vereecken, Alberto Viglione, Patrick Willems, Andy Wood, Ross Woods, Chong-Yu Xu, and Erwin Zehe
Proc. IAHS, 380, 3–8, https://doi.org/10.5194/piahs-380-3-2018, https://doi.org/10.5194/piahs-380-3-2018, 2018
Nevil Quinn, Günter Blöschl, András Bárdossy, Attilio Castellarin, Martyn Clark, Christophe Cudennec, Demetris Koutsoyiannis, Upmanu Lall, Lubomir Lichner, Juraj Parajka, Christa D. Peters-Lidard, Graham Sander, Hubert Savenije, Keith Smettem, Harry Vereecken, Alberto Viglione, Patrick Willems, Andy Wood, Ross Woods, Chong-Yu Xu, and Erwin Zehe
Hydrol. Earth Syst. Sci., 22, 5735–5739, https://doi.org/10.5194/hess-22-5735-2018, https://doi.org/10.5194/hess-22-5735-2018, 2018
Mehdi Rahmati, Lutz Weihermüller, Jan Vanderborght, Yakov A. Pachepsky, Lili Mao, Seyed Hamidreza Sadeghi, Niloofar Moosavi, Hossein Kheirfam, Carsten Montzka, Kris Van Looy, Brigitta Toth, Zeinab Hazbavi, Wafa Al Yamani, Ammar A. Albalasmeh, Ma'in Z. Alghzawi, Rafael Angulo-Jaramillo, Antônio Celso Dantas Antonino, George Arampatzis, Robson André Armindo, Hossein Asadi, Yazidhi Bamutaze, Jordi Batlle-Aguilar, Béatrice Béchet, Fabian Becker, Günter Blöschl, Klaus Bohne, Isabelle Braud, Clara Castellano, Artemi Cerdà, Maha Chalhoub, Rogerio Cichota, Milena Císlerová, Brent Clothier, Yves Coquet, Wim Cornelis, Corrado Corradini, Artur Paiva Coutinho, Muriel Bastista de Oliveira, José Ronaldo de Macedo, Matheus Fonseca Durães, Hojat Emami, Iraj Eskandari, Asghar Farajnia, Alessia Flammini, Nándor Fodor, Mamoun Gharaibeh, Mohamad Hossein Ghavimipanah, Teamrat A. Ghezzehei, Simone Giertz, Evangelos G. Hatzigiannakis, Rainer Horn, Juan José Jiménez, Diederik Jacques, Saskia Deborah Keesstra, Hamid Kelishadi, Mahboobeh Kiani-Harchegani, Mehdi Kouselou, Madan Kumar Jha, Laurent Lassabatere, Xiaoyan Li, Mark A. Liebig, Lubomír Lichner, María Victoria López, Deepesh Machiwal, Dirk Mallants, Micael Stolben Mallmann, Jean Dalmo de Oliveira Marques, Miles R. Marshall, Jan Mertens, Félicien Meunier, Mohammad Hossein Mohammadi, Binayak P. Mohanty, Mansonia Pulido-Moncada, Suzana Montenegro, Renato Morbidelli, David Moret-Fernández, Ali Akbar Moosavi, Mohammad Reza Mosaddeghi, Seyed Bahman Mousavi, Hasan Mozaffari, Kamal Nabiollahi, Mohammad Reza Neyshabouri, Marta Vasconcelos Ottoni, Theophilo Benedicto Ottoni Filho, Mohammad Reza Pahlavan-Rad, Andreas Panagopoulos, Stephan Peth, Pierre-Emmanuel Peyneau, Tommaso Picciafuoco, Jean Poesen, Manuel Pulido, Dalvan José Reinert, Sabine Reinsch, Meisam Rezaei, Francis Parry Roberts, David Robinson, Jesús Rodrigo-Comino, Otto Corrêa Rotunno Filho, Tadaomi Saito, Hideki Suganuma, Carla Saltalippi, Renáta Sándor, Brigitta Schütt, Manuel Seeger, Nasrollah Sepehrnia, Ehsan Sharifi Moghaddam, Manoj Shukla, Shiraki Shutaro, Ricardo Sorando, Ajayi Asishana Stanley, Peter Strauss, Zhongbo Su, Ruhollah Taghizadeh-Mehrjardi, Encarnación Taguas, Wenceslau Geraldes Teixeira, Ali Reza Vaezi, Mehdi Vafakhah, Tomas Vogel, Iris Vogeler, Jana Votrubova, Steffen Werner, Thierry Winarski, Deniz Yilmaz, Michael H. Young, Steffen Zacharias, Yijian Zeng, Ying Zhao, Hong Zhao, and Harry Vereecken
Earth Syst. Sci. Data, 10, 1237–1263, https://doi.org/10.5194/essd-10-1237-2018, https://doi.org/10.5194/essd-10-1237-2018, 2018
Short summary
Short summary
This paper presents and analyzes a global database of soil infiltration data, the SWIG database, for the first time. In total, 5023 infiltration curves were collected across all continents in the SWIG database. These data were either provided and quality checked by the scientists or they were digitized from published articles. We are convinced that the SWIG database will allow for a better parameterization of the infiltration process in land surface models and for testing infiltration models.
Roland Baatz, Pamela L. Sullivan, Li Li, Samantha R. Weintraub, Henry W. Loescher, Michael Mirtl, Peter M. Groffman, Diana H. Wall, Michael Young, Tim White, Hang Wen, Steffen Zacharias, Ingolf Kühn, Jianwu Tang, Jérôme Gaillardet, Isabelle Braud, Alejandro N. Flores, Praveen Kumar, Henry Lin, Teamrat Ghezzehei, Julia Jones, Henry L. Gholz, Harry Vereecken, and Kris Van Looy
Earth Syst. Dynam., 9, 593–609, https://doi.org/10.5194/esd-9-593-2018, https://doi.org/10.5194/esd-9-593-2018, 2018
Short summary
Short summary
Focusing on the usage of integrated models and in situ Earth observatory networks, three challenges are identified to advance understanding of ESD, in particular to strengthen links between biotic and abiotic, and above- and below-ground processes. We propose developing a model platform for interdisciplinary usage, to formalize current network infrastructure based on complementarities and operational synergies, and to extend the reanalysis concept to the ecosystem and critical zone.
Hanna Post, Harrie-Jan Hendricks Franssen, Xujun Han, Roland Baatz, Carsten Montzka, Marius Schmidt, and Harry Vereecken
Biogeosciences, 15, 187–208, https://doi.org/10.5194/bg-15-187-2018, https://doi.org/10.5194/bg-15-187-2018, 2018
Short summary
Short summary
Estimated values of selected key CLM4.5-BGC parameters obtained with the Markov chain Monte Carlo (MCMC) approach DREAM(zs) strongly altered catchment-scale NEE predictions in comparison to global default parameter values. The effect of perturbed meteorological input data on the uncertainty of the predicted carbon fluxes was notably higher for C3-grass and C3-crop than for coniferous and deciduous forest. A future distinction of different crop types including management is considered essential.
Félicien Meunier, Valentin Couvreur, Xavier Draye, Mohsen Zarebanadkouki, Jan Vanderborght, and Mathieu Javaux
Hydrol. Earth Syst. Sci., 21, 6519–6540, https://doi.org/10.5194/hess-21-6519-2017, https://doi.org/10.5194/hess-21-6519-2017, 2017
Short summary
Short summary
To maintain its yield, a plant needs to transpire water that it acquires from the soil. A deep understanding of the mechanisms that lead to water uptake location and intensity is required to correctly simulate the water transfer in the soil to the atmosphere. This work presents novel and general solutions of the water flow equation in roots with varying hydraulic properties that deeply affect the uptake pattern and the transpiration rate and can be used in ecohydrological models.
Hongjuan Zhang, Harrie-Jan Hendricks Franssen, Xujun Han, Jasper A. Vrugt, and Harry Vereecken
Hydrol. Earth Syst. Sci., 21, 4927–4958, https://doi.org/10.5194/hess-21-4927-2017, https://doi.org/10.5194/hess-21-4927-2017, 2017
Short summary
Short summary
Applications of data assimilation (DA) arise in many fields of geosciences, perhaps most importantly in weather forecasting and hydrology. We want to investigate the roles of data assimilation methods and land surface models (LSMs) in joint estimation of states and parameters in the assimilation experiments. We find that all DA methods can improve prediction of states, and that differences between DA methods were limited but that the differences between LSMs were much larger.
Carsten Montzka, Michael Herbst, Lutz Weihermüller, Anne Verhoef, and Harry Vereecken
Earth Syst. Sci. Data, 9, 529–543, https://doi.org/10.5194/essd-9-529-2017, https://doi.org/10.5194/essd-9-529-2017, 2017
Short summary
Short summary
Global climate models require adequate parameterization of soil hydraulic properties, but typical resampling to the model grid introduces uncertainties. Here we present a method to scale hydraulic parameters to individual model grids and provide a global data set that overcomes the problems. It preserves the information of sub-grid variability of the water retention curve by deriving local scaling parameters that enables modellers to perturb hydraulic parameters for model ensemble generation.
Roland Baatz, Harrie-Jan Hendricks Franssen, Xujun Han, Tim Hoar, Heye Reemt Bogena, and Harry Vereecken
Hydrol. Earth Syst. Sci., 21, 2509–2530, https://doi.org/10.5194/hess-21-2509-2017, https://doi.org/10.5194/hess-21-2509-2017, 2017
Short summary
Short summary
Soil moisture is a major variable that affects regional climate, weather and hydrologic processes on the Earth's surface. In this study, real-world data of a network of cosmic-ray sensors were assimilated into a regional land surface model to improve model states and soil hydraulic parameters. The results show the potential of these networks for improving model states and parameters. It is suggested to widen the number of observed variables and to increase the number of estimated parameters.
Xiaoqian Jiang, Roland Bol, Barbara J. Cade-Menun, Volker Nischwitz, Sabine Willbold, Sara L. Bauke, Harry Vereecken, Wulf Amelung, and Erwin Klumpp
Biogeosciences, 14, 1153–1164, https://doi.org/10.5194/bg-14-1153-2017, https://doi.org/10.5194/bg-14-1153-2017, 2017
Short summary
Short summary
It is the first study to distinguish the species of nano-sized (d=1−20 nm), small-sized (d=20−450 nm) colloidal P, and dissolved P (d<1 nm) of hydromorphic surface grassland soils from Cambisol, Stagnic Cambisol to Stagnosol using FFF and 31P-NMR. Evidence of nano-sized associations of OC–Fe(Al)–PO43/pyrophosphate in Stagnosol. Stagnic properties affect P speciation and availability by releasing dissolved inorganic and ester-bound P forms as well as nano-sized organic matter–Fe/Al–P colloids.
Bernd Schalge, Jehan Rihani, Gabriele Baroni, Daniel Erdal, Gernot Geppert, Vincent Haefliger, Barbara Haese, Pablo Saavedra, Insa Neuweiler, Harrie-Jan Hendricks Franssen, Felix Ament, Sabine Attinger, Olaf A. Cirpka, Stefan Kollet, Harald Kunstmann, Harry Vereecken, and Clemens Simmer
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2016-557, https://doi.org/10.5194/hess-2016-557, 2016
Manuscript not accepted for further review
Short summary
Short summary
In this work we show how we used a coupled atmosphere-land surface-subsurface model at highest possible resolution to create a testbed for data assimilation. The model was able to capture all important processes and interactions between the compartments as well as showing realistic statistical behavior. This proves that using a model as a virtual truth is possible and it will enable us to develop data assimilation methods where states and parameters are updated across compartment.
Wei Qu, Heye R. Bogena, Johan A. Huisman, Marius Schmidt, Ralf Kunkel, Ansgar Weuthen, Henning Schiedung, Bernd Schilling, Jürgen Sorg, and Harry Vereecken
Earth Syst. Sci. Data, 8, 517–529, https://doi.org/10.5194/essd-8-517-2016, https://doi.org/10.5194/essd-8-517-2016, 2016
Short summary
Short summary
The Rollesbroich catchment is a hydrological observatory of the TERENO (Terrestrial Environmental Observatories) initiative. Hydrometeorological data and spatiotemporal variations in soil water content are measured at high temporal resolution and can be used for many purposes, e.g. validation of remote sensing retrievals, improving hydrological understanding, optimizing data assimilation and inverse modelling techniques. The data set is freely available online (http://www.tereno.net).
Wolfgang Kurtz, Guowei He, Stefan J. Kollet, Reed M. Maxwell, Harry Vereecken, and Harrie-Jan Hendricks Franssen
Geosci. Model Dev., 9, 1341–1360, https://doi.org/10.5194/gmd-9-1341-2016, https://doi.org/10.5194/gmd-9-1341-2016, 2016
Short summary
Short summary
This paper describes the development of a modular data assimilation (DA) system for the integrated Earth system model TerrSysMP with the help of the PDAF data assimilation library.
Currently, pressure and soil moisture data can be used to update model states and parameters in the subsurface compartment of TerrSysMP.
Results from an idealized twin experiment show that the developed DA system provides a good parallel performance and is also applicable for high-resolution modelling problems.
X. Jiang, R. Bol, S. Willbold, H. Vereecken, and E. Klumpp
Biogeosciences, 12, 6443–6452, https://doi.org/10.5194/bg-12-6443-2015, https://doi.org/10.5194/bg-12-6443-2015, 2015
Short summary
Short summary
Overall P content increased with decreasing size of soil aggregate-sized fractions. The relative distribution and speciation of varying P forms were independent of particle size. The majority of alkaline extractable P was in the amorphous Fe/Al oxide fraction, most of which was orthophosphate. Significant amounts of monoester P were also bound to these oxides. Residual P contained similar amounts of P occluded in amorphous and crystalline Fe oxides. This P may be released by FeO dissolution.
Y. Rothfuss, S. Merz, J. Vanderborght, N. Hermes, A. Weuthen, A. Pohlmeier, H. Vereecken, and N. Brüggemann
Hydrol. Earth Syst. Sci., 19, 4067–4080, https://doi.org/10.5194/hess-19-4067-2015, https://doi.org/10.5194/hess-19-4067-2015, 2015
Short summary
Short summary
Profiles of soil water stable isotopes were followed non-destructively and with high precision for a period of 290 days in the laboratory
Rewatering at the end of the experiment led to instantaneous resetting of the isotope profiles, which could be closely followed with the new method
The evaporation depth dynamics was determined from isotope gradients calculation
Uncertainty associated with the determination of isotope kinetic fractionation where highlighted from inverse modeling.
X. Han, X. Li, G. He, P. Kumbhar, C. Montzka, S. Kollet, T. Miyoshi, R. Rosolem, Y. Zhang, H. Vereecken, and H.-J. H. Franssen
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmdd-8-7395-2015, https://doi.org/10.5194/gmdd-8-7395-2015, 2015
Revised manuscript not accepted
Short summary
Short summary
DasPy is a ready to use open source parallel multivariate land data assimilation framework with joint state and parameter estimation using Local Ensemble Transform Kalman Filter. The Community Land Model (4.5) was integrated as model operator. The Community Microwave Emission Modelling platform, COsmic-ray Soil Moisture Interaction Code and the Two-Source Formulation were integrated as observation operators for the multivariate assimilation of soil moisture and soil temperature, respectively.
S. Gebler, H.-J. Hendricks Franssen, T. Pütz, H. Post, M. Schmidt, and H. Vereecken
Hydrol. Earth Syst. Sci., 19, 2145–2161, https://doi.org/10.5194/hess-19-2145-2015, https://doi.org/10.5194/hess-19-2145-2015, 2015
H. Post, H. J. Hendricks Franssen, A. Graf, M. Schmidt, and H. Vereecken
Biogeosciences, 12, 1205–1221, https://doi.org/10.5194/bg-12-1205-2015, https://doi.org/10.5194/bg-12-1205-2015, 2015
Short summary
Short summary
This study introduces an extension of the classical two-tower approach for uncertainty estimation of measured net CO2 fluxes (NEE). Because land surface properties cannot be assumed identical at two eddy covariance towers, a correction for systematic flux differences is proposed to be added to the classical weather filter. With this extension, the overestimation of NEE uncertainty due to systematic flux differences (which are assumed to increase with tower distance) can considerably be reduced.
B. Scharnagl, S. C. Iden, W. Durner, H. Vereecken, and M. Herbst
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hessd-12-2155-2015, https://doi.org/10.5194/hessd-12-2155-2015, 2015
Preprint withdrawn
X. Han, H.-J. H. Franssen, R. Rosolem, R. Jin, X. Li, and H. Vereecken
Hydrol. Earth Syst. Sci., 19, 615–629, https://doi.org/10.5194/hess-19-615-2015, https://doi.org/10.5194/hess-19-615-2015, 2015
Short summary
Short summary
This paper presents the joint assimilation of cosmic-ray neutron counts and land surface temperature with parameter estimation of leaf area index at an irrigated corn field. The results show that the data assimilation can reduce the systematic input errors due to the lack of irrigation data. The estimations of soil moisture, evapotranspiration and leaf area index can be improved in the joint assimilation framework.
V. Couvreur, J. Vanderborght, L. Beff, and M. Javaux
Hydrol. Earth Syst. Sci., 18, 1723–1743, https://doi.org/10.5194/hess-18-1723-2014, https://doi.org/10.5194/hess-18-1723-2014, 2014
W. Kurtz, H.-J. Hendricks Franssen, P. Brunner, and H. Vereecken
Hydrol. Earth Syst. Sci., 17, 3795–3813, https://doi.org/10.5194/hess-17-3795-2013, https://doi.org/10.5194/hess-17-3795-2013, 2013
V. R. N. Pauwels, G. J. M. De Lannoy, H.-J. Hendricks Franssen, and H. Vereecken
Hydrol. Earth Syst. Sci., 17, 3499–3521, https://doi.org/10.5194/hess-17-3499-2013, https://doi.org/10.5194/hess-17-3499-2013, 2013
Related subject area
Subject: Vadose Zone Hydrology | Techniques and Approaches: Modelling approaches
Comparison of root water uptake models in simulating CO2 and H2O fluxes and growth of wheat
Understanding the mass, momentum, and energy transfer in the frozen soil with three levels of model complexities
A field-validated surrogate crop model for predicting root-zone moisture and salt content in regions with shallow groundwater
Characterizing uncertainty in the hydraulic parameters of oil sands mine reclamation covers and its influence on water balance predictions
Simulating preferential soil water flow and tracer transport using the Lagrangian Soil Water and Solute Transport Model
Assessment of simulated soil moisture from WRF Noah, Noah-MP, and CLM land surface schemes for landslide hazard application
Efficient estimation of effective hydraulic properties of stratal undulating surface layer using time-lapse multi-channel GPR
Partitioning snowmelt and rainfall in the critical zone: effects of climate type and soil properties
A unique vadose zone model for shallow aquifers: the Hetao irrigation district, China
Modelling of shallow water table dynamics using conceptual and physically based integrated surface-water–groundwater hydrologic models
Capturing soil-water and groundwater interactions with an iterative feedback coupling scheme: new HYDRUS package for MODFLOW
Caffeine vs. carbamazepine as indicators of wastewater pollution in a karst aquifer
Predicting the soil water retention curve from the particle size distribution based on a pore space geometry containing slit-shaped spaces
Technical note: Saturated hydraulic conductivity and textural heterogeneity of soils
Water ages in the critical zone of long-term experimental sites in northern latitudes
Ecohydrological particle model based on representative domains
Impact of capillary rise and recirculation on simulated crop yields
Soil hydraulic material properties and layered architecture from time-lapse GPR
Using lagged dependence to identify (de)coupled surface and subsurface soil moisture values
Shallow water table effects on water, sediment, and pesticide transport in vegetative filter strips – Part 1: nonuniform infiltration and soil water redistribution
Shallow water table effects on water, sediment, and pesticide transport in vegetative filter strips – Part 2: model coupling, application, factor importance, and uncertainty
A pore-size classification for peat bogs derived from unsaturated hydraulic properties
Monitoring and modeling infiltration–recharge dynamics of managed aquifer recharge with desalinated seawater
Effect of unrepresented model errors on estimated soil hydraulic material properties
Saturated hydraulic conductivity model computed from bimodal water retention curves for a range of New Zealand soils
Ross scheme, Newton–Raphson iterative methods and time-stepping strategies for solving the mixed form of Richards' equation
Feasibility analysis of using inverse modeling for estimating field-scale evapotranspiration in maize and soybean fields from soil water content monitoring networks
A case study of field-scale maize irrigation patterns in western Nebraska: implications for water managers and recommendations for hyper-resolution land surface modeling
Benchmarking test of empirical root water uptake models
iCRESTRIGRS: a coupled modeling system for cascading flood–landslide disaster forecasting
EnKF with closed-eye period – towards a consistent aggregation of information in soil hydrology
Prediction of biopore- and matrix-dominated flow from X-ray CT-derived macropore network characteristics
A Lagrangian model for soil water dynamics during rainfall-driven conditions
Quantifying shallow subsurface water and heat dynamics using coupled hydrological-thermal-geophysical inversion
Stem–root flow effect on soil–atmosphere interactions and uncertainty assessments
The effect of different evapotranspiration methods on portraying soil water dynamics and ET partitioning in a semi-arid environment in Northwest China
Sensitivity of water stress in a two-layered sandy grassland soil to variations in groundwater depth and soil hydraulic parameters
Understanding NMR relaxometry of partially water-saturated rocks
Estimating flow and transport parameters in the unsaturated zone with pore water stable isotopes
Estimation of temporal and spatial variations in groundwater recharge in unconfined sand aquifers using Scots pine inventories
Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor
Characterizing coarse-resolution watershed soil moisture heterogeneity using fine-scale simulations
Assimilation of surface soil moisture into a multilayer soil model: design and evaluation at local scale
Estimating root zone soil moisture using near-surface observations from SMOS
Influence of soil, land use and climatic factors on the hydraulic conductivity of soil
Improving soil moisture profile reconstruction from ground-penetrating radar data: a maximum likelihood ensemble filter approach
Spatial distribution of solute leaching with snowmelt and irrigation: measurements and simulations
Linking soil moisture balance and source-responsive models to estimate diffuse and preferential components of groundwater recharge
Sensitivity of groundwater recharge using climatic analogues and HYDRUS-1D
A new approach to model the spatial and temporal variability of recharge to karst aquifers
Thuy Huu Nguyen, Matthias Langensiepen, Jan Vanderborght, Hubert Hüging, Cho Miltin Mboh, and Frank Ewert
Hydrol. Earth Syst. Sci., 24, 4943–4969, https://doi.org/10.5194/hess-24-4943-2020, https://doi.org/10.5194/hess-24-4943-2020, 2020
Short summary
Short summary
The mechanistic Couvreur root water uptake (RWU) model that is based on plant hydraulics and links root system properties to RWU, water stress, and crop development can evaluate the impact of certain crop properties on crop performance in different environments and soils, while the Feddes RWU approach does not possess such flexibility. This study also shows the importance of modeling root development and how it responds to water deficiency to predict the impact of water stress on crop growth.
Lianyu Yu, Yijian Zeng, and Zhongbo Su
Hydrol. Earth Syst. Sci., 24, 4813–4830, https://doi.org/10.5194/hess-24-4813-2020, https://doi.org/10.5194/hess-24-4813-2020, 2020
Short summary
Short summary
Soil mass and heat transfer processes were represented in three levels of model complexities to understand soil freeze–thaw mechanisms. Results indicate that coupled mass and heat transfer models considerably improved simulations of the soil hydrothermal regime. Vapor flow and thermal effects on water flow are the main mechanisms for the improvements. Given the explicit consideration of airflow, vapor flow and its effects on heat transfer were enhanced during the freeze–thaw transition period.
Zhongyi Liu, Zailin Huo, Chaozi Wang, Limin Zhang, Xianghao Wang, Guanhua Huang, Xu Xu, and Tammo Siert Steenhuis
Hydrol. Earth Syst. Sci., 24, 4213–4237, https://doi.org/10.5194/hess-24-4213-2020, https://doi.org/10.5194/hess-24-4213-2020, 2020
Short summary
Short summary
We have developed an integrated surrogate model for arid irrigated areas with shallow groundwater that links crop growth with soil water and salinity in the vadose zone. The model recognizes that field capacity is reached when the matric potential is equal to the height above the groundwater table. The model applies areas with shallow groundwater for which only very few surrogate models are available for most surface irrigation systems in the world without suffering from high groundwater.
M. Shahabul Alam, S. Lee Barbour, and Mingbin Huang
Hydrol. Earth Syst. Sci., 24, 735–759, https://doi.org/10.5194/hess-24-735-2020, https://doi.org/10.5194/hess-24-735-2020, 2020
Short summary
Short summary
This study quantifies uncertainties in the prediction of long-term water balance for mine reclamation soil covers using random sampling of model parameter distributions. Parameter distributions were obtained from model optimization for field monitoring data. Variability in climate is a greater source of uncertainty than the model parameters in evaporation predictions, while climate variability and model parameters exert similar uncertainty on predictions of net percolation.
Alexander Sternagel, Ralf Loritz, Wolfgang Wilcke, and Erwin Zehe
Hydrol. Earth Syst. Sci., 23, 4249–4267, https://doi.org/10.5194/hess-23-4249-2019, https://doi.org/10.5194/hess-23-4249-2019, 2019
Short summary
Short summary
We present our hydrological LAST-Model to simulate preferential soil water flow and tracer transport in macroporous soils. It relies on a Lagrangian perspective of the movement of discrete water particles carrying tracer masses through the subsoil and is hence an alternative approach to common models. Sensitivity analyses reveal the physical validity of the model concept and evaluation tests show that LAST can depict well observed tracer mass profiles with fingerprints of preferential flow.
Lu Zhuo, Qiang Dai, Dawei Han, Ningsheng Chen, and Binru Zhao
Hydrol. Earth Syst. Sci., 23, 4199–4218, https://doi.org/10.5194/hess-23-4199-2019, https://doi.org/10.5194/hess-23-4199-2019, 2019
Short summary
Short summary
This study assesses the usability of WRF model-simulated soil moisture for landslide monitoring in northern Italy. In particular, three advanced land surface model schemes (Noah, Noah-MP, and CLM4) are used to provide multi-layer soil moisture data. The results have shown Noah-MP can provide the best landslide monitoring performance. It is also demonstrated that a single soil moisture sensor located in plain area has a high correlation with a significant proportion of the study area.
Xicai Pan, Stefan Jaumann, Jiabao Zhang, and Kurt Roth
Hydrol. Earth Syst. Sci., 23, 3653–3663, https://doi.org/10.5194/hess-23-3653-2019, https://doi.org/10.5194/hess-23-3653-2019, 2019
Short summary
Short summary
This study suggests an efficient approach to obtain plot-scale soil hydraulic properties for the shallow structural soils via non-invasive ground-penetrating radar measurements. Facilitated by spatial information of lateral water flow, this approach is more efficient than the widely used inversion approaches relying on intensive soil moisture monitoring. The acquisition of such quantitative information is of great interest to fields such as hydrology and precision agriculture.
John C. Hammond, Adrian A. Harpold, Sydney Weiss, and Stephanie K. Kampf
Hydrol. Earth Syst. Sci., 23, 3553–3570, https://doi.org/10.5194/hess-23-3553-2019, https://doi.org/10.5194/hess-23-3553-2019, 2019
Short summary
Short summary
Streamflow in high-elevation and high-latitude areas may be vulnerable to snow loss, making it important to quantify how snowmelt and rainfall are divided between soil storage, drainage below plant roots, evapotranspiration and runoff. We examine this separation in different climates and soils using a physically based model. Results show runoff may be reduced with snowpack decline in all climates. The mechanisms responsible help explain recent observations of streamflow sensitivity to snow loss.
Zhongyi Liu, Xingwang Wang, Zailin Huo, and Tammo Siert Steenhuis
Hydrol. Earth Syst. Sci., 23, 3097–3115, https://doi.org/10.5194/hess-23-3097-2019, https://doi.org/10.5194/hess-23-3097-2019, 2019
Short summary
Short summary
A novel approach is taken in simulating the hydrology of the vadose zone in areas with shallow groundwater. The model recognizes that field capacity is reached when the matric potential is equal to the height above the groundwater table. The model can be used in areas with shallow groundwater to optimize irrigation water use and minimize tailwater losses.
Mohammad Bizhanimanzar, Robert Leconte, and Mathieu Nuth
Hydrol. Earth Syst. Sci., 23, 2245–2260, https://doi.org/10.5194/hess-23-2245-2019, https://doi.org/10.5194/hess-23-2245-2019, 2019
Short summary
Short summary
Modelling of shallow water table fluctuations is usually carried out using physically based numerical models. These models have notable limitations regarding intensive required data and computational burden. This paper presents an alternative modelling approach for modelling of such cases by introducing modifications to the calculation of groundwater recharge and saturated flow of a conceptual hydrologic model.
Jicai Zeng, Jinzhong Yang, Yuanyuan Zha, and Liangsheng Shi
Hydrol. Earth Syst. Sci., 23, 637–655, https://doi.org/10.5194/hess-23-637-2019, https://doi.org/10.5194/hess-23-637-2019, 2019
Short summary
Short summary
Accurately capturing the soil-water–groundwater interaction is vital for all disciplines related to subsurface flow but is difficult when undergoing significant nonlinearity in the modeling system. A new soil-water flow package is developed to solve the switching-form Richards’ equation. A multi-scale water balance analysis joins unsaturated–saturated models at separated scales. The whole system is solved efficiently with an iterative feedback coupling scheme.
Noam Zach Dvory, Yakov Livshitz, Michael Kuznetsov, Eilon Adar, Guy Gasser, Irena Pankratov, Ovadia Lev, and Alexander Yakirevich
Hydrol. Earth Syst. Sci., 22, 6371–6381, https://doi.org/10.5194/hess-22-6371-2018, https://doi.org/10.5194/hess-22-6371-2018, 2018
Short summary
Short summary
This research is paramount given the significance of karst aquifers as essential drinking water sources. While CBZ is considered conservative, CAF is subject to sorption and degradation, and therefore each of these two pollutants can be considered effective tracers for specific assessment of aquifer contamination. The model presented in this paper shows how each of the mentioned contaminants could serve as a better tool for aquifer contamination characterization and its treatment.
Chen-Chao Chang and Dong-Hui Cheng
Hydrol. Earth Syst. Sci., 22, 4621–4632, https://doi.org/10.5194/hess-22-4621-2018, https://doi.org/10.5194/hess-22-4621-2018, 2018
Short summary
Short summary
The soil water retention curve (SWRC) is fundamental to researching water flow and chemical transport in unsaturated media. However, the traditional prediction models underestimate the water content in the dry range of the SWRC. A method was therefore proposed to improve the estimation of the SWRC using a pore model containing slit-shaped spaces. The results show that the predicted SWRCs using the improved method reasonably approximated the measured SWRCs.
Carlos García-Gutiérrez, Yakov Pachepsky, and Miguel Ángel Martín
Hydrol. Earth Syst. Sci., 22, 3923–3932, https://doi.org/10.5194/hess-22-3923-2018, https://doi.org/10.5194/hess-22-3923-2018, 2018
Short summary
Short summary
Saturated hydraulic conductivity (Ksat) is an important soil parameter that highly depends on soil's particle size distribution (PSD). The nature of this dependency is explored in this work in two ways, (1) by using the information entropy as a heterogeneity parameter of the PSD and (2) by using descriptions of PSD in forms of textural triplets, different than the usual description in terms of the triplet of sand, silt, and clay contents.
Matthias Sprenger, Doerthe Tetzlaff, Jim Buttle, Hjalmar Laudon, and Chris Soulsby
Hydrol. Earth Syst. Sci., 22, 3965–3981, https://doi.org/10.5194/hess-22-3965-2018, https://doi.org/10.5194/hess-22-3965-2018, 2018
Short summary
Short summary
We estimated water ages in the upper critical zone with a soil physical model (SWIS) and found that the age of water stored in the soil, as well as of water leaving the soil via evaporation, transpiration, or recharge, was younger the higher soil water storage (inverse storage effect). Travel times of transpiration and evaporation were different. We conceptualized the subsurface into fast and slow flow domains and the water was usually half as young in the fast as in the slow flow domain.
Conrad Jackisch and Erwin Zehe
Hydrol. Earth Syst. Sci., 22, 3639–3662, https://doi.org/10.5194/hess-22-3639-2018, https://doi.org/10.5194/hess-22-3639-2018, 2018
Short summary
Short summary
We present a Lagrangian model for non-uniform soil water dynamics. It handles 2-D diffusion (based on a spatial random walk and implicit pore space redistribution) and 1-D advection in representative macropores (as film flow with dynamic interaction with the soil matrix). The interplay between the domains is calculated based on an energy-balance approach which does not require any additional parameterisation. Model tests give insight into the evolution of the non-uniform infiltration patterns.
Joop Kroes, Iwan Supit, Jos van Dam, Paul van Walsum, and Martin Mulder
Hydrol. Earth Syst. Sci., 22, 2937–2952, https://doi.org/10.5194/hess-22-2937-2018, https://doi.org/10.5194/hess-22-2937-2018, 2018
Short summary
Short summary
Impact of upward flow by capillary rise and recirculation on crop yields is often neglected or underestimated. Case studies and model experiments are used to illustrate the impact of this upward flow in the Dutch delta. Neglecting upward flow results in yield reductions for grassland, maize and potatoes. Half of the withheld water behind these yield effects comes from recirculated percolation water as occurs in free-drainage conditions; the other half from increased upward capillary rise.
Stefan Jaumann and Kurt Roth
Hydrol. Earth Syst. Sci., 22, 2551–2573, https://doi.org/10.5194/hess-22-2551-2018, https://doi.org/10.5194/hess-22-2551-2018, 2018
Short summary
Short summary
Ground-penetrating radar (GPR) is a noninvasive and nondestructive measurement method to monitor the hydraulic processes precisely and efficiently. We analyze synthetic as well as measured data from the ASSESS test site and show that the analysis yields accurate estimates for the soil hydraulic material properties as well as for the subsurface architecture by comparing the results to references derived from time domain reflectometry (TDR) and subsurface architecture ground truth data.
Coleen D. U. Carranza, Martine J. van der Ploeg, and Paul J. J. F. Torfs
Hydrol. Earth Syst. Sci., 22, 2255–2267, https://doi.org/10.5194/hess-22-2255-2018, https://doi.org/10.5194/hess-22-2255-2018, 2018
Short summary
Short summary
Remote sensing has been popular for mapping surface soil moisture. However, estimating subsurface values using surface soil moisture remains a challenge, as decoupling can occur. Depth-integrated soil moisture values used in hydrological models are affected by vertical variability. Using statistical methods, we investigate vertical variability between the surface (5 cm) and subsurface (40 cm) to quantify decoupling. We also discuss potential controls for decoupling during wet and dry conditions.
Rafael Muñoz-Carpena, Claire Lauvernet, and Nadia Carluer
Hydrol. Earth Syst. Sci., 22, 53–70, https://doi.org/10.5194/hess-22-53-2018, https://doi.org/10.5194/hess-22-53-2018, 2018
Short summary
Short summary
Seasonal shallow water tables (WTs) in lowlands limit vegetation-buffer efficiency to control runoff pollution. Mechanistic models are needed to quantify true field efficiency. A new simplified algorithm for soil infiltration over WTs is tested against reference models and lab data showing WT effects depend on local settings but are negligible after 2 m depth. The algorithm is coupled to a complete vegetation buffer model in a companion paper to analyze pesticide and sediment control in situ.
Claire Lauvernet and Rafael Muñoz-Carpena
Hydrol. Earth Syst. Sci., 22, 71–87, https://doi.org/10.5194/hess-22-71-2018, https://doi.org/10.5194/hess-22-71-2018, 2018
Short summary
Short summary
Vegetation buffers, often placed in lowlands to control runoff pollution, can exhibit limited efficiency due to seasonal shallow water tables (WTs). A new shallow water table infiltration algorithm developed in a companion paper is coupled to a complete vegetation buffer model to quantify pesticide and sediment control in the field. We evaluated the model on two field experiments in France with and without WT conditions and show WTs can control efficiency depending on land and climate settings.
Tobias Karl David Weber, Sascha Christian Iden, and Wolfgang Durner
Hydrol. Earth Syst. Sci., 21, 6185–6200, https://doi.org/10.5194/hess-21-6185-2017, https://doi.org/10.5194/hess-21-6185-2017, 2017
Yonatan Ganot, Ran Holtzman, Noam Weisbrod, Ido Nitzan, Yoram Katz, and Daniel Kurtzman
Hydrol. Earth Syst. Sci., 21, 4479–4493, https://doi.org/10.5194/hess-21-4479-2017, https://doi.org/10.5194/hess-21-4479-2017, 2017
Short summary
Short summary
We monitor infiltration at multiple scales during managed aquifer recharge with desalinated seawater in an infiltration pond, while groundwater recharge is evaluated by simplified and numerical models. We found that pond-surface clogging is negated by the high-quality desalinated seawater or negligible compared to the low-permeability layers of the unsaturated zone. We show that a numerical model with a 1-D representative sediment profile is able to capture infiltration and recharge dynamics.
Stefan Jaumann and Kurt Roth
Hydrol. Earth Syst. Sci., 21, 4301–4322, https://doi.org/10.5194/hess-21-4301-2017, https://doi.org/10.5194/hess-21-4301-2017, 2017
Short summary
Short summary
We investigate the quantitative effect of neglected sensor position, small-scale heterogeneity, and lateral flow on soil hydraulic material properties. Thus, we analyze a fluctuating water table experiment in a 2-D architecture (ASSESS) with increasingly complex studies based on time domain reflectometry and hydraulic potential data. We found that 1-D studies may yield biased parameters and that estimating sensor positions as well as small-scale heterogeneity improves the model significantly.
Joseph Alexander Paul Pollacco, Trevor Webb, Stephen McNeill, Wei Hu, Sam Carrick, Allan Hewitt, and Linda Lilburne
Hydrol. Earth Syst. Sci., 21, 2725–2737, https://doi.org/10.5194/hess-21-2725-2017, https://doi.org/10.5194/hess-21-2725-2017, 2017
Short summary
Short summary
Descriptions of soil hydraulic properties, such as soil moisture release curve, θ(h), and saturated hydraulic conductivities, Ks, are a prerequisite for hydrological models. Because it is usually more difficult to describe Ks than θ(h) from pedotransfer functions, we developed a physical unimodal model to compute Ks solely from hydraulic parameters derived from the Kosugi θ(h). We further adaptations to this model to adapt it to dual-porosity structural soils.
Fadji Hassane Maina and Philippe Ackerer
Hydrol. Earth Syst. Sci., 21, 2667–2683, https://doi.org/10.5194/hess-21-2667-2017, https://doi.org/10.5194/hess-21-2667-2017, 2017
Short summary
Short summary
In many fields like climate change, hydrology and agronomy, water movement in unsaturated soils is usually simulated using the Richards equation. However, this equation requires lot of computational effort to be solved due to its highly nonlinear behavior, which hampers its use in simulations. In this paper, we analyze and developed some numerical strategies and we evaluate their reliability and efficiency.
Foad Foolad, Trenton E. Franz, Tiejun Wang, Justin Gibson, Ayse Kilic, Richard G. Allen, and Andrew Suyker
Hydrol. Earth Syst. Sci., 21, 1263–1277, https://doi.org/10.5194/hess-21-1263-2017, https://doi.org/10.5194/hess-21-1263-2017, 2017
Short summary
Short summary
Estimates of evapotranspiration are vital for validation of models. However, those datasets are often limited to research applications. Here, we explore using vadose zone modeling with widespread and readily available soil water content monitoring networks. While this work focused on one agricultural site, the framework can be used everywhere there is basic data. The resulting evapotranspiration and soil water content measurements are valuable benchmarks for evaluation of land surface models.
Justin Gibson, Trenton E. Franz, Tiejun Wang, John Gates, Patricio Grassini, Haishun Yang, and Dean Eisenhauer
Hydrol. Earth Syst. Sci., 21, 1051–1062, https://doi.org/10.5194/hess-21-1051-2017, https://doi.org/10.5194/hess-21-1051-2017, 2017
Short summary
Short summary
The human use of water for irrigation is often ignored in models and operational forecasts. We describe four plausible and relatively simple irrigation routines that can be coupled to the next generation of models. The routines are tested against a unique irrigation dataset from western Nebraska. The most aggressive water-saving irrigation routine indicates a potential irrigation savings of 120 mm yr−1 and yield losses of less than 3 % against the crop model benchmark and historical averages.
Marcos Alex dos Santos, Quirijn de Jong van Lier, Jos C. van Dam, and Andre Herman Freire Bezerra
Hydrol. Earth Syst. Sci., 21, 473–493, https://doi.org/10.5194/hess-21-473-2017, https://doi.org/10.5194/hess-21-473-2017, 2017
Short summary
Short summary
Some empirical root water uptake (RWU) models were assessed under varying environmental conditions predicted from numerical simulations with a detailed physical model. The widely used empirical RWU model by Feddes only performs well in scenarios of low RWU compensation. The RWU model by Jarvis cannot mimic the RWU patterns predicted by the physical model for high root length density scenarios. The two proposed models are more capable of predicting similar RWU patterns.
Ke Zhang, Xianwu Xue, Yang Hong, Jonathan J. Gourley, Ning Lu, Zhanming Wan, Zhen Hong, and Rick Wooten
Hydrol. Earth Syst. Sci., 20, 5035–5048, https://doi.org/10.5194/hess-20-5035-2016, https://doi.org/10.5194/hess-20-5035-2016, 2016
Short summary
Short summary
We developed a new approach to couple a distributed hydrological model, CREST, to a geotechnical landslide model, TRIGRS, to simulate both flood- and rainfall-triggered landslide hazards. By implementing more sophisticated and realistic representations of hydrological processes in the coupled model system, it shows better performance than the standalone landslide model in the case study. It highlights the important physical connection between rainfall, hydrological processes and slope stability.
Hannes H. Bauser, Stefan Jaumann, Daniel Berg, and Kurt Roth
Hydrol. Earth Syst. Sci., 20, 4999–5014, https://doi.org/10.5194/hess-20-4999-2016, https://doi.org/10.5194/hess-20-4999-2016, 2016
Short summary
Short summary
The representation of soil water movement comes with uncertainties in all model components. We assess the key uncertainties for the case of a one-dimensional soil profile with measured water contents. We employ a data assimilation method to represent and reduce the key uncertainties. For intermittent phases where model assumptions are violated, we introduce a "closed-eye period" to bridge the gap. We also demonstrate the need to include heterogeneity.
Muhammad Naveed, Per Moldrup, Marcel G. Schaap, Markus Tuller, Ramaprasad Kulkarni, Hans-Jörg Vogel, and Lis Wollesen de Jonge
Hydrol. Earth Syst. Sci., 20, 4017–4030, https://doi.org/10.5194/hess-20-4017-2016, https://doi.org/10.5194/hess-20-4017-2016, 2016
Short summary
Short summary
Quantification of rapid flow of water and associated transport of contaminants through large soil pores generated by earthworms or decaying plant roots is of crucial importance for sustaining both soil and water quality. Advanced visualization and analysis techniques based on state-of-the-art X-ray computed tomography have been applied to 65 soil cores extracted from an agricultural field in Silstrup, Denmark, to improve models for the prediction of fast, preferential flow processes in soils.
Erwin Zehe and Conrad Jackisch
Hydrol. Earth Syst. Sci., 20, 3511–3526, https://doi.org/10.5194/hess-20-3511-2016, https://doi.org/10.5194/hess-20-3511-2016, 2016
Anh Phuong Tran, Baptiste Dafflon, Susan S. Hubbard, Michael B. Kowalsky, Philip Long, Tetsu K. Tokunaga, and Kenneth H. Williams
Hydrol. Earth Syst. Sci., 20, 3477–3491, https://doi.org/10.5194/hess-20-3477-2016, https://doi.org/10.5194/hess-20-3477-2016, 2016
Short summary
Short summary
Quantifying water and heat fluxes in the shallow subsurface is particularly important due to their strong control on recharge, evaporation and biogeochemical processes. This study developed and tested a new inversion scheme to estimate subsurface hydro-thermal parameters by joint using different hydrological, thermal and geophysical data. It is especially useful for the increasing number of studies that are taking advantage of autonomously collected measurements to explore ecosystem dynamics.
Tzu-Hsien Kuo, Jen-Ping Chen, and Yongkang Xue
Hydrol. Earth Syst. Sci., 20, 1509–1522, https://doi.org/10.5194/hess-20-1509-2016, https://doi.org/10.5194/hess-20-1509-2016, 2016
Short summary
Short summary
The stem-root flow mechanism was parameterized and incorporated into the Simplified Simple Biosphere model to analyze its impact on soil moisture and land-atmospheric interactions. By testing against the Lien Hua Chih (Taiwan) and HAPEX-Mobilhy (France) measurements, the model shows that stem-root flow reduced the top-soil moisture content and moistened the deeper soil layers. Such soil moisture redistribution results in significant changes in heat flux exchange between land and atmosphere.
Lianyu Yu, Yijian Zeng, Zhongbo Su, Huanjie Cai, and Zhen Zheng
Hydrol. Earth Syst. Sci., 20, 975–990, https://doi.org/10.5194/hess-20-975-2016, https://doi.org/10.5194/hess-20-975-2016, 2016
Short summary
Short summary
The coupled water vapor and heat transport model using two different ET (ETdir, ETind) methods varied concerning the simulation of soil moisture and ET components, while agreed well for the simulation of soil temperature. Considering aerodynamic and surface resistance terms improved the ETdir method regarding simulating soil evaporation, especially after irrigation. The interactive effect of crop growth parameters with changing environment played an important role in estimating ET components.
M. Rezaei, P. Seuntjens, I. Joris, W. Boënne, S. Van Hoey, P. Campling, and W. M. Cornelis
Hydrol. Earth Syst. Sci., 20, 487–503, https://doi.org/10.5194/hess-20-487-2016, https://doi.org/10.5194/hess-20-487-2016, 2016
Short summary
Short summary
The sensitivity of the combined model (LINGRA-N and HYDRUS-1D) to hydraulic parameters, water stress, crop yield and lower boundary conditions was assessed. We showed that it is sufficient to estimate limited amount of key parameters in optimization strategies. A combined modelling approach could increase water use efficiency (12–22.5 %) and yield (5–7%) by changing irrigation scheduling. Result calls for taking into account weather forecast and soil water content data in precision agriculture.
O. Mohnke, R. Jorand, C. Nordlund, and N. Klitzsch
Hydrol. Earth Syst. Sci., 19, 2763–2773, https://doi.org/10.5194/hess-19-2763-2015, https://doi.org/10.5194/hess-19-2763-2015, 2015
M. Sprenger, T. H. M. Volkmann, T. Blume, and M. Weiler
Hydrol. Earth Syst. Sci., 19, 2617–2635, https://doi.org/10.5194/hess-19-2617-2015, https://doi.org/10.5194/hess-19-2617-2015, 2015
Short summary
Short summary
We present a novel approach that includes information about the pore water stable isotopic composition in inverse model approaches to estimate soil hydraulic parameters. Different approaches are presented and their adequacy regarding the model efficiency, realism and parameter identifiability are discussed. The advantages of the new approach are shown by an application of the inverse estimated parameters to infer the water balance and the transit time for three different study sites.
P. Ala-aho, P. M. Rossi, and B. Kløve
Hydrol. Earth Syst. Sci., 19, 1961–1976, https://doi.org/10.5194/hess-19-1961-2015, https://doi.org/10.5194/hess-19-1961-2015, 2015
Short summary
Short summary
We present a novel simulation method for estimating spatially distributed and transient groundwater recharge in unconfined sandy aquifers. The approach uses field data for the most important parameters affecting groundwater recharge and accounts for parameter uncertainty. The results show that tree canopy cover is the most important factor in controlling groundwater recharge at our study area. Tree canopy is thinned by forestry, which may lead to a significant increase of groundwater recharge.
F. Meskini-Vishkaee, M. H. Mohammadi, and M. Vanclooster
Hydrol. Earth Syst. Sci., 18, 4053–4063, https://doi.org/10.5194/hess-18-4053-2014, https://doi.org/10.5194/hess-18-4053-2014, 2014
W. J. Riley and C. Shen
Hydrol. Earth Syst. Sci., 18, 2463–2483, https://doi.org/10.5194/hess-18-2463-2014, https://doi.org/10.5194/hess-18-2463-2014, 2014
M. Parrens, J.-F. Mahfouf, A. L. Barbu, and J.-C. Calvet
Hydrol. Earth Syst. Sci., 18, 673–689, https://doi.org/10.5194/hess-18-673-2014, https://doi.org/10.5194/hess-18-673-2014, 2014
T. W. Ford, E. Harris, and S. M. Quiring
Hydrol. Earth Syst. Sci., 18, 139–154, https://doi.org/10.5194/hess-18-139-2014, https://doi.org/10.5194/hess-18-139-2014, 2014
N. Jarvis, J. Koestel, I. Messing, J. Moeys, and A. Lindahl
Hydrol. Earth Syst. Sci., 17, 5185–5195, https://doi.org/10.5194/hess-17-5185-2013, https://doi.org/10.5194/hess-17-5185-2013, 2013
A. P. Tran, M. Vanclooster, and S. Lambot
Hydrol. Earth Syst. Sci., 17, 2543–2556, https://doi.org/10.5194/hess-17-2543-2013, https://doi.org/10.5194/hess-17-2543-2013, 2013
D. Schotanus, M. J. van der Ploeg, and S. E. A. T. M. van der Zee
Hydrol. Earth Syst. Sci., 17, 1547–1560, https://doi.org/10.5194/hess-17-1547-2013, https://doi.org/10.5194/hess-17-1547-2013, 2013
M. O. Cuthbert, R. Mackay, and J. R. Nimmo
Hydrol. Earth Syst. Sci., 17, 1003–1019, https://doi.org/10.5194/hess-17-1003-2013, https://doi.org/10.5194/hess-17-1003-2013, 2013
B. Leterme, D. Mallants, and D. Jacques
Hydrol. Earth Syst. Sci., 16, 2485–2497, https://doi.org/10.5194/hess-16-2485-2012, https://doi.org/10.5194/hess-16-2485-2012, 2012
A. Hartmann, J. Lange, M. Weiler, Y. Arbel, and N. Greenbaum
Hydrol. Earth Syst. Sci., 16, 2219–2231, https://doi.org/10.5194/hess-16-2219-2012, https://doi.org/10.5194/hess-16-2219-2012, 2012
Cited articles
Albasha, R., Mailhol, J.-C., and Cheviron, B.:
Compensatory uptake functions in empirical macroscopic root water uptake models – experimental and numerical analysis,
Agr. Water Manage.,
155, 22–39, https://doi.org/10.1016/j.agwat.2015.03.010, 2015.
Allen, R. G., Jensen, M. E., Wright, J. L., and Burman, R. D.:
Operational estimates of reference evapotranspiration,
Agron J.,
81, 650–662, 1989.
Allen, R. G., Pereira, L. S., Raes, D., and Smith, M.:
Crop Evapotranspiration – Guidelines for Computing Crop Water Requirements – FAO Irrigation and Drainage paper 56,
FAO, Rome, 300, 6541, 1998.
Amenu, G. G. and Kumar, P.:
A model for hydraulic redistribution incorporating coupled soil-root moisture transport,
Hydrol. Earth Syst. Sci.,
12, 55–74, https://doi.org/10.5194/hess-12-55-2008, 2008.
Bechmann, M., Schneider, C., Carminati, A., Vetterlein, D., Attinger, S., and Hildebrandt, A.:
Effect of parameter choice in root water uptake models – the arrangement of root hydraulic properties within the root architecture affects dynamics and efficiency of root water uptake,
Hydrol. Earth Syst. Sci.,
18, 4189–4206, https://doi.org/10.5194/hess-18-4189-2014, 2014.
Bingham, I. J., Walters, D. R., Foulkes, M. J., and Paveley, N. D.:
Crop traits and the tolerance of wheat and barley to foliar disease,
Ann. Appl. Biol.,
154, 159–173, https://doi.org/10.1111/j.1744-7348.2008.00291.x, 2009.
Brandyk, T. and Wesseling, J. G.:
Steady state capillary rise in some soil profiles,
Z. Pflanz. Bodenkunde,
148, 54–65, https://doi.org/10.1002/jpln.19851480107, 1985.
Bunce, J. A.:
Effects of water stress on leaf expansion, net photosynthesis, and vegetative growth of soybeans and cotton,
Can. J. Bot.,
56, 1492–1498, 1978.
Cai, G., Vanderborght, J., Klotzsche, A., van der Kruk, J., Neumann, J., Hermes, N., and Vereecken, H.:
Construction of minirhizotron facilities for investigating root zone processes,
Vadose Zone J.,
15, https://doi.org/10.2136/vzj2016.05.0043, 2016.
Cai, G., Vanderborght, J., Couvreur, V., Mboh, C. M., and Vereecken, H.: Parameterization of Root Water Uptake Models Considering Dynamic
Root Distributions and Water Uptake Compensation, Vadose Zone J., 17, https://doi.org/10.2136/vzj2016.12.0125, 2018.
Cermak, J., Kucera, J., and Nadezhdina, N.:
Sap flow measurements with some thermodynamic methods, flow integration within trees and scaling up from sample trees to entire forest stands,
Trees-Struct. Funct.,
18, 529–546, https://doi.org/10.1007/s00468-004-0339-6, 2004.
Chabot, R., Bouarfa, S., Zimmer, D., Chaumont, C., and Moreau, S.:
Evaluation of the sap flow determined with a heat balance method to measure the transpiration of a sugarcane canopy,
Agr. Water Manage.,
75, 10–24, https://doi.org/10.1016/j.agwat.2004.12.010, 2005.
Cohen, Y., Takeuchi, S., Nozaka, J., and Yano, T.:
Accuracy of sap flow measurement using heat balance and heat pulse methods,
Agron J.,
85, 1080–1086, 1993.
Couvreur, V., Vanderborght, J., and Javaux, M.:
A simple three-dimensional macroscopic root water uptake model based on the hydraulic architecture approach,
Hydrol. Earth Syst. Sci.,
16, 2957–2971, https://doi.org/10.5194/hess-16-2957-2012, 2012.
Couvreur, V., Vanderborght, J., Beff, L., and Javaux, M.:
Horizontal soil water potential heterogeneity: simplifying approaches for crop water dynamics models,
Hydrol. Earth Syst. Sci.,
18, 1723–1743, https://doi.org/10.5194/hess-18-1723-2014, 2014a.
Couvreur, V., Vanderborght, J., Draye, X., and Javaux, M.:
Dynamic aspects of soil water availability for isohydric plants: focus on root hydraulic resistances,
Water Resour. Res.,
50, 8891–8906, https://doi.org/10.1002/2014wr015608, 2014b.
De Jong van Lier, Q., Van Dam, J., Metselaar, K., De Jong, R., and Duijnisveld, W.:
Macroscopic root water uptake distribution using a matric flux potential approach,
Vadose Zone J.,
7, 1065–1078, https://doi.org/10.2136/vzj2007.0083, 2008.
Doussan, C., Pagès, L., and Vercambre, G.: Modelling of the hydraulic architecture of root systems: an integrated approach to water absorption-model
description, Ann. Bot., 81, 213–223, https://doi.org/10.1006/anbo.1997.0540, 1998.
Doussan, C., Pierret, A., Garrigues, E., and Pagès, L.:
Water uptake by plant roots: II – modelling of water transfer in the soil root-system with explicit account of flow within the root system – comparison with experiments,
Plant Soil,
283, 99–117, https://doi.org/10.1007/s11104-004-7904-z, 2006.
Dynamax: Dynagage Sap Flow Sensor User Manual, available at:
http://dynamax.com/images/uploads/papers/Dynagage_Manual.pdf
(last access: 29 June 2017), 2009.
Feddes, R. A., Kowalik, P., Kolinskamalinka, K., and Zaradny, H.:
Simulation of field water uptake by plants using a soil water dependent root extraction function,
J. Hydrol.,
31, 13–26, https://doi.org/10.1016/0022-1694(76)90017-2, 1976.
Fitter, A. H., Graves, J. D., Self, G. K., Brown, T. K., Bogie, D. S., and Taylor, K.:
Root production, turnover and respiration under two grassland types along an altitudinal gradient: influence of temperature and solar radiation,
Oecologia,
114, 20–30, https://doi.org/10.1007/s004420050415, 1998.
Garré, S., Javaux, M., Vanderborght, J., and Vereecken, H.:
Three-dimensional electrical resistivity tomography to monitor root zone water dynamics,
Vadose Zone J.,
10, 412–424, https://doi.org/10.2136/vzj2010.0079, 2011.
Gong, D., Kang, S., Zhang, L., Du, T., and Yao, L.:
A two-dimensional model of root water uptake for single apple trees and its verification with sap flow and soil water content measurements,
Agr. Water Manage.,
83, 119–129, https://doi.org/10.1016/j.agwat.2005.10.005, 2006.
Granier, A., Huc, R., and Barigah, S.:
Transpiration of natural rain forest and its dependence on climatic factors,
Agr. Forest Meteorol.,
78, 19–29, https://doi.org/10.1016/0168-1923(95)02252-x, 1996.
Green, S. and Clothier, B.:
The root zone dynamics of water uptake by a mature apple tree,
Plant Soil,
206, 61–77, https://doi.org/10.1023/a:1004368906698, 1998.
Groh, J., Vanderborght, J., Pütz, T., and Vereecken, H.:
How to control the lysimeter bottom boundary to investigate the effect of climate change on soil processes?,
Vadose Zone J.,
15, https://doi.org/10.2136/vzj2015.08.0113, 2016.
Heinen, M.:
FUSSIM2: brief description of the simulation model and application to fertigation scenarios,
Agronomie,
21, 285–296, https://doi.org/10.1051/agro:2001124, 2001.
Howard, S., Ong, C., Black, C., and Khan, A.:
Using sap flow gauges to quantify water uptake by tree roots from beneath the crop rooting zone in agroforestry systems,
Agroforest. Syst.,
35, 15–29, https://doi.org/10.1007/bf02345326, 1996.
Huber, B.:
Beobachtung und Messung pflanzlicher Saftströme,
Ber. Dtsch. Bot. Ges.,
50, 89–109, 1932.
Jaeger, L. and Kessler, A.:
Twenty years of heat and water balance climatology at the Hartheim Pine Forest, Germany,
Agr. Forest Meteorol.,
84, 25–36, https://doi.org/10.1016/s0168-1923(96)02372-6, 1997.
Jarvis, N.:
A simple empirical model of root water uptake,
J. Hydrol.,
107, 57–72, https://doi.org/10.1016/0022-1694(89)90050-4, 1989.
Jarvis, N.:
Comment on “Macroscopic root water uptake distribution using a matric flux potential approach”,
Vadose Zone J.,
9, 499–502, https://doi.org/10.2136/vzj2009.0148, 2010.
Jarvis, N. J.:
Simple physics-based models of compensatory plant water uptake: concepts and eco-hydrological consequences,
Hydrol. Earth Syst. Sci.,
15, 3431–3446, https://doi.org/10.5194/hess-15-3431-2011, 2011.
Javaux, M., Schröder, T., Vanderborght, J., and Vereecken, H.:
Use of a three-dimensional detailed modeling approach for predicting root water uptake,
Vadose Zone J.,
7, 1079–1088, https://doi.org/10.2136/vzj2007.0115, 2008.
Khalid, M., Afzal, F., Gul, A., Ahanger, M. A., and Ahmad, P.: Analysis of
novel haplotype variation at TaDREB-D1 and TaCwi-D1 genes influencing drought
tolerance in bread/synthetic wheat derivatives, in: Water Stress and Crop
Plants, John Wiley & Sons, Ltd, 206–226, 2016.
Knaps, A.: Klimastatistik: Jahresmittelwerte von 1961–2015, available
at: http://www.fz-juelich.de/gs/DE/UeberUns/Organisation/S-U/Meteorologie/klima/statistik_tabelle.html, last access:
26 October 2016.
Langensiepen, M., Kupisch, M., Graf, A., Schmidt, M., and Ewert, F.:
Improving the stem heat balance method for determining sap-flow in wheat,
Agr. Forest Meteorol.,
186, 34–42, https://doi.org/10.1016/j.agrformet.2013.11.007, 2014.
Luo, Y., OuYang, Z., Yuan, G., Tang, D., and Xie, X.:
Evaluation of macroscopic root water uptake models using lysimeter data,
T. ASAE,
46, 625–634, 2003.
Mansfield, T. A. and Atkinson, C. J.: Stomatal behaviour in water stressed plants, in: Stress responses in plants: adaptation and acclimation
mechanisms, edited by: Alscher, R. G. and Cumming, J. R., Wiley-Liss, New York, 241–264, 1990.
Massai, R. and Remorini, D.:
Estimation of water requirements in a young peach orchard under irrigated and stressed conditions,
in:
Proceedings of the Third International Symposium on Irrigation of Horticultural Crops, Vols 1 and 2,
edited by:
Ferreira, M. I. and Jones, H. G.,
Acta Horticulturae, 537, 77–86, 2000.
Matsuo, N., Ozawa, K., and Mochizuki, T.:
Genotypic differences in root hydraulic conductance of rice (Oryza sativa L.) in response to water regimes,
Plant Soil,
316, 25–34, https://doi.org/10.1007/s11104-008-9755-5, 2009.
Maurel, C., Simonneau, T., and Sutka, M.:
The significance of roots as hydraulic rheostats,
J. Exp. Bot.,
61, 3191–3198, https://doi.org/10.1093/jxb/erq150, 2010.
Merotto Jr, A. and Mundstock, C.:
Wheat root growth as affected by soil strength,
Rev. Bras. Cienc. Solo,
23, 197–202, 1999.
Meyer, W. S. and Barrs, H. D.:
Roots in irrigated clay soils: measurement techniques and responses to root zone conditions,
Irrigation Sci.,
12, 125–134, 1991.
Molz, F. J.:
Models of water transport in the soilplant system: a review,
Water Resour. Res.,
17, 1245–1260, https://doi.org/10.1029/WR017i005p01245, 1981.
Mualem, Y.:
A new model for predicting the hydraulic conductivity of unsaturated porous media,
Water Resour. Res.,
12, 513–522, https://doi.org/10.1029/wr012i003p00513, 1976.
Musick, J. T. and Dusek, D. A.:
Planting date and water deficit effects on development and yield of irrigated winter wheat,
Agron J.,
72, 45–52, 1980.
Nimah, M. and Hanks, R.:
Model for estimating soil water, plant, and atmospheric interrelations: I. Description and sensitivity,
Soil Sci. Soc. Am. J.,
37, 522–527, https://doi.org/10.2136/sssaj1973.03615995003700040018x, 1973.
Oroud, I. M.: Climate change impacts on green water fluxes in the Eastern
Mediterranean, in: Climate Change and the Sustainable Use of Water Resources,
Springer, 3–15, 2012.
Peters, A., Durner, W., and Iden, S. C.:
Modified Feddes type stress reduction function for modeling root water uptake: accounting for limited aeration and low water potential,
Agr. Water Manage.,
185, 126–136, https://doi.org/10.1016/j.agwat.2017.02.010, 2017.
Poorter, H., Niklas, K. J., Reich, P. B., Oleksyn, J., Poot, P., and Mommer, L.:
Biomass allocation to leaves, stems and roots: meta-analyses of interspecific variation and environmental control,
New Phytol.,
193, 30–50, https://doi.org/10.1111/j.1469-8137.2011.03952.x, 2012.
Rodriguez, D., Ewert, F., Goudriaan, J., Manderscheid, R., Burkart, S., and Weigel, H. J.:
Modelling the response of wheat canopy assimilation to atmospheric CO2 concentrations,
New Phytol.,
150, 337–346, https://doi.org/10.1046/j.1469-8137.2001.00106.x, 2001.
Schmidt, M.: TERENO Data Discovery Portal – Eifel/Lower Rhine Valley Observatory, available
at: http://teodoor.icg.kfa-juelich.de/ibg3searchportal2/index.jsp, last access: 6 October 2014.
Senock, R. S., Ham, J. M., Loughin, T. M., Kimball, B. A., Hunsaker, D. J., Pinter, P. J., Wall, G. W., Garcia, R. L., and LaMorte, R. L.:
Sap flow in wheat under free-air CO2 enrichment,
Plant Cell Environ.,
19, 147–158, https://doi.org/10.1111/j.1365-3040.1996.tb00236.x, 1996.
Šimůnek, J. and Hopmans, J. W.:
Modeling compensated root water and nutrient uptake,
Ecol. Model.,
220, 505–521, https://doi.org/10.1016/j.ecolmodel.2008.11.004, 2009.
Šimůnek, J., Šejna, M., Saito, H., Sakai, M., and van Genuchten, M.:
The HYDRUS-1-D software package for simulating the one-dimensional movement of water, heat and multiple solutes in variably-saturated media,
in:
HYDRUS Software Series 3, Version 4.17 ed.,
Department of Environmental Sciences, University of California Riverside, Riverside, California, US, 2013.
Šimůnek, J., van Genuchten, M. T., and Šejna, M.:
Recent developments and applications of the HYDRUS computer software packages,
Vadose Zone J.,
15, https://doi.org/10.2136/vzj2016.04.0033, 2016.
Skaggs, T. H., van Genuchten, M. T., Shouse, P. J., and Poss, J. A.:
Macroscopic approaches to root water uptake as a function of water and salinity stress,
Agr. Water Manage.,
86, 140–149, https://doi.org/10.1016/j.agwat.2006.06.005, 2006.
Steudle, E.:
Water uptake by roots: effects of water deficit,
J. Exp. Bot.,
51, 1531–1542, https://doi.org/10.1093/jexbot/51.350.1531, 2000.
Tardieu, F., Parent, B., Caldeira, C. F., and Welcker, C.:
Genetic and physiological controls of growth under water deficit,
Plant Physiol.,
164, 1628–1635, https://doi.org/10.1104/pp.113.233353, 2014.
Thorup-Kristensen, K., Cortasa, M. S., and Loges, R.:
Winter wheat roots grow twice as deep as spring wheat roots, is this important for N uptake and N leaching losses?,
Plant Soil,
322, 101–114, https://doi.org/10.1007/s11104-009-9898-z, 2009.
Trillo, N. and Fernandez, R. J.:
Wheat plant hydraulic properties under prolonged experimental drought: stronger decline in root-system conductance than in leaf area,
Plant Soil,
277, 277–284, https://doi.org/10.1007/s11104-005-7493-5, 2005.
Twine, T. E., Kustas, W., Norman, J., Cook, D., Houser, P., Meyers, T., Prueger, J., Starks, P., and Wesely, M.:
Correcting eddy-covariance flux underestimates over a grassland,
Agr. Forest Meteorol.,
103, 279–300, https://doi.org/10.1016/s0168-1923(00)00123-4, 2000.
Unger, P. W. and Kaspar, T. C.:
Soil compaction and root growth – a review,
Agron J.,
86, 759–766, 1994.
Vadez, V.:
Root hydraulics: the forgotten side of roots in drought adaptation,
Field Crop. Res.,
165, 15–24, https://doi.org/10.1016/j.fcr.2014.03.017, 2014.
Van Genuchten, M. T.:
A closed-form equation for predicting the hydraulic conductivity of unsaturated soils,
Soil Sci. Soc. Am. J.,
44, 892–898, 1980.
van Lier, Q. D., van Dam, J. C., Metselaar, K., de Jong, R., and Duijnisveld, W. H. M.:
Macroscopic root water uptake distribution using a matric flux potential approach,
Vadose Zone J.,
7, 1065–1078, https://doi.org/10.2136/vzj2007.0083, 2008.
Vandoorne, B., Beff, L., Lutts, S., and Javaux, M.:
Root water uptake dynamics of Cichorium intybus var. sativum under water-limited conditions,
Vadose Zone J.,
11, https://doi.org/10.2136/vzj2012.0005, 2012.
Vereecken, H., Huisman, J. A., Franssen, H. J. H., Bruggemann, N., Bogena, H. R., Kollet, S., Javaux, M., van der Kruk, J., and Vanderborght, J.:
Soil hydrology: recent methodological advances, challenges, and perspectives,
Water Resour. Res.,
51, 2616–2633, https://doi.org/10.1002/2014wr016852, 2015.
Vereecken, H., Schnepf, A., Hopmans, J. W., Javaux, M., Or, D., Roose, D. O. T., Vanderborght, J., Young, M. H., Amelung, W., Aitkenhead, M., Allison, S. D., Assouline, S., Baveye, P., Berli, M., Bruggemann, N., Finke, P., Flury, M., Gaiser, T., Govers, G., Ghezzehei, T., Hallett, P., Franssen, H. J. H., Heppell, J., Horn, R., Huisman, J. A., Jacques, D., Jonard, F., Kollet, S., Lafolie, F., Lamorski, K., Leitner, D., McBratney, A., Minasny, B., Montzka, C., Nowak, W., Pachepsky, Y., Padarian, J., Romano, N., Roth, K., Rothfuss, Y., Rowe, E. C., Schwen, A., Šimůnek, J., Tiktak, A., Van Dam, J., van der Zee, S., Vogel, H. J., Vrugt, J. A., Wohling, T., and Young, I. M.:
Modeling soil processes: review, key challenges, and new perspectives,
Vadose Zone J.,
15, https://doi.org/10.2136/vzj2015.09.0131, 2016.
Walter, A. and Schurr, U.: Dynamics of leaf and root growth: endogenous control versus environmental impact, Ann. Bot., 95, 891–900,
https://doi.org/10.1093/aob/mci103, 2005.
Wang, M., Zheng, Q. S., Shen, Q. R., and Guo, S. W.:
The critical role of potassium in plant stress response,
Int. J. Mol. Sci.,
14, 7370–7390, https://doi.org/10.3390/ijms14047370, 2013.
Wells, C. and Birchfield, S.:
Rootfly: Software for Minirhizotron Image Analysis,
Clemson University, Kingstree, SC, 2009.
Wesseling, J.: Meerjarige simulaties van grondwateronttrekking voor verschillende bodemprofielen, grondwatertrappen en gewassen met het model SWATRE,
Wageningen, SC-DLO Report 152, 1991.
Wesselius, J. C. and Brouwer, R.: Influence of water stress on
photosynthesis, respiration and leaf growth of Zea mais L.,
Mededelingen Landbouwhogeschool Wageningen, 72, 1–15, 1972.
White, C. A., Sylvester-Bradley, R., and Berry, P. M.:
Root length densities of UK wheat and oilseed rape crops with implications for water capture and yield,
J. Exp. Bot.,
66, 2293–2303, https://doi.org/10.1093/jxb/erv077, 2015.
Xin-yang, Z. and Yang-ren, W.: Effect of water and nitrogen stresses on correlation among winter wheat organs, 7th International
Conference on Computer and Computing Technologies in Agriculture (CCTA), Beijing, China, September 18–20, 2013, 316–325, 2013.
Yang, D., Zhang, T., Zhang, K., Greenwood, D. J., Hammond, J. P., and White, P. J.:
An easily implemented agro-hydrological procedure with dynamic root simulation for water transfer in the crop–soil system: validation and application,
J. Hydrol.,
370, 177–190, https://doi.org/10.1016/j.jhydrol.2009.03.005, 2009.
Yang, J., Hammer, R. D., and Blanchar, R. W.:
Minirhizotron quantification of soybean root growth as affected by reduced – a horizon in soil,
J. Plant Nutr. Soil Sc.,
166, 708–711, https://doi.org/10.1002/jpln.200321193, 2003.
Zhang, X. Y., Pei, D., and Chen, S. Y.:
Root growth and soil water utilization of winter wheat in the North China Plain,
Hydrol. Process,
18, 2275–2287, https://doi.org/10.1002/hyp.5533, 2004.
Zhang, Z., Tian, F., Hu, H., and Yang, P.:
A comparison of methods for determining field evapotranspiration: photosynthesis system, sap flow, and eddy covariance,
Hydrol. Earth Syst. Sci.,
18, 1053–1072, https://doi.org/10.5194/hess-18-1053-2014, 2014.
Zhou, S., Han, Y. Y., Chen, Y. H., Kong, X. Z., and Wang, W.:
The involvement of expansins in response to water stress during leaf development in wheat,
J. Plant Physiol.,
183, 64–74, https://doi.org/10.1016/j.jplph.2015.05.012, 2015.
Search articles
Short summary
Different crop growths had consequences for the parameterization of root water uptake models. The root hydraulic parameters of the Couvreur model but not the water stress parameters of the Feddes–Jarvis model could be constrained by the field data measured from rhizotron facilities. The simulated differences in transpiration from the two soils and the different water treatments could be confirmed by sap flow measurements. The Couvreur model predicted the ratios of transpiration fluxes better.
Different crop growths had consequences for the parameterization of root water uptake models....
Hydrology and Earth System Sciences
An interactive open-access journal of the European Geosciences Union
All site content, except where otherwise noted, is licensed under the Creative Commons Attribution 4.0 License.