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Table of Contents


Volume 7 Issue 3, August 2008


    • Youssef Loukili, Allan D. Woodbury and Kenneth R. Snelgrove
      SABAE-HW: An Enhanced Water Balance Prediction in the Canadian Land Surface Scheme Compared with Existing Models
      A new land surface scheme, SABAE-HW, an extension of the Canadian LSS (CLASS v2.6), is presented. The model is user-friendly and allows specified soil column depth and layers. Diverse simulations under warm and freezing weather conditions reveal the worth of SABAE-HW predictions that are contrasted to results from other models including SHAW.
      Vadose Zone Journal 2008 7:865-877
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    • Eran Segal, Scott A. Bradford, Pete Shouse, Naftali Lazarovitch and Dennis Corwin
      Integration of Hard and Soft Data to Characterize Field-Scale Hydraulic Properties for Flow and Transport Studies
      Acquiring a high level of confidence in the hydraulic properties at field sites is a challenge. We present an integrated approach, using both “hard” and “soft” data sets of field and laboratory scales in conjunction with pedotransfer functions, interpolation algorithms, and numerical modeling to characterize vadose zone hydraulic properties.
      Vadose Zone Journal 2008 7:878-889
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    • Sergio M. Abit, Aziz Amoozegar, Michael J. Vepraskas and Christopher P. Niewoehner
      Solute Transport in the Capillary Fringe and Shallow Groundwater: Field Evaluation
      We present results from a field evaluation of horizontal transport of miscible solutes in the capillary fringe and shallow groundwater. Bromide tracer applied above the capillary fringe entered and moved horizontally in the capillary fringe until bromide was partially moved into the shallow groundwater by rain-induced fluctuation of the water table.
      Vadose Zone Journal 2008 7:890-898
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    • G. Webb, S.W. Tyler, J. Collord, D. Van Zyl, T. Halihan, J. Turrentine and T. Fenstemaker
      Field-Scale Analysis of Flow Mechanisms in Highly Heterogeneous Mining Media
      Field-scale infiltration results conducted at a highly heterogeneous Au heap leach mine revealed only limited preferential flow when the applied fluxes were far below the field saturated hydraulic conductivity. These results confirm the high Au recovery rates commonly seen in these systems.
      Vadose Zone Journal 2008 7:899-908
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    • Onur Akay, Garey A. Fox and Jirka Šimůnek
      Numerical Simulation of Flow Dynamics during Macropore–Subsurface Drain Interactions Using HYDRUS
      Macropores have the potential to be hydraulically connected to subsurface drains, thereby impacting contaminant transport. This research modeled laboratory experiments of surface-connected and buried macropores located in the vicinity of a drain using a three-dimensional flow code capable of simulating both soil matrix and macropore flow domains.
      Vadose Zone Journal 2008 7:909-918
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    • Craig F. Nichol, Dwayne K. Rowlett and S. Lee Barbour
      A New Standpipe Lysimeter Design for the Measurement of Soil Matric Suction
      Soil matric suction in deep vadose zones is controlled by the net infiltration rate. Measurements using borehole installations are difficult. A new method for measuring soil matric suction within boreholes is presented that requires no electronics and no calibration. Careful consideration of the soil materials and response times is required.
      Vadose Zone Journal 2008 7:919-929
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    • Prabhakar Sharma, Hesham M. Abdou and Markus Flury
      Effect of the Lower Boundary Condition and Flotation on Colloid Mobilization in Unsaturated Sandy Sediments
      We demonstrate that during unsaturated flow in sediments, colloids can be mobilized by attachment to a moving liquid-gas interface. As hydraulic boundary conditions imposed by sampling devices or column outflow systems will affect liquid-gas interface configurations, colloid mobilization is affected by the type of boundary condition as well.
      Vadose Zone Journal 2008 7:930-940
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    • Karletta Chief, Ty P. A. Ferré and Andrew C. Hinnell
      The Effects of Anisotropy on In Situ Air Permeability Measurements
      In situ air permeability measurements were modeled with a three-dimensional finite element flow model. Results showed that anisotropy produces an error factor of 2 for air permeameters with high diameter/height ratios. In situ and ex situ air permeability can be used to infer anisotropy, especially for large diameter/height ratios and small horizontal permeability.
      Vadose Zone Journal 2008 7:941-947
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    • Uri Nachshon, Noam Weisbrod and Maria Ines Dragila
      Quantifying Air Convection through Surface-Exposed Fractures: A Laboratory Study
      Quantitative relationships were established between the velocities of convection cells, the mass-transfer rate due to convection, and the Rayleigh and Sherwood numbers for a large aperture fracture. Convective flow and the consequently high replacement rate of fracture air could impact evaporation and gas exchange rates with the atmosphere.
      Vadose Zone Journal 2008 7:948-956
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    • Ken'ichirou Kosugi
      Comparison of Three Methods for Discretizing the Storage Term of the Richards Equation
      Numerical experiments and theoretical interpretation conducted in this study revealed why the extensively used mass conservative approach for discretizing the storage term of the Richards equation, based on a mixed form of the equation, is superior to the traditional chain rule expansion approach and another mass conservative approach using a chord-slope approximation.
      Vadose Zone Journal 2008 7:957-965
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    • Martin H. Schroth, Mart Oostrom, Richard Dobson and Josef Zeyer
      Thermodynamic Model for Fluid–Fluid Interfacial Areas in Porous Media for Arbitrary Drainage–Imbibition Sequences
      Vadose Zone Journal 2008 7:966-971
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    • M. A. Mojid and H. Cho
      Wetting Solution and Electrical Double Layer Contributions to Bulk Electrical Conductivity of Sand–Clay Mixtures
      Wetting liquids and electrical double layers contribute to the bulk electrical conductivity of expandable soils in a rather unusual way. Leached cations in soils offset cationic contributions of a wetting liquid to surface conductivity. Changing sample volume with a wetting liquid shows a pseudobehavior of the electrical formation factor.
      Vadose Zone Journal 2008 7:972-980
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    • Alex Mayer, Todd Sandman and Michael Breidenbach
      Effect of Flow Regime on Physical Nonequilibrium Transport in Unsaturated Porous Media
      Mobile–immobile (MIM) transport parameters estimated from tracer experiments in two sands depended strongly on water content or pore velocity. Dispersivities and mass transfer coefficients in transient flow in the uniform sand were higher than for steady flow, indicating that MIM behavior depends on flow regime and porous medium characteristics.
      Vadose Zone Journal 2008 7:981-991
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    • Naem Th. Mazahrih, Nedal Katbeh-Bader, Steven R. Evett, James E. Ayars and Thomas J. Trout
      Field Calibration Accuracy and Utility of Four Down-Hole Water Content Sensors
      A field calibration of the neutron moisture meter (NMM) and three capacitance (EM) sensors in a Panoche clay loam soil in the San Joaquin Valley, California, showed that, in contrast to the NMM, EM sensor calibrations changed greatly with depth, often requiring separate calibrations for every 10- or 20-cm depth range, and were relatively inaccurate.
      Vadose Zone Journal 2008 7:992-1000
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    • Radek Fučík, Jirí Mikyška, Michal Beneš and Tissa H. Illangasekare
      Semianalytical Solution for Two-Phase Flow in Porous Media with a Discontinuity
      We present a benchmark solution for one-dimensional porous media with heterogeneity involving two soils separated by a sharp interface. The proposed solution allows the inclusion of advection terms in a limited way. A computationally efficient algorithm and several computational results are presented.
      Vadose Zone Journal 2008 7:1001-1007
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    • Todd H. Skaggs and Peter J. Shouse
      Roots and Root Function: Introduction
      The topics addressed in this special section on plant roots and root function include: imaging techniques for observing roots and uptake processes; methods for measuring water potential in the root zone; modeling of uptake mechanisms; species- and biome-level investigations of root development and functioning; and effects of gravity on root growth.
      Vadose Zone Journal 2008 7:1008-1009
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    • A. Pohlmeier, A. Oros-Peusquens, M. Javaux, M. I. Menzel, J. Vanderborght, J. Kaffanke, S. Romanzetti, J. Lindenmair, H. Vereecken and N. J. Shah
      Changes in Soil Water Content Resulting from Ricinus Root Uptake Monitored by Magnetic Resonance Imaging
      The application of a new MRI method for the determination of water content changes in soils is described. By coregistration of the 3D root architecture in a soil chamber planted with a 4-wk-old Ricinus communis carmencita, we showed that the largest water content changes took place in the regions with highest root densities.
      Vadose Zone Journal 2008 7:1010-1017
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    • Eran Segal, Tammar Kushnir, Yechezkel Mualem and Uri Shani
      Microsensing of Water Dynamics and Root Distributions in Sandy Soils
      The mechanisms of root water and nutrient uptake in soils have not been studied experimentally in detail because of the difficulty of measuring quantities at the microscale. We used magnetic resonance imaging and microtensiometry to image a seedling's root system and to quantify the dynamics of water migration toward roots and especially at the root–soil interface.
      Vadose Zone Journal 2008 7:1018-1026
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    • Eran Segal, Tammi Kushnir, Yechezkel Mualem and Uri Shani
      Water Uptake and Hydraulics of the Root Hair Rhizosphere
      Root hairs develop along the surface of roots to enhance the uptake of soil moisture and nutrients; however, the exact nature of this structural development is not fully understood. A model and magnetic resonance imaging technology demonstrate that root surface area is effectively increased by root hair presence and consequently enhance root water uptake.
      Vadose Zone Journal 2008 7:1027-1034
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    • Sascha E. Oswald, Manoj Menon, Andrea Carminati, Peter Vontobel, Eberhard Lehmann and Rainer Schulin
      Quantitative Imaging of Infiltration, Root Growth, and Root Water Uptake via Neutron Radiography
      Water flow in soil and plant roots is imaged by neutron radiography, a non-invasive method sensitive to the detection of water. For the first time, we image complete root systems and their development jointly with water distribution dynamics during and after irrigation. Our systems consisted of either a lupin or a maize plant in a fine sand medium.
      Vadose Zone Journal 2008 7:1035-1047
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    • Martine J. van der Ploeg, Hermanus P. A. Gooren, Gerben Bakker and Gerrit H. de Rooij
      Matric Potential Measurements by Polymer Tensiometers in Cropped Lysimeters under Water-Stressed Conditions
      Direct soil water potential measurements by polymer tensiometers help in defining levels of local water stress in root water uptake experiments, especially in dry soil where moisture content measurements become less informative. Observed temporal matric potential patterns showed changing root water uptake behavior under water-stressed conditions.
      Vadose Zone Journal 2008 7:1048-1054
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    • Rodrigo Vargas and Michael F. Allen
      Dynamics of Fine Root, Fungal Rhizomorphs, and Soil Respiration in a Mixed Temperate Forest: Integrating Sensors and Observations
      New technologies are providing crucial information to understand belowground processes. We integrated continuous measurements of fine roots and rhizomorphs with automated measurements of soil respiration. Large changes in root and rhizomorph length occurred in less than 4 days and may contribute to daily variation in soil respiration.
      Vadose Zone Journal 2008 7:1055-1064
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    • Q. de Jong van Lier, J. C. van Dam, K. Metselaar, R. de Jong and W. H. M. Duijnisveld
      Macroscopic Root Water Uptake Distribution Using a Matric Flux Potential Approach
      A physically based model is presented that includes a water uptake partitioning mechanism based on root density and matric flux potential, suppressing the need of several empirical parameters. Simulation results show good agreement between model predictions and long-term experimental measurements of soil water content.
      Vadose Zone Journal 2008 7:1065-1078
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    • Mathieu Javaux, Tom Schröder, Jan Vanderborght and Harry Vereecken
      Use of a Three-Dimensional Detailed Modeling Approach for Predicting Root Water Uptake
      The impact of the parameterization of a three-dimensional root-soil water flow model (R-SWMS) was investigated. Radial root conductivity and soil hydraulic functions controlled the distribution of the soil-root water fluxes. It was shown that different water content spatial distributions may result in similar one-dimensional sink term profiles.
      Vadose Zone Journal 2008 7:1079-1088
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    • Tom Schröder, Mathieu Javaux, Jan Vanderborght, Bernd Körfgen and Harry Vereecken
      Effect of Local Soil Hydraulic Conductivity Drop Using a Three-Dimensional Root Water Uptake Model
      In this study a microscopic model was developed that links a three-dimensional soil macroscopic flow model with the water flow in the root system, considering local hydraulic effects. Results show that local effects play a large role, especially when the radial root conductivity regulating root water uptake is larger than the soil hydraulic conductivity.
      Vadose Zone Journal 2008 7:1089-1098
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    • Deniz I. Demirkanli, Fred J. Molz, Daniel I. Kaplan and Robert A. Fjeld
      A Fully Transient Model for Long-Term Plutonium Transport in the Savannah River Site Vadose Zone: Root Water Uptake
      A transient variably saturated flow model with root water uptake is developed and coupled to a previously developed reactive transport model to evaluate observed upward migration of Pu in 11-yr-old field lysimeters. This analysis strongly suggests that upward migration is the result of Pu uptake into the transpiration stream.
      Vadose Zone Journal 2008 7:1099-1109
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    • Brent D. Newman and Robert C. Graham
      Species-Level Impacts on Chaparral Root Zone Hydrology
      Impacts of chaparral vegetation on root zone hydrology for a 50-year old experiment are described. Water content, matric potential, chloride mass balance, and stable isotope results suggest only minor species-level differences. However, some differences are statistically significant, indicating that vegetation type is affecting hydrologic behavior.
      Vadose Zone Journal 2008 7:1110-1118
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    • H. Jochen Schenk
      The Shallowest Possible Water Extraction Profile: A Null Model for Global Root Distributions
      A soil water infiltration and extraction model was designed to test the hypothesis that ecosystem-level root profiles tend to be as shallow as possible and as deep as needed to fulfill evapotranspirational demands. The model was tested succesfully against root data from eight biomes, showing that it allows prediction of global root distributions.
      Vadose Zone Journal 2008 7:1119-1124
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    • M. B. Kirkham
      Horizontal Root Growth: Water Uptake and Stomatal Resistance under Microgravity
      Astronauts need to grow food in space. Growth is directly related to stomatal opening, but stomatal resistance has not been measured under microgravity. I grew wheat in horizontal columns with soil to simulate gravity-free conditions. The roots did not grow into the soil; stomatal resistance was high. Aeroponics may be needed for growth in space.
      Vadose Zone Journal 2008 7:1125-1131
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