All Stories

  1. An improved van Genuchten soil water characteristic model to account for surface adsorptive forces
  2. Wi-Fi signal for soil moisture sensing
  3. Experimental evidence of non-equilibrium water flow during bare-soil evaporation
  4. Extending the measurement range for determining soil hydraulic properties with the simplified evaporation method using relative humidity sensors
  5. Effects of improved water retention by increased soil organic matter on the water balance of arable soils: A numerical analysis
  6. Prediction of absolute unsaturated hydraulic conductivity – comparison of four different capillary bundle models
  7. Soil water retention and hydraulic conductivity measured in a wide saturation range
  8. Validating coupled flow theory for bare‐soil evaporation under different boundary conditions
  9. Improved calculation of soil hydraulic conductivity with the simplified evaporation method
  10. Reproducibility of the wet part of the soil water retention curve: a European interlaboratory comparison
  11. Full prediction of unsaturated hydraulic conductivity – comparison of four different capillary bundle models
  12. Supplementary material to "Full prediction of unsaturated hydraulic conductivity – comparison of four different capillary bundle models"
  13. The Influence of the Osmotic Potential on Evapotranspiration
  14. Coupled hydrothermal modelling of subsurface heating in the vicinity of high-power power cables under natural conditions
  15. Validation of coupled water, vapor and heat flow models with evaporation experiments
  16. Prediction of the absolute hydraulic conductivity function from soil water retention data
  17. Soil water retention and hydraulic conductivity measured in a wide saturation range
  18. Rock fragments influence the water retention and hydraulic conductivity of soils
  19. Prediction of the absolute hydraulic conductivity function from soil water retention data
  20. Supplementary material to "Prediction of the absolute hydraulic conductivity function from soil water retention data"
  21. Reproducibility of the Wet Part of the Soil Water Retention Curve: A European Interlaboratory Comparison
  22. Supplementary material to "Reproducibility of the Wet Part of the Soil Water Retention Curve: A European Interlaboratory Comparison"
  23. Rock fragments influence the water retention and hydraulic conductivity of soils
  24. Effective Hydraulic Properties of Stony Soils: Simulation, Laboratory Experiment and Modeling
  25. Simultaneous estimation of soil hydraulic properties and surface evaporation using inverse modeling for a large field-lysimeter
  26. Effective hydraulic properties of 3D virtual stony soils identified by inverse modeling
  27. Effective hydraulic properties of 3D virtual stony soils identified by inverse modeling
  28. The improved integral suspension pressure method (ISP+) for precise particle size analysis of soil and sedimentary materials
  29. A Simple Model to Predict Hydraulic Conductivity in Medium to Dry Soil From the Water Retention Curve
  30. Capillary, Film, and Vapor Flow in Transient Bare Soil Evaporation (1): Identifiability Analysis of Hydraulic Conductivity in the Medium to Dry Moisture Range
  31. Capillary, Film, and Vapor Flow in Transient Bare Soil Evaporation (2): Experimental Identification of Hydraulic Conductivity in the Medium to Dry Moisture Range
  32. Developing Pseudo Continuous Pedotransfer Functions for International Soils Measured with the Evaporation Method and the HYPROP System: II. The Soil Hydraulic Conductivity Curve
  33. Actual evaporation from bare soils - A comparison of numerical modelling and field lysimeter data
  34. Coupled water, vapor and heat flow in evaporation experiments under different boundary conditions
  35. Determining the particle-size distribution of soil materials with the integral suspension pressure (ISP) method – lessons learned from PARIO measurements
  36. Effective hydraulic properties of virtual stony soils: Forward 3D simulations evaluated by 1D inverse modeling
  37. Innovative method for installing soil moisture probes in a large‐scale undisturbed gravel lysimeter
  38. Developing Pseudo Continuous Pedotransfer Functions for International Soils Measured with the Evaporation Method and the HYPROP System: I. The Soil Water Retention Curve
  39. A physical based model to describe effective hydraulic conductivity of the soil mixtures
  40. Effect of stones on soil hydraulic properties: measurement and modeling
  41. Testing the improved Integral Suspension Pressure method ISP+ with the PARIO™ device
  42. Studying Unimodal, Bimodal, PDI and Bimodal-PDI Variants of Multiple Soil Water Retention Models: I. Direct Model Fit Using the Extended Evaporation and Dewpoint Methods
  43. Studying Unimodal, Bimodal, PDI and Bimodal-PDI Variants of Multiple Soil Water Retention Models: II. Evaluation of Parametric Pedotransfer Functions Against Direct Fits
  44. Temperature Dependence of Soil Hydraulic Properties: Transient Measurements and Modeling
  45. Effects of Bentonite, Hydrogel and Biochar Amendments on Soil Hydraulic Properties from Saturation to Oven Dryness
  46. A Modular Framework for Modeling Unsaturated Soil Hydraulic Properties Over the Full Moisture Range
  47. Measuring near‐saturated hydraulic conductivity of soils by quasi unit‐gradient percolation—2. Application of the methodology
  48. Measuring near‐saturated hydraulic conductivity of soils by quasi unit‐gradient percolation—1. Theory and numerical analysis
  49. Determination of the Soil Water Retention Curve around the Wilting Point: Optimized Protocol for the Dewpoint Method
  50. Numerical test of the laboratory evaporation method using coupled water, vapor and heat flow modelling
  51. Influence of Stone Content on Soil Hydraulic Properties: Experimental Investigation and Test of Existing Model Concepts
  52. Local Solute Sinks and Sources Cause Erroneous Dispersion Fluxes in Transport Simulations with the Convection–Dispersion Equation
  53. Eddy covariance based surface-atmosphere exchange and crop coefficient determination in a mountainous peatland
  54. Measurement and estimation of the soil water retention curve using the evaporation method and the pseudo continuous pedotransfer function
  55. Robust Inverse Modeling of Growing Season Net Ecosystem Exchange in a Mountainous Peatland: Influence of Distributional Assumptions on Estimated Parameters and Total Carbon Fluxes
  56. Comparing Methods for Measuring Water Retention of Peat Near Permanent Wilting Point
  57. A pore-size classification for peat bogs derived from unsaturated hydraulic properties
  58. Towards an unbiased filter routine to determine precipitation and evapotranspiration from high precision lysimeter measurements
  59. Peatland bog pedogenesis is reflected in unsaturated hydraulic properties
  60. Supplementary material to "Peatland bog pedogenesis is reflected in unsaturated hydraulic properties"
  61. Modified Feddes type stress reduction function for modeling root water uptake: Accounting for limited aeration and low water potential
  62. New method for particle size analysis of soils
  63. Unsaturated hydraulic properties ofSphagnummoss and peat reveal trimodal pore-size distributions
  64. Prediction of capillary air-liquid interfacial area vs. saturation function from relationship between capillary pressure and water saturation
  65. Lead removal from aqueous solutions by raw sawdust and magnesium pretreated biochar: Experimental investigations and numerical modelling
  66. Biofilm effect on soil hydraulic properties: Experimental investigation using soil‐grown real biofilm
  67. Improving prediction of hydraulic conductivity by constraining capillary bundle models to a maximum pore size
  68. Modeling dynamic non-equilibrium water flow observations under various boundary conditions
  69. soil water retention
  70. A comprehensive filtering scheme for high-resolution estimation of the water balance components from high-precision lysimeters
  71. Revisiting the simplified evaporation method: Identification of hydraulic functions considering vapor, film and corner flow
  72. Relationships between soil hydraulic parameters and induced polarization spectra
  73. Does water repellency of pyrochars and hydrochars counter their positive effects on soil hydraulic properties?
  74. Closed‐Form Model for Hydraulic Properties Based on Angular Pores with Lognormal Size Distribution
  75. High-resolution estimation of the water balance components from high-precision lysimeters
  76. Comment on “Simple consistent models for water retention and hydraulic conductivity in the complete moisture range” by A. Peters
  77. The effect of temperature-induced soil water repellency on transient capillary pressure-water content relations during capillary rise
  78. Changes in the molecular composition of organic matter leached from an agricultural topsoil following addition of biomass-derived black carbon (biochar)
  79. Water retention characteristics of soils over the whole moisture range: a comparison of laboratory methods
  80. Physically-based model of soil hydraulic properties accounting for variable contact angle and its effect on hysteresis
  81. Virtual Soils: Moisture Measurements and Their Interpretation by Inverse Modeling
  82. Effect of soil water repellency on soil hydraulic properties estimated under dynamic conditions
  83. Virtual Soils: Assessment of the Effects of Soil Structure on the Hydraulic Behavior of Cultivated Soils
  84. Inverse Estimation of Soil Hydraulic and Root Distribution Parameters from Lysimeter Data
  85. Dynamic Nonequilibrium of Water Flow in Porous Media: A Review
  86. Estimating Freundlich isotherm parameters of heavy metals from multiple batch extraction tests using a Bayesian approach
  87. Inverse modeling of dynamic nonequilibrium in water flow with an effective approach
  88. Consistent parameter constraints for soil hydraulic functions
  89. Combined Transient Method for Determining Soil Hydraulic Properties in a Wide Pressure Head Range
  90. Extended multistep outflow method for the accurate determination of soil hydraulic properties near water saturation
  91. Analysis of the Agreement of Soil Hydraulic Properties Obtained from Multistep‐Outflow and Evaporation Methods
  92. Evaporation Method for Measuring Unsaturated Hydraulic Properties of Soils: Extending the Measurement Range
  93. The evaporation method: Extending the measurement range of soil hydraulic properties using the air‐entry pressure of the ceramic cup
  94. Reply to comment by N. Shokri and D. Or on “A simple model for describing hydraulic conductivity in unsaturated porous media accounting for film and capillary flow”
  95. Environmental Fate – Geoökologie in einer sich verändernden Umwelt
  96. Free‐Form estimation of soil hydraulic properties using Wind’s method
  97. A simple model for describing hydraulic conductivity in unsaturated porous media accounting for film and capillary flow
  98. From the pore scale to the lab scale: 3-D lab experiment and numerical simulation of drainage in heterogeneous porous media
  99. Prediction of capillary hysteresis in a porous material using lattice-Boltzmann methods and comparison to experimental data and a morphological pore network model
  100. Simplified evaporation method for determining soil hydraulic properties
  101. Assessing Contaminant Mobilization from Waste Materials: Application of Bayesian Parameter Estimation to Batch Extraction Tests at Varying Liquid-to-Solid Ratios
  102. Multiple batch extraction test to estimate contaminant release parameters using a Bayesian approach
  103. Effective hydraulic properties of layered soils at the lysimeter scale determined by inverse modelling
  104. Free‐form estimation of the unsaturated soil hydraulic properties by inverse modeling using global optimization
  105. Spatial and temporal variability of water repellency in a sandy soil contaminated with tar oil and heavy metals
  106. Improved estimation of soil water retention characteristics from hydrostatic column experiments
  107. Spatial variability of arsenic and chromium in the soil water at a former wood preserving site
  108. Closed‐Form Expression for the Multi‐Modal Unsaturated Conductivity Function
  109. Simulation of chromium transport in the unsaturated zone for predicting contaminant entries into the groundwater
  110. Modeling Transient Water and Solute Transport in a Biporous Soil
  111. Hydraulic conductivity estimation for soils with heterogeneous pore structure
  112. Transport of phthalate-esters in undisturbed and unsaturated soil columns