| Time |
Referent |
Title |
| 08:30
- 08:50 |
von
Waldow |
The kinematic wave approach for modelling long-term meso-scale unsaturated zone flow and transport |
| 08:50
- 09:10 |
Samani |
A simple method for simultaneous prediction of saturated hydraulic conductivity and effective porosity
(Full Paper) |
| 09:10
- 09:30 |
Puhlmann |
Artificial nerual networks for estimating soil hydraulic parameters from evaporation experiments |
| 09:30
- 09:50 |
Zarei |
A simple model for nonsteady evaporation |
| 09:50
- 10:10 |
Givi |
Evaluation
of the Multivariate Adaptive Regression Splines (MARS) and Artificial
Neural Networks (ANN) Techniques for Estimating Soil Available Water |
| 10:10
- 10:30 |
Abbasi |
Experimental and numerical analyse of water flow and sulfate transport in the soil |
| 10:30
- 11:00 |
break |
| 11:00
- 11:40 |
Kutilek |
Keynote:
Soil Water in the System of Hydropedology (Full Paper) |
| 11:40
- 12:00 |
Skierucha |
The measurement of dielectric properties of soil at microwave frequencies using open-ended coaxial and three-wire TDR probes |
| 12:00
- 12:20 |
Wegehenkel |
The validation of soil water balance models with different measurement methods
(Full Paper) |
| 12:20
- 12:40 |
Tillmann |
Non-invasive 3D conductivity measurements during flow experiments in columns with MERIT |
| 12:40
- 13:00 |
Malekian |
Modified Soil Antecedent Moisture Conditions for Curve Number Method |
| 13:00
- 14:30 |
break |
| 14:30
- 14:50 |
Hajnos |
Pore size distribution of soil under annual and perennial crops from water |
| 14:50
- 15:10 |
Pla-Sentis |
Hydrological properties of disturbed soils in dry-land vineyards of NE Spain |
| 15:10
- 15:30 |
Wessolek |
Interaction between elevated
CO2, nitrogen impact and groundwater recharge under climate change conditions |
| 15:30
- 15:50 |
Dörner |
Water flow in soilslopes under ecological and conventional
management (Full Paper) |
| 15:50
- 16:10 |
Schindler |
Hydrological evaluation of peat soil development |
| 16:10
- 16:40 |
break |
| 16:40
- 17:00 |
Einecke |
Spatial distribution and physical properties of a lignitic mine soil for |
| 17:00
- 17:20 |
Hurraß |
Water repellency in soils a consequence of SOM
properties? |
| 17:20
- 17:40 |
Pochet |
Excessive drainage in fine clayey soils rich in high charge halloysite |
| 17:40
- 18:00 |
Zamboni |
Water reuse in Po Plain |
