Unsaturated zone flow and solute transport modelli

Authors: Christian Reszler Johann Fank

Publish Date: 2016/01/25

Volume: 75, Issue: 3, Pages: 253-

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Abstract

This study presents the test of the widely used model MIKE SHE at the lysimeter in Wagna in Southern Styria Austria At the lysimeter comprehensive data of vegetation ie cultivation types and soil hydraulic properties are available to parameterise the model The aim of the study is to test the water movement and solute transport simulation in the unsaturated zone and the evapotranspiration module by a comparison with measured recharge rates at the lysimeter bottom and measured soil water contents and soil tensions in different depths For the unsaturated zone calculation the Richards equation and the Van Genuchten–Mualem approach is used With the parameterised model the solute transport module is tested against data of a tracer experiment Bromide The water content simulation in the different soil depths yielded good results However particularly in the gravel zone below 70 cm the strong recharge dynamics and at the same time also strong water content dynamics can hardly be reproduced by one individual soil physical parameter set Two different sets were identified and the corresponding soil water retention functions are located at the opposite ends of the relatively large range obtained by the measurements in this zone Also the saturated hydraulic conductivity had to be increased by an order of magnitude to accurately represent the recharge dynamics The test of the solute transport simulation showed generally very good results However the early rapid rise of the measured concentrations could not be reproduced with either parameter set The discrepancies found in the study indicate a complex pore system in the gravel zone consisting of different flow paths eg system of matrix flow and macropore flow activated at different soil moisture conditions which cannot be fully represented by the used approach However the parameter study herein highlights the main parameters to be altered in a calibration procedure at point scale The paper includes also a step from point to regional scale For comparison test calculations with data which are usually available on regional scale showed good results for the 5year average balance −7  compared to measurements but rather large deviations from the measurements at shorter time scalesThe authors would like to thank the anonymous reviewers for their valuable comments on the manuscript Franz Feichtinger from the Institute for Land and Water Management Research of the Austrian Federal Agency for Water Management Bundesamt für Wasserwirtschaft in Petzenkirchen/Austria is acknowledged for providing the comprehensive soil physical laboratory measurements The Bromide analytics were carried out in the environmental laboratory at Joanneum Research Gernot Klammler is thanked for numerous suggestions for the manuscript

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