Comparison of methods for determining unsaturated hydraulic conductivity in the wet range to evaluate the sensitivity of wetting front detectors
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1 janvier 2012
- handle: 10670/1.wx97vf
Mots-clés
inverse modelling instantaneous profile method pedotransfer functions wetting front detector field capacity HYDRUS-2DSujets proches
Instruction and study--Methods Instruction and study--MethodsCiter ce document
GT Adhanom et al., « Comparison of methods for determining unsaturated hydraulic conductivity in the wet range to evaluate the sensitivity of wetting front detectors », Water SA, ID : 10670/1.wx97vf
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Résumé
The design of passive lysimeters or wetting front detectors determines the tensions at which they collect a water sample from an unsaturated soil. When deployed in the field to help manage irrigation, it is necessary to know the minimum flux of water that can be sampled by a passive lysimeter and how this relates to the drainage flux at field capacity. This requires a good estimate of the unsaturated hydraulic conductivity characteristic, K (h), in the wet range (< 10 kPa). We compared various field, laboratory and theoretical approaches for obtaining the K (h) function and compared these to a reference K (h) function derived by applying inverse modelling approaches to field drainage experimental data. The Van Genuchten model and three of the pedotransfer models produced K (h) functions with a root mean square error of less than 5% compared to the reference, and appear to be simple methods of obtaining a reasonable estimate of unsaturated hydraulic conductivity. However, despite the goodness of fit, there can be a 10-fold difference in conductivity at a given tension < 10 kPa estimated from the different methods. Moreover, water content at field capacity depends entirely on whether field capacity is defined as time elapsed after saturation, a set tension or a minimum flux.