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## Water SA

*versão On-line* ISSN 0378-4738

#### Resumo

ADHANOM, GT et al. **Comparison of methods for determining unsaturated hydraulic conductivity in the wet range to evaluate the sensitivity of wetting front detectors**.* Water SA* [online]. 2012, vol.38, n.1, pp. 67-76. ISSN 0378-4738.

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.

**Palavras-chave
:
**inverse modelling; instantaneous profile method; pedotransfer functions; wetting front detector; field capacity; HYDRUS-2D.