A model for Evaporation and Drainage investigations at Ground of Ordinary Rainfed-areas
Mehmet Aydin
Ecological Modelling, 2008, vol. 217, issue 1, 148-156
Abstract:
Quantification of water losses through evaporation and drainage from bare soils in arid and semi-arid regions is very important for an effective management strategy to conserve soil water. In this study, a model for Evaporation and Drainage investigations at Ground of Ordinary Rainfed-areas (hereafter E-DiGOR) is presented. Daily potential evaporation (Ep) from bare soils was calculated using the Penman–Monteith equation with a surface resistance of zero. Actual soil evaporation (Ea) was computed according to Aydin et al. [Aydin, M., Yang, S.L., Kurt, N., Yano, T., 2005. Test of a simple model for estimating evaporation from bare soils in different environments. Ecol. Model. 182 (1), 91–105; Aydin, M., Yano, T., Evrendilek, F., Uygur, V., 2008. Implications of climate change for evaporation from bare soils in a Mediterranean environment. Environ. Monit. Assess. 140, 123–130]. Deep drainage (D) was simply calculated by the mass balance, taking field capacity into account. In order to test the performance of the model mainly for drainage estimations, a micro-lysimeter-experiment was carried out under field conditions. The experimental terrain was nearly flat, with no appreciable slope. Estimated and measured water balance components such as actual evaporation (R2=91.4%; P<0.01), drainage (R2=88.5%; P<0.01) and soil water storage (R2=89.7%; P<0.01) were in agreement. This agreement supported the model hypothesis, thus rendering the model useful in estimating soil evaporation, drainage and water storage in an interactive way with a few parameters.
Keywords: Arid environment; Rainfed-areas; Soil evaporation; Drainage; Modelling (search for similar items in EconPapers)
Date: 2008
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Citations: View citations in EconPapers (2)
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Persistent link: https://EconPapers.repec.org/RePEc:eee:ecomod:v:217:y:2008:i:1:p:148-156
DOI: 10.1016/j.ecolmodel.2008.06.015
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