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Simulations of coupled non-isothermal soil moisture transport and evaporation fluxes in a forest area

Publikace na Přírodovědecká fakulta |
2017

Tento text není v aktuálním jazyce dostupný. Zobrazuje se verze "en".Abstrakt

This study focuses on the quantification of non-isothermal soil moisture transport and evaporation fluxes in vegetated area. A one-dimensional numerical model is developed by integrating a multi-phase flow model with a twolayer energy-balance model.

The non-isothermal multi-phase flow model solves four governing equations for coupled air, vapour, moisture, and heat transport in soil porous medium. The two-layer energy balance model estimates evaporation fluxes from transpiration, interception, and soil surface.

The model was implemented to an oak forest area in Missouri, USA. For model calibration and validation, measurements of energy fluxes, soil moisture, and soil temperature were used.

The proposed model is compared with a simple model that couples the Penman-Monteith equation with the Richards' equation. The results indicate that the simple model underestimate the total evaporation rate.