<abstract xmlns="http://www.w3.org/1999/xhtml"><p> 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. On the contrary, the proposed model includes a more detailed description of energy transfer, which could improve the accuracy in estimating evaporation rates. The proposed model could be a promising tool to quantify the energy and moisture fluxes in a soil-vegetation-atmosphere continuum in vegetated area.</p></abstract>

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. On the contrary, the proposed model includes a more detailed description of energy transfer, which could improve the accuracy in estimating evaporation rates. The proposed model could be a promising tool to quantify the energy and moisture fluxes in a soil-vegetation-atmosphere continuum in vegetated area.

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

Journal of Hydrology and Hydromechanics

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

This study focuses on the quantification of non-isothermal soil moisture transport and evaporation fluxes in vegetated area. A one-dimensional numerical model...

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

Publicado en línea: 07 nov 2017

Páginas: 410 - 425

Recibido: 20 abr 2016

Aceptado: 11 feb 2017

DOI: https://doi.org/10.1515/johh-2017-0038

Palabras clave
Soil-vegetation-atmosphere transfer model, Evaporation flux, Soil moisture transport, Forest meteorology

© 2017

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

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

Publicado en línea: 07 nov 2017

Páginas: 410 - 425

Recibido: 20 abr 2016

Aceptado: 11 feb 2017

DOI: https://doi.org/10.1515/johh-2017-0038

Palabras claveSoil-vegetation-atmosphere transfer model, Evaporation flux, Soil moisture transport, Forest meteorology

© 2017

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Palabras clave
Soil-vegetation-atmosphere transfer model, Evaporation flux, Soil moisture transport, Forest meteorology