JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-GE Geological & Soil Environment

[A-GE39] [EE] Subsurface Mass Transport and Environmental Assessment

Tue. May 23, 2017 10:45 AM - 12:15 PM 301A (International Conference Hall 3F)

convener:Shoichiro Hamamoto(Department of Biological and Environmental Engineering, The University of Tokyo), Yuki Kojima(Gifu University), Hirotaka Saito(Department of Ecoregion Science, Tokyo University of Agriculture and Technology), Yasushi Mori(Graduate School of Environmental and Life Science, Okayama University), Chairperson:Shoichiro Hamamoto(Department of Biological and Environmental Engineering, The University of Tokyo), Chairperson:Yasushi Mori(Graduate School of Environmental and Life Science, Okayama University)

11:35 AM - 11:55 AM

[AGE39-04] Numerical Analysis of Mass and Energy Transport in Subsurface and at the Soil-atmosphere Interface using HYDRUS

*Hirotaka Saito1, Jirka Simunek2, Giuseppe Brunetti3 (1.Department of Ecoregion Science, Tokyo University of Agriculture and Technology, 2.Department of Environmental Sciences, University of California, 3.Department of Civil Engineering, University of Calabria)

Keywords:HYDRUS, Soil-atmospheric interface

It is broadly accepted that mass and energy fluxes in the subsurface in general, and in arid and semi-arid regions in particular, are closely coupled and cannot be evaluated without considering their mutual interactions. While the subsurface processes are commonly implemented in existing models, which often consider both isothermally and thermally induced water and vapor flow, the effects of slope inclination, slope azimuth, variable surface albedo and plant shading on incoming radiation and spatially variable surface mass and energy balance, and consequently soil moisture distribution, are rarely considered. These factors have been recently implemented into the HYDRUS model. In this presentation, the effect of soil heterogeneity and surface roughness on mass and energy fluxes in the subsurface and at the soil-atmosphere interface is evaluated numerically with the HYDRUS model. Additionally, we will demonstrate the use of the HYDRUS model to simulate processes relevant to the ground source heat pump systems.