Absorption test and drying process
Posted: Thu May 14, 2015 3:43 am -1100
Hello,
I am trying to simulate the drying process of a test specimen of stone during two years (200x2000 mm). We considered the following initial conditions: the temperature is T=20ºC and the water content is the free water saturation. We considered the upper surface as a adiabatic border, lateral surfaces with a climate of T=20ºC and HR=60% and the bottom surface with a climate of T=20ºC and HR=90% during two years.
As you can see in the attached file, after two years of drying out (simulation), the outside part of the specimen is dry but not the inside inside part (figures on the right) (20cm_OL_v3.zip).
Then, we only changed the climatic conditions of the bottom surface to simulate that it is in direct contact with an infinite source of water using a .kli file (clima_hum_asc.kli is in each simulation folder):
$WUFI$ 1.1.1991_0.00 - 1.1.1992_0.00
Azimut : 0 º, Inclination : 0 º, Abgeleitet von ibp1991.wet
1000
8760 1000 0 16 1 16 1
But, as you can see in the attached figure, the drying process are very different because in this case the inside part after two years is completely dry (figures on the left) (20cm_OL_v1.zip), why? which is the reason? We just copy the simulation and change this surface boundary condition. There is something wrong in the .kli file?
Is it a simulation error due to material because the slope of the Moisture Storage Function is very high for values near to 100% of HR?
Thanks,
I am trying to simulate the drying process of a test specimen of stone during two years (200x2000 mm). We considered the following initial conditions: the temperature is T=20ºC and the water content is the free water saturation. We considered the upper surface as a adiabatic border, lateral surfaces with a climate of T=20ºC and HR=60% and the bottom surface with a climate of T=20ºC and HR=90% during two years.
As you can see in the attached file, after two years of drying out (simulation), the outside part of the specimen is dry but not the inside inside part (figures on the right) (20cm_OL_v3.zip).
Then, we only changed the climatic conditions of the bottom surface to simulate that it is in direct contact with an infinite source of water using a .kli file (clima_hum_asc.kli is in each simulation folder):
$WUFI$ 1.1.1991_0.00 - 1.1.1992_0.00
Azimut : 0 º, Inclination : 0 º, Abgeleitet von ibp1991.wet
1000
8760 1000 0 16 1 16 1
But, as you can see in the attached figure, the drying process are very different because in this case the inside part after two years is completely dry (figures on the left) (20cm_OL_v1.zip), why? which is the reason? We just copy the simulation and change this surface boundary condition. There is something wrong in the .kli file?
Is it a simulation error due to material because the slope of the Moisture Storage Function is very high for values near to 100% of HR?
Thanks,