Table of contents
Comments from Alex Klein-Paste
I see.
You probably know already that the cooling of any object comes from three main heat fluxes: conduction, convection and radiation. In addition you have phase changes like evaporation that require large amount of latent heat.
Thin aluminium rescue blanket work mainly to reduce radiative losses by changing the surface properties of the object (more specifically the emissitivity).
When you are outdoors and have a clear sky the temperature of the sky (basically the temperature of the atmosphere is very low (point an IR thermometer at nighttime to a clear sky and you will read probably between -40 and -70 degrees C.
In the lab however, your sky is the ceiling and walls of the lab. These are at the same temperature as the air and very close to the outer surface of your object.
So the lab is not a good place to investigate the loss of heat by radiation.
Now you still can investigate the effect of convection (heat exchange with the air) and the effects of evaporation. But mind that some differences from a real-life situation and the lab will exist due to this lack of radiative cooling.
Alex
Test
Using a maniking/patient simulator to evaluate the effect of wet clothing removal on skin temperature in subjects exposed to cold.
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Dry Group
30 minutes cooling (Phase 1):
2 minutes exposure time:
Removal of clothing.
→ →
Insulating in bubble wrap, cotton blanket and thermal blanket.
→ →
30 minutes heating after insulating (Phase 2):
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Wet Group
30 minutes cooling (Phase 1):
2 minutes insulating time:
→ →
→ →
30 minutes heating after insulating (Phase 2):
Pulse:
Interval average:
Temperature diff:
Temperature rate:
[°C/min]
[°C/s]
Note: Reason for selecting cubic spline interpolation with boundary conditions