L2: Heat balance & Clothing Flashcards
What is conduction?
Transfer of heat through direct contact with a solid material
What is convection? and what are the two types of convection?
Movement of air or fluid past the skin which carries heat.
Force: wind
Natural: Heating of air
What is radiation?
Transfer of heat via electromagnetic radiation
What is evaporation?
Transition from a liquid to vapour utilises heat
How does metabolic heat production work?
Energy is required by cells and is utilised in the form of ATP. Majority of the stored energy from ATP is released as HEAT as negligible amount is converted into mechanical work.
What is the heat balance equation?
(M-W) = (K+C+R+Esk) + S
What are the 6 parameters for determining temperature change?
Temperature Vapour pressure Air speed Radiation Clothing Metabolic rate
Dry heat loss formula?
(Temperature of skin - temperature of ambient) / insulation of clothing and air layers
evaporative heat loss formula?
PH2O skin - PH20 ambient / vapour resistance of clothing and air layers.
How does heat loss occur (fundamental principles)
Skin temperature is greater than ambient temperature. The greater the difference the greater the temperature drop.
What is the cross over temperature point in which heat gain occurs?
around 35 degrees
How does temperature and vapour pressure effect evaporative heat loss?
Vapour pressure increases for a given relative humidity when temperature increases. This is due to increased water molecules caused by greater kinetic energy. When vapour pressure increases beyond the vapour pressure of the skin (5 - 6kPa) condensation on the skin occurs.
Why can individuals survive at higher temperatures with a low relative humidity?
Lower relative humidity means a reduction in absolute vapour pressure for a given temperature. This means that a higher temperature can be achieved before ambient vapour becomes higher than that of the skin (5 - 6kPa)
what percentage of heat loss is attributable to respiration?
10%
What is the limit of climate cooling power?
For a given heat production (gain) the ability of the environment to dissipate that heat needs to be equal or greater. The limit of climate cooling power is determined by the difference between the skin temperature and ambient temperature along with the skin vapour pressure and ambient vapour pressure (Evaporative heat loss)