wk1 thermal balance and pathophysiology Flashcards
what is the formula for heat storage
S = M - W +- E +- C +- R +- K (all in ‘W. m^-2’ watts per square meter)
M - metabolic energy production
w - work done
e - evaporative heat transfer
c - convective heat transfer
r - radiative heat transfer
k - conductive heat transfer
what is the formula of heat storage also referred to as
the 1st law of thermodynamics
what are the 4 main environmental parameters affecting heat balance
ambient temp
humidity - diffusion gradient reduced when it’s very humid
air velocity
solar radiation
what personal factors affect heat balance
age
biological sex
body surface area
aerobic fitness
what are the task dependant factors affecting heat balance
rate of metabolic heat production
clothing
what measures the total heat generation and exchange
whole body calorimeters
what is another example of how we can measure body heat storage and exchange
thermometry
on a graph depicting heat loss and production how would you find the ‘whole body heat storage’
it’s the shaded area between the two values
what are the efferent responses to cold temps
blood vessels constrict
shivering
what is the efferent response to high temps
blood vessels dilate to produce sweat
what locations do we measure body core temp
oesophageal - mouth (most accurate)
rectal - anus
gastro intestinal - from mouth to anus (moving blood away from gut during exercise so is slow)
tympnic - ear canal
what is the thermoeffector response during heat stress
body temp spikes
effector output increases proportionally to body temp (plateaus at max value)
body temp change is needed to cause effector output
how is skin (cutaneous) temp different to core
skin can vary around the body core is always the same, it is not regulated
how do we measure skin temp
Has to be at a min of 4 sites
infared thermography - measures radiating energy released from the body
thermocouples - connected wires attached to the body
ibuttons - small metallic buttons placed on the body
what is the sweating response across time
steep rise to own plateau - no uniformity in sweat rates
decline local - due to hidromeiosis (reduction of sweating occurring when sweat glands are blocked)
decline central - osmoregulatory and baroreceptive
what is vital about sweat loss through evaporation
humans can only dissipate heat from skin if environmental temp > skin temp