Normal physiological range for core body temperature
37celcius0.6 +-
Conduction
is the transfer of heat from one object to another through direct contact
convection
the transfer of heat through air or water movement
Radiation
heat loss through transfer of energy waves sent by one object and absorbed by another
body absorbs radiant heat energy when the temperature of the environment is higher than skin temperature
Evaporation
conversion of sweat from liquid to gas/water vapour
maximal evaporative heatless from the body occurs when sweat is vaporised from the skin
Significance of humidity and wind in relation to body heat loss
Humidity:
- dry air receives vaporised sweat readily
- wet air receives little evaporated sweat because it is already heavily laden with moisture
Heat Cramps
Causes: intense/prolonged exercise in the heat, muscle fatigue, sodium loss in sweat
Symptoms: pain, involuntary spasms of active muscles. low sodium
Heat Syncope
Causes: peripheral vasodilation and pooling of venous blood, hypotension. hypohydration
Symptoms: light headedness, partial loss of consciousness, pale, high core temperature
Heat exhaustion
Causes: increasing negative water balance
Symptoms: fatigue, loss of coordination, dizzy pale, reduced sweating, high core temperature
Heath Stroke
Causes: Thermoregulatory failure, dehydration
Symptoms: core temp is above 41, lack of sweating, seizures, twitching
steps to prevent heat related disorders
Acclimatise: 5 to 10 days
Rehydrate
Massage/stretching
Immediate who body cooling
adapt activities to climatic constraints
Heat Acclimatisation
Perform trading sessions in similar environmental conditions for 5-10 days
90-100 mins of exercise in heat
Signs of heat acclimatisation during sub-maximal exercise
lower HR
lower core temp
higher sweat rate
Homeostasis
the condition in which the body's internal environment remains relatively constant
Chronic adaptations to exercise in heat
- sweat response increases
- muscle blood flow decreases
- increased lactic acid
- increased plasma volume
- a more dilute sweat composition
- lower electrolyte loss
- earlier onset sweating
- reduced rate of muscle glycogen used
Shivering
contractions of skeletal muscles (involuntary)
Goosebumps
contractions of erector pili muscle (traps the air you radiate)
Peripheral vasoconstriction
decrease in diameter of blood vessels under the skin- more blood at the core
Non-shivering thermogenesis
metabolic rate increases
Exercise in cold
lower HR
Increased SV
Body surface area to body mass ratio
A larger surface area to body mass ratio makes heat loss easier
Children have a larger are to mass ratio
30 to 40% of heat loss is through the head
individuals with greater amount of body fat can retain more heat- more fat less heat loss
Windchill in heat loss
wind increases the rate of heat loss (via convection and conduction) because the warmer insulating air layer surrounding the body continually exchanges with the cooler ambient air
Frostbite
a medical condition in which localised damage is caused to skin due to heat loss
Symptoms: skin is yellow or white, burning sensation, hard