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Lecture25-12
Lecture25-12

... Q = mLf = (1000 g)  (80 cal/g) = 80,000 cal How much heat can the water deliver by cooling from 50°C to 0°C? Q = cwater m x T = (1 cal/g °C)  (1000 g)  (50°C) = 50,000 cal Thus, there is not enough heat available to melt all the ice!! Follow-up: How much more water at 50°C would you need? ...
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Heat transfer



Heat transfer is the exchange of thermal energy between physical systems, depending on the temperature and pressure, by dissipating heat. The fundamental modes of heat transfer are conduction or diffusion, convection and radiation.Heat transfer always occurs from a region of high temperature to another region of lower temperature. Heat transfer changes the internal energy of both systems involved according to the First Law of Thermodynamics. The Second Law of Thermodynamics defines the concept of thermodynamic entropy, by measurable heat transfer.Thermal equilibrium is reached when all involved bodies and the surroundings reach the same temperature. Thermal expansion is the tendency of matter to change in volume in response to a change in temperature.
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