The general equation for converting from one scale to another is given by where the subscript L and U represent the lower fixed point and the upper fixed points respectively on scale of reference.
Fourier’slaw of heat transfer states that the heat transfer rate through a surface is the product of the temperature difference across the surface and the thermal conductivity of the material.
Conduction is the form of heat transfer in solids where one end of a solid is in contact with a heat source, the atoms gain thermal energy and begin to vibrate from their sites, causing heat to gradually transfer to the colder end.
The zeroth law of thermodynamics states that if bodies A and B are separately in thermal equilibrium with a third body C, then they are in thermal equilibrium with each other.
Heat is a form of energy in transit and when two bodies that are at different temperature come in contact, there will be a spontaneous movement of heat from the body with higher temperature to a body with lower temperature and not vice-versa except work is done on the system.
Convection is the mode of heat transfer in fluids, i.e., liquids and gases, where the layer of fluid nearest the heat source absorbs heat energy, expands and moves up to be replaced by a colder layer which in turn absorbs heat energy, and the process continues until all the fluid gets heated up.
The first law of thermodynamics states that if an amount of heat flows into a system, then this energy must appear as increased internal energy for the system and/or work done by the system on its surroundings.
The quantity Q-W is the same for all processes and depends only on the initial and final states and does not depend at all on how the system gets from one to the other.
For an ideal gas changing from conditions (P 1 V 1 T 1 ) to (P 2 V 2 T 2 ) in an adiabatic process then and where is the ratio of specific heat at constant pressure to that at constant volume.