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calorimetry as a primary or direct way to measure quantity of energy transferred as heat. It relies on temperature as one of its primitive concepts, and used in calorimetry. It is presupposed that enough processes exist physically to allow measurement of differences in internal energies. Such processes are not restricted to adiabatic transfers of energy as work. They include calorimetry, which is the commonest practical way of finding internal energy differences. The needed temperature can be either empirical or absolute thermodynamic. Like thermodynamic work, heat transfer is a process involving more than one system, not a property of any one system. In thermodynamics, energy transferred as heat contributes to change in the system’s cardinal energy variable of state, for example its The hottest product flower and horse all over printed slippersinternal energy, or for example its enthalpy. This is to be distinguished from the ordinary language conception of heat as a property of an isolated system. The Sun and Earth form an ongoing example of a heating process. Some of the Sun’s thermal radiation strikes and heats the Earth. Compared to the Sun, Earth has a much lower temperature and so sends far less thermal radiation back to the Sun. The heat of this process can be quantified by the net amount, and direction , of energy it transferred in a given period of time. Conduction transfers heat energy in solids. The

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