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Dissipation and the so-called entropy production
Dissipation and the so-called entropy production

... In these equations Fe is an external dissipative field (e.g. an electric field applied to a molten salt), the scalars Ci and Di couple the system to the field. The system can easily be generalized to tensor coupling parameters if required. If we denote a set of thermostatted particles as belonging t ...
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... exterior atmosphere transverse to the direction of conduction. Biot’s starting point was Newton’s law of cooling, according to which the rate at which a body loses heat to its surroundings is proportional to the difference in temperature between the bar and the exterior atmosphere. Biot, who was a s ...
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... physics. Originally described as weakly interacting, massless particles in the standard model of particle physics, it took more than 40 years from their first experimental observation until the discovery of neutrino oscillations in 1998 [Fuk98] showed that neutrinos must indeed be massive particles. ...
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... pressure drop of the hydrogen. Control volumes CVref,1..N and CVhyd,1..N exchange only heat i.e no exchange of work or mass. The heat exchange rate relation is derived by applying a first law energy balance to CVtot . This is seen in (3). The needed U A value is determined using (4) which is derived ...
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Heat



In physics, heat is energy in a process of transfer between a system and its surroundings, other than as work or with the transfer of matter. When there is a suitable physical pathway, heat flows from a hotter body to a colder one. The pathway can be direct, as in conduction and radiation, or indirect, as in convective circulation.Because it refers to a process of transfer between two systems, the system of interest, and its surroundings considered as a system, heat is not a state or property of a single system. If heat transfer is slow and continuous, so that the temperature of the system of interest remains well defined, it can sometimes be described by a process function.Kinetic theory explains heat as a macroscopic manifestation of the motions and interactions of microscopic constituents such as molecules and photons.In calorimetry, sensible heat is defined with respect to a specific chosen state variable of the system, such as pressure or volume. Sensible heat transferred into or out of the system under study causes change of temperature while leaving the chosen state variable unchanged. Heat transfer that occurs with the system at constant temperature and that does change that particular state variable is called latent heat with respect to that variable. For infinitesimal changes, the total incremental heat transfer is then the sum of the latent and sensible heat increments. This is a basic paradigm for thermodynamics, and was important in the historical development of the subject.The quantity of energy transferred as heat is a scalar expressed in an energy unit such as the joule (J) (SI), with a sign that is customarily positive when a transfer adds to the energy of a system. It can be measured by calorimetry, or determined by calculations based on other quantities, relying on the first law of thermodynamics.
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