Equilibrium thermodynamics contrasts from non-balance thermodynamics, in that, with the last, the condition of the framework under scrutiny will normally not be uniform but rather will shift locally in those as vitality, entropy, and temperature circulations as slopes are forced by dissipative thermodynamic fluxes. In balance thermodynamics, the condition of the framework will be viewed as uniform all through, characterized visibly by those amounts as temperature, weight, or volume.
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