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  2. Felicific calculus - Wikipedia

    en.wikipedia.org/wiki/Felicific_calculus

    Sum up all the values of all the pleasures on the one side, and those of all the pains on the other. The balance, if it be on the side of pleasure, will give the good tendency of the act upon the whole, with respect to the interests of that individual person; if on the side of pain, the bad tendency of it upon the whole.

  3. Stefan problem - Wikipedia

    en.wikipedia.org/wiki/Stefan_problem

    Nanoscale solidification, with variable phase change temperature and energy/density effects are modelled in. [16] [17] Solidification with flow in a channel has been studied, in the context of lava [18] and microchannels, [19] or with a free surface in the context of water freezing over an ice layer.

  4. Excess property - Wikipedia

    en.wikipedia.org/wiki/Excess_property

    The pure component's molar volume and molar enthalpy are equal to the corresponding partial molar quantities because there is no volume or internal energy change on mixing for an ideal solution. The molar volume of a mixture can be found from the sum of the excess volumes of the components of a mixture:

  5. Temperature - Wikipedia

    en.wikipedia.org/wiki/Temperature

    In thermodynamic terms, temperature is an intensive variable because it is equal to a differential coefficient of one extensive variable with respect to another, for a given body. It thus has the dimensions of a ratio of two extensive variables. In thermodynamics, two bodies are often considered as connected by contact with a common wall, which ...

  6. Entropy (classical thermodynamics) - Wikipedia

    en.wikipedia.org/wiki/Entropy_(classical...

    Figure 1. A thermodynamic model system. Differences in pressure, density, and temperature of a thermodynamic system tend to equalize over time. For example, in a room containing a glass of melting ice, the difference in temperature between the warm room and the cold glass of ice and water is equalized by energy flowing as heat from the room to the cooler ice and water mixture.

  7. Thermodynamic beta - Wikipedia

    en.wikipedia.org/wiki/Thermodynamic_beta

    The thermodynamic beta was originally introduced in 1971 (as Kältefunktion "coldness function") by Ingo Müller , one of the proponents of the rational thermodynamics school of thought, [5] [6] based on earlier proposals for a "reciprocal temperature" function. [1] [7] [non-primary source needed]

  8. Thermodynamic temperature - Wikipedia

    en.wikipedia.org/wiki/Thermodynamic_temperature

    A unit increment of one kelvin is exactly 1.8 times one degree Rankine; thus, to convert a specific temperature on the Kelvin scale to the Rankine scale, x K = 1.8 x °R, and to convert from a temperature on the Rankine scale to the Kelvin scale, x °R = x /1.8 K. Consequently, absolute zero is "0" for both scales, but the melting point of ...

  9. Fugacity - Wikipedia

    en.wikipedia.org/wiki/Fugacity

    For an ideal gas, fugacity and pressure are equal, and so φ = 1. Taken at the same temperature and pressure, the difference between the molar Gibbs free energies of a real gas and the corresponding ideal gas is equal to RT ln φ. The fugacity is closely related to the thermodynamic activity. For a gas, the activity is simply the fugacity ...