enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Inversion temperature - Wikipedia

    en.wikipedia.org/wiki/Inversion_temperature

    The inversion temperature in thermodynamics and cryogenics is the critical temperature below which a non-ideal gas (all gases in reality) that is expanding at constant enthalpy will experience a temperature decrease, and above which will experience a temperature increase.

  3. Joule–Thomson effect - Wikipedia

    en.wikipedia.org/wiki/Joule–Thomson_effect

    In thermodynamics, the Joule–Thomson effect (also known as the Joule–Kelvin effect or Kelvin–Joule effect) describes the temperature change of a real gas or liquid (as differentiated from an ideal gas) when it is expanding; typically caused by the pressure loss from flow through a valve or porous plug while keeping it insulated so that no heat is exchanged with the environment.

  4. Joule expansion - Wikipedia

    en.wikipedia.org/wiki/Joule_expansion

    At temperatures below their inversion temperature gases will cool during Joule expansion, while at higher temperatures they will heat up. [ 5 ] [ 6 ] The inversion temperature of a gas is typically much higher than room temperature; exceptions are helium, with an inversion temperature of about 40 K, and hydrogen, with an inversion temperature ...

  5. Thermodynamic temperature - Wikipedia

    en.wikipedia.org/wiki/Thermodynamic_temperature

    Thermodynamic temperature is a quantity defined in thermodynamics as distinct from kinetic theory or statistical mechanics.. Historically, thermodynamic temperature was defined by Lord Kelvin in terms of a macroscopic relation between thermodynamic work and heat transfer as defined in thermodynamics, but the kelvin was redefined by international agreement in 2019 in terms of phenomena that are ...

  6. Inversion (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Inversion_(meteorology)

    In meteorology, an inversion (or temperature inversion) is a phenomenon in which a layer of warmer air overlies cooler air. Normally, air temperature gradually decreases as altitude increases, but this relationship is reversed in an inversion. [2] An inversion traps air pollution, such as smog, near the ground.

  7. Category:Thermodynamic properties - Wikipedia

    en.wikipedia.org/wiki/Category:Thermodynamic...

    Pages in category "Thermodynamic properties" The following 60 pages are in this category, out of 60 total. ... Inversion temperature; L. Latent internal energy; M.

  8. Population inversion - Wikipedia

    en.wikipedia.org/wiki/Population_inversion

    where T is the thermodynamic temperature of the group of atoms, k is the Boltzmann constant and g 1 and g 2 are the degeneracies of each state. Calculable is the ratio of the populations of the two states at room temperature ( T ≈ 300 K ) for an energy difference Δ E that corresponds to light of a frequency corresponding to visible light ...

  9. Redlich–Kwong equation of state - Wikipedia

    en.wikipedia.org/wiki/Redlich–Kwong_equation_of...

    In physics and thermodynamics, the Redlich–Kwong equation of state is an empirical, algebraic equation that relates temperature, pressure, and volume of gases. It is generally more accurate than the van der Waals equation and the ideal gas equation at temperatures above the critical temperature.