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  2. Ray (TV series) - Wikipedia

    en.wikipedia.org/wiki/Ray_(TV_series)

    Ray is an Indian anthology drama television series on Netflix created by Sayantan Mukherjee, based on the works of Satyajit Ray. The series is directed by Srijit Mukherji , Vasan Bala and Abhishek Chaubey .

  3. Cosmic ray - Wikipedia

    en.wikipedia.org/wiki/Cosmic_ray

    The magnitude of the energy of cosmic ray flux in interstellar space is very comparable to that of other deep space energies: cosmic ray energy density averages about one electron-volt per cubic centimetre of interstellar space, or ≈1 eV/cm 3, which is comparable to the energy density of visible starlight at 0.3 eV/cm 3, the galactic magnetic ...

  4. Ray Ntlokwana - Wikipedia

    en.wikipedia.org/wiki/Ray_Ntlokwana

    Mvuyiswa Renek “Ray” Ntlokwana (5 May 1937 – 20 July 2000) [1] was a South African actor from Gugulethu, who was affectionately known as “Velaphi” following his lead role in the SABC Xhosa comedy, Velaphi, a name he was associated with throughout his career.

  5. Heat-transfer fluid - Wikipedia

    en.wikipedia.org/wiki/Heat-transfer_fluid

    Heat Capacity: A fluid’s heat capacity indicates how much thermal energy it can transport and store, impacting the efficiency of the heat transfer process. [ 2 ] Thermal Conductivity and Thermal Diffusivity : These properties influence the rate at which heat is transferred through the fluid, affecting how quickly a system can respond to ...

  6. Enthalpy of neutralization - Wikipedia

    en.wikipedia.org/wiki/Enthalpy_of_neutralization

    The enthalpy change for this reaction is -57.62 kJ/mol at 25 °C. For weak acids or bases, the heat of neutralization is pH-dependent. [1] In the absence of any added mineral acid or alkali, some heat is required for complete dissociation. The total heat evolved during neutralization will be smaller.

  7. Earth's internal heat budget - Wikipedia

    en.wikipedia.org/wiki/Earth's_internal_heat_budget

    Most of the heat flow from the thicker continental crust is attributed to internal radiogenic sources; in contrast the thinner oceanic crust has only 2% internal radiogenic heat. [2] The remaining heat flow at the surface would be due to basal heating of the crust from mantle convection. Heat fluxes are negatively correlated with rock age, [1 ...

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