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Comparison of temperature scales. * Normal human body temperature is 36.8 °C ±0.7 °C, or 98.2 °F ±1.3 °F. The commonly given value 98.6 °F is simply the exact conversion of the nineteenth-century German standard of 37 °C. Since it does not list an acceptable range, it could therefore be said to have excess (invalid) precision.
A temperature coefficient describes the relative change of a physical property that is associated with a given change in temperature. For a property R that changes when the temperature changes by dT, the temperature coefficient α is defined by the following equation: Here α has the dimension of an inverse temperature and can be expressed e.g ...
Specific latent heat. L. L = ∂ Q / ∂ m {\displaystyle L=\partial Q/\partial m} J⋅kg −1. L 2 T −2. Ratio of isobaric to isochoric heat capacity, heat capacity ratio, adiabatic index, Laplace coefficient. γ. γ = C p / C V = c p / c V = C m p / C m V {\displaystyle \gamma =C_ {p}/C_ {V}=c_ {p}/c_ {V}=C_ {mp}/C_ {mV}} 1.
The Van 't Hoff equation relates the change in the equilibrium constant, Keq, of a chemical reaction to the change in temperature, T, given the standard enthalpy change, ΔrH⊖, for the process. The subscript means "reaction" and the superscript means "standard". It was proposed by Dutch chemist Jacobus Henricus van 't Hoff in 1884 in his book ...
Thermochemical equation. In thermochemistry, a thermochemical equation is a balanced chemical equation that represents the energy changes from a system to its surroundings. One such equation involves the enthalpy change, which is denoted with Δ H. In variable form, a thermochemical equation would appear similar to the following:
Most scientists measure temperature using the Celsius scale and thermodynamic temperature using the Kelvin scale, which is the Celsius scale offset so that its null point is 0 K = −273.15 °C, or absolute zero. Many engineering fields in the US, notably high-tech and US federal specifications (civil and military), also use the Kelvin and ...
Relations. The laws of thermodynamics imply the following relations between these two heat capacities (Gaskell 2003:23): A corresponding expression for the difference in specific heat capacities (intensive properties) at constant volume and constant pressure is: where ρ is the density of the substance under the applicable conditions.
ΔT (timekeeping) the difference between two time scales, Universal Time and Terrestrial Time, which results from a drift in the length of a day. The interval of time used in determining velocity. The increment between successive nerve impulses.