Catoctin/Fauquier contact

Catoctin/Fauquier contact
Power washing a quarry block near Aldie, VA that preserves a soft sediment contact of the Fauquier Formation cap carbonate and pillow basalt of the Catoctin Formation.

Thursday, February 17, 2011

Isotope Partition Function ("The Urey Equation")


The partition function for determining equilibrium isotope fractionation factors as formulated by Urey (1947) for diatomic molecules (sometimes called the "Urey Equation"):
Where,

σ = symmetry number for molecule
I = moment of inertia for molecule
M = molecular mass
h = Planck's Constant
c = Speed of Light
ω = vibrational frequency
k = Boltzmann's Constant
T = Temperature

The subscripts 1 and 2 refer to two isotopologues that are undergoing an isotope exchange reaction.   

Isotopologue definition: Molecules that differ from one another only in isotopic composition, e.g., C16O and C18O.

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