mollwollfumble said:
Two comments. How do you tune a laser? And I don’t see why isotope ratio would be expected to correlate with formation temperature.
I can’t help with the laser question, sorry.
Different stable isotopes of an element have very slightly different chemical and physical properties because of their mass differences. For elements of low atomic number, the mass differences are sufficiently large for physical, chemical, and biological processes to “fractionate” or change the relative proportions of various isotopes.
Stable isotope fractionation is a well-researched tool. Oxygen isotope fractionation is a common paleothermometer in geochemistry (eg paleoclimate inferences from oxygen isotopes preserved in ice cores). Carbon isotope fractionation used as a biogenic-or-not separation tool.
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For example, from:
http://en.wikipedia.org/wiki/Kinetic_fractionation
A naturally occurring example of kinetic fractionation is the evaporation of seawater to form clouds. In this instance, isotopically lighter water molecules (i.e., those with 16O) will evaporate slightly more easily than will the isotopically heavier water molecules with 18O.
Heavier isotopes favor the less energetic liquid phase of water during evaporation and condensation. Water vapor is enriched with light isotopes relative to sea water. Clouds are depleted of light isotopes relative to water vapor. This results in higher latitude waters being isotopically “light”. As water vapor is driven poleward by Earth’s energy budget and rotating Hadley cells, the heavy isotopes are left behind as clouds and rain.
During this process the oxygen isotopes are fractionated: the clouds become enriched with 16O, the seawater becomes enriched in 18O. Thus, rainwater is observed to be isotopically lighter than seawater.
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For some background reading, see below (the first one is a great summary):
http://wwwrcamnl.wr.usgs.gov/isoig/res/funda.html
http://en.wikipedia.org/wiki/Isotope_fractionation
http://en.wikipedia.org/wiki/Equilibrium_fractionation
http://en.wikipedia.org/wiki/Kinetic_fractionation