Stable Isotopes Flashcards
(31 cards)
Delta Notation
- Means of expressing the relative abundance of the heavier stable isotope in a mixture of atoms
- units are per mil
d = (Rsample/Rstandard-1)*1000 R = molar ratio of heavy-to-light isotope (ex: 13C/12C)
Founding Fathers of Isotope Ecology
Tom Hoering (Carnegie), Harmon Craig (Scripps), Harold Urey (U of Chicago), Sam Epstein (Caltech)
Hutchinson’s ecological niche
n-dimensional set of points in a space whose axes represent environmental variables
Electron
tiny subatomic particle with negative charge
proton
subatomic particle with a positive charge
Neutron
Subatomic particle with no charge. Similar mass to protons
Atomic Number (Z)
Integer that expresses the number of protons in the nucleus
Mass Number (A)
The sum of protons and neutrons in a nucleus
Atomic Mass
The mass of a neutral, noncharged, atom of a nuclide
Atomic Mass Unit (AMU)
A measure of atomic mass
1 AMU = 1/12 mass of 12C
Radioactive Decay
Decay of an element to a different form with a more stable energy configuration
Half-Life
Time required for one half of the atoms in a sample of a radioactive isotope to decay
Isotopes
Atoms which have the same number of protons in their nuclei, but different numbers of neutrons
Isotopologues
Isotopic species of the same molecule
Carbon dioxide has 12 isotopologues: 12C16O16O, 12C16O17O, etc
Isotopomers
Isotopologues that differ from one another only in the position of the isotopic elements
International Reference Standard for Hydrogen
V-SMOW, Vienna Standard Mean Ocean Water
International Reference Standard for Oxygen
V-SMOW, Vienna Standard Mean Ocean Water
V-PDB, Vienna Pee Dee Belemnite
International Reference Standard for Carbon
V-PDB, Vienna Pee Dee Belemnite
International Reference Standard for Nitrogen
Air, Atmospheric Air
Fractionation
Isotopic separation/sorting
Isotopes of the same element undergo the same chemical reactions because they have the same protons and electrons. Isotopes have different thermodynamic properties due to their different masses (melting point, vapor pressure, diffusion coefficient, and equilibrium and kinetic rate constants). Thus, different isotopes react at different rates in chemical reactions, which leads to fractionation.
Results of fractionation
abundance of heavy isotopes in the reactant being different from the abundance of heavy isotopes in the product
lighter goes faster
Isotopic fractionation factor (alpha)
alpha = (1000 +delta of reactant)/(1000+delta of product)
Exchange - Equilibrium Fractionation
- equilibrium
- complete back-reactions occur
- product/reactant offset by constant fractionation factor
- physical state changes (water to vapor)
- chemical transformations (carbonic acid to carbon dioxide and water)
ex: liquid droplet formation from vapor in clouds, evaporation at the boundary layer (100% RH) of body of water
Transport/Diffusive Fractionation
- non-equilibrium
- kinetic fractionation dealing with flux rather than chemical reaction
- incomplete back-flux is the rule
ex: diffusion through boundary layer over water, out of leaves, through soils