Isotopes Flashcards
Light isotopes
Isotopes of elements with atomic number below 8
Heavy Isotopes
isotopes of elements with atomic number typically above 70
Stable Isotopes
the number of protons and neutrons in these nuclei will not be modified under any naturally occurring circumstances and processes on earth: their nucleus will remain strictly as it is
Radioactive Isotopes
have unstable nuclei and disintegrate at a constant rate by emitting particles and energy
Radiogenic Isotopes
produced by the disintegration of radioactive isotope
Cosmogenic isotopes
produced by cosmic radiation in the upper reaches of the atm
Kinetic fractionation
dominant fractionation when rapid and nonreversible reacitions occur (evaporation, diffusion)
Caused by difference in diffusion rates between isotopes of the same elements—> due to differences in activation energy between two isotopes of different mass
Lighter elements diffuse faster than heavier ones (products therefore always lighter than reactants
Fractionation
Isotopes of same element will have the same chemical characteristics; however difference in mass will result in slight difference in behaviour, causing different isotopes of the same element to partition between different compounds or phases: fractionation
Equilibrium fractionation
occurs when reversible reactions occur (equilibrium)
Lower extent of fractionation, caused by the difference in bonding energy between isotopes,
Difference in density caused by different mass and therefore bonding energy
Higher mass on isotope = higher dissociation energy (bonding energy)
How is α defined and why is it important?
It is the fractionation factor, defined as the ratio between the isotope ratios in two compounds at equilibrium
quantifies the extent of fractionation
How doe temp affect the fractionation factor
The higher the temperature, the lower the extent of fractionation
What is the “Global Meteoric Water Line” and what is its importance? What are the secondary factors affecting the “Global Meteoritc Water Line”?
d18O versus d2H
- shows how water becomes lighter with each subsequent precipitation
affected by:
- altitude: more depleted heavy isotope with height
- Latitude: depleted more south/north of equator
- Distance from coast: more depleted further from coast
- Amount effect: more precipitation, more depletion of heavy isotope
Rayleigh fractionation
Rayleigh distillation is a process of isotopic fractionation in an open system, where one phase is removed from the system and is no longer in contact and isotopic equilibrium with the other phase
Allows us to quantify the isotopic composition of the two phases at any point of the evaporation processs
How does humidity affect the fractionation of water during evaporation?
more humid environments will produce fractionations closer to that produced at equilibrium as there is more humidity in the air with which the evaporated water can stay in