Geological Time and Radiometric Dating Flashcards
What are the two numbers which specify an element?
Atomic Number Z - specifies element
Atomic Mass A - specifies isotope
What happens to the atomic number and the atomic mass in alpha decay?
Z -> Z-2, A-> A-4
What happens to the atomic number and the atomic mass in beta decay?
Z -> Z+1, A -> A
What is the equation for the number of nuclei over time?
N(t) = N(0)*exp(-λt)
What is the equation for an atoms half life?
T(1/2) = ln(2)/λ
What are the 4 steps in the formation of the Earth?
1-Nebular dust gathers and begins to collapse
2-Protostar forms out of gas, and planetesimals form out of dust, as cloud condenses into pancake shape
3-Planetesimals grow to about 1000km and star is formed
4-Accretion of planetesimals by collision causes growth of larger bodies
How long does this process take approximately?
~10^8 years.
What are the three sources of heat during the planet formation?
- Kinetic energy from collisions
- Gravitational contraction
- Radioactivity, decay processes
What happens if the heat generation in a planet is more than the heat escape?
The planet turns molten.
What happens if a planet turns molten?
Heavier elements pull to the centre, and the iron catastrophe happens!
What happens in the iron catastrophe? (3 steps)
- Heat melts Fe
- Dense molten Fe falls towards core
- Releases G.P.E
What can we use the iron catastrophe for with the Earth?
Whole planet at some point was a molten rock, so everything was mixed up with equal isotopes everywhere. Can use this as time 0 for our rock dating.
What is the definition of a rock?
A rock is a mixture of minerals, possibly with organic and inorganic constituents.
What is the definition of a mineral?
Naturally occurring inorganic substance, with well defined crystal structure. Impurities often present, useful for radiometric dating.
What is the method of radiometric dating?
- Exploit radioactive decay of an element with known decay constant
- Take sample from rock of specific mineral
- Use mass spectrometer to measure ratios between different isotopes