Lecture 4 Flashcards
What is a use of radioactive isotopes in particular 14C
- Radiochemical dating
What C isotopes does all organic matter contain
- All organic matter contains 12C and 13C as well as 14C which is continuously being created by cosmic radiation in the thermosphere
How is 14C formed and what does it decay to
- 14N + 1n –> 14C + 1H
- 14C –> 14N + beta-
How does radiochemical dating work
- Whilst plant or animal is alive it will have the same proportion of 14,6C as the surroundings
- When the plant or animal dies the intake of radiocarbon stops and that already present gradually decays
- Thus the smaller A is, the longer the period between death and the present time
What are some assumptions made in carbon dating
- 14C production is constant and equally spread
- Exchange has stopped- microorganisms etc
What do radio-dating methods require
- Measurement of amount of radio-isotope now
- Knowledge or good assumption of the amount of radio-isotope present at the time to be date
- Time elapsed can be calculated based on decay laws- since t1/2 is known, need to measure activity
How can you carry out radiochemical dating of geological samples
- Requires isotope decays with very long half-lives
- 3 options
- Use of decay series of 238U to 206Pb
- Use of 87Rb–> 87Sr + Beta- :date lunar samples
- Decay of 40K to 40Ar by electron capture
How does the use of decay series of 238U to 206Pb work for dating
- Analyse U minerals for their U/Pb ratio
- e.g. if find 1:1 ratio and assume no Pb present at start then 1 half life has passed- 4.5 billion years old (approx age of earth)
- Useful as half life is close to age of earth- but not very abundant
How does the use of Decay of 40K to 40Ar by electron capture work for dating
- 40K/40Ar ratio determined by mass spectrometer
- Method assumes that all of the argon is trapped in the rock after it has cooled
What needs to be thought about when carrying out radiodating
- Events such as nuclear testing
- Released neutrons into atmosphere
- Made 14C
- Not reliable carbon dating for this time
How is radiation detected
- Electrical collection of ions
- Scintillation
Describe how radiation is detected by electrical collection of ions
- Air ionisation- no gas amplification uses air
- Gas ionisation- (Geiger-Muller counter)
- GM is most common type of detector
- Gas amplification
- Multiplication factor 10^8-10^10
- Long dead time after excitation
Describe how radiation is detected by scinitillation
- Light production
- Liquid Scintillation Counter (Lsc):
- Low energy beta and alpha
- Solvent mixed with scintillating material
- Very low background
- Much more sensitive - both tubes must be activated at the same time
Describe nuclear applications in analysis
- Neutron activation analysis
- Mossbauer spectroscopy
- Nuclear spectroscopy
Describe neutron activation analysis
- Bombard sample with neutrons leads to unstable nucleus- produces gamma rays which can be measured
- The wavelength of the gamma-rays are characteristic of the element so provides a method of qualitative analysis
- Also intensity of rays relate to the concentration of the element so gives quantitative information
- Some 50 elements can be analysed using samples as small as 10^-12 g.