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Isotopes

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Title: Isotopes


1
Lecture 9 Isotopes
2
Look For the Following Key Ideas
  • Elements consist of isotopes with the same number
    of protons, but differing numbers of neutrons
  • Stable isotopes provide a variety of
    information on the Earth system including
    paleo-conditions, ecosystem dynamics, global
    productivity, weathering rates
  • Radioisotopes provide a variety of information
    on the Earth system including ocean circulation,
    sedimentation, process rates CLOCKS

3
Overview
  • Isotopes
  • overview
  • Stable Isotopes
  • C, H, N, O, S, Sr
  • Radioisotopes
  • C, H, U-series

4
Isotope Systematics
Isotope Identical number of protons, different
number of neutrons. Identical chemistry,
different rates. 2 Flavors stable (280) and
radioactive (1700 ? 67)
5
Isotope Systematics
6
Isotope Systematics
The wonders of mass spectrometry allow very
precise measurements. Sensible units are needed.
7
Isotope Systematics
C, H, O, N, S (Standards) C Pee Dee
belemnite carbonate (PDB) H/O Standard Mean
Ocean Water (V-SMOW) S Diablo Canyon
Troilite (a meteor) N Atmospheric N2
8
Isotope Systematics
d13C () ( - 1) 1000
13C/12Csample
13C/12Cstandard
9
Group Problem 1 (10 min)
Pretend I provide each group with three samples
of distilled water (equal volumes) with the
following d2H values -400, 0, and 600.
Calculate the D/H ratios for each of these
samples. Assume the D/H of SMOW is
1.5010-4. Now pretend you mix the three samples
together and calculate the resulting D/H. From
the D/H, calculate the resulting d2H.
d2H () ( - 1) 1000
2H/1Hsample
2H/1HSMOW
10
Some Uses of Stable Isotopes
  • Isotope Ratios Vary in Nature
  • ? Kinetic Processes (KIE)
  • ? Thermodynamic Processes (EIE)

11
Some Uses of Stable Isotopes
  • ? Kinetic Processes (KIE)
  • Lighter Isotope Reacts Faster
  • Quantum Mechanical

12CO2 H2O ? 12CH2O O2 (kC12)
13CO2 H2O ? 13CH2O O2 (kC13)
kC12 gt kC13
12
Some Uses of Stable Isotopes
  • ? Equilibrium Processes (EIE)
  • Equilibrium Achieved
  • Thermodynamic effect

HDO H2 ?? H2O HD (exchange)
13
Some Uses of Stable Isotopes
  • 13C/12C Biological Pump, Trophic..
  • 2H/1H Temp/Ice Volume
  • 15N/14N Trophic Interactions
  • 18O/16O Temperature/Ice Volume
  • 34S/32S Atmospheric O2
  • 87Sr/86Sr Global Weathering

14
Some Uses of Stable Isotopes
  • Rayleigh Process After changing form/phase, each
    increment is isolated from contact with the
    initial form/phase.

15
Some Uses of Stable Isotopes
16
Some Uses of Stable Isotopes
  • Carbon Source
  • Photosynthesis
  • C3 plants (annual) d13C -21 to -35
  • C4 plants (perrenials) d13C -11 to -15
  • Aquatic plants d13C -11 to -39

17
Biological Pump
122CO2 138H2O 16HNO3 H3PO4 ?
(CH2O)80(CH2)42(NH3)16(H3PO4) 175O2
B
(1-f)B
CO2 HNO3 H3PO4
fB
(CH2O)80(CH2)42(NH3)16(H3PO4)
Burial and Preservation of OM.
18
Biological Pump
122CO2 138H2O 16HNO3 H3PO4 ?
(CH2O)80(CH2)42(NH3)16(H3PO4) 175O2
B
(1-f)B
CO2 HNO3 H3PO4
fB
(CH2O)80(CH2)42(NH3)16(H3PO4)
Burial and Preservation of OM.
19
Isotopes
  • Imbalance of protons and neutrons ? nuclear
    instability

20
Radioisotopes
  • Imbalance of protons and neutrons ? nuclear
    instability
  • B- emission (electron N ? P)
  • B emission (positron P ? N)
  • Electron Capture (P ? N)
  • Alpha Emission (He nucleus)
  • Gamma ray (just energy)

21
Group Problem 2 (8 min)
  • 238U is a common radioisotope of Uranium. 238U
    decays through a complex process of 6b- decays
    and 8a decays. What are the final daughter
    nuclei?
  • On a plot of atomic number vs. Neutron number,
    plot out all possible decay pathways. All
    pathways produce 234Th, 234U, 218Po, and 210Pb
    as intermediates. 210Po is never formed.

22
Some Uses of Radioisotopes
  • 40K/40Ar Dating ancient rocks
  • 238U/234Th Particle scavenging
  • 226Ra/222Rn Air-Sea gas exchange
  • 226Ra/220Pb Sedimentation Rates
  • 14C Mixing, age dating
  • 3H Modern mixing

23
Mathematically
  • dN/dt -lN (activity rate first order)
  • ln(N/No) -lt
  • N/No e-lt
  • N Noe-lt
  • No atoms at t 0
  • l decay constant

24
Group Problem 3 (8 min)
  • Derive the mathematical expression for half life.
  • Determine the mathematical relationship between
    the half life (T1/2) and the mean lifetime (t
    1/l). What fraction of an isotope has decayed
    after 1 mean lifetime?

25
Secular Equilibrium
  • Parent and Daughter(s)
  • Parent is long lived
  • No chemical separation for several half lives
  • lN(p) lN(d)
  • ? Deviations are useful
  • lN activity

26
14C Special Focus
  • Production 14N n ? 14C p
  • Decay 14C ? 14N b- neutrino
  • l 1.2110-4 y-1

27
14C Special Focus
  • Natural Prodcution rate of 14C

28
14C Special Focus
  • The Bomb Spike

29
14C Special Focus
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