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Nuclear Chemistry

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Title: Nuclear Chemistry


1
Nuclear Chemistry
  • Chapter 23

2
n/p too large
n/p too small
23.2
3
Types Of Radioactive Decay
  • An alpha (a) particle has the same composition as
    a helium nucleus two protons and two neutrons
    (positive charge)
  • Beta (b-) particles are high-energy electrons
    (from the nucleus, not from the electron cloud).
  • Gamma (g) rays are a highly penetrating form of
    electromagnetic radiation. No charge.
  • Positrons are particles having the same mass as
    electrons but carrying a charge of 1.
  • Electron capture (EC) is a process in which the
    nucleus absorbs an electron from an inner
    electron shell, usually the first or second, with
    the release of an X-ray.
  • Most radionuclides undergo one specific type of
    decay, though some can undergo two or more types.

4
How Far Will Radiation Penetrate?
5
Summary Of Decay Types
6
Atomic number (Z) number of protons in nucleus
Mass number (A) number of protons number of
neutrons
atomic number (Z) number of neutrons
A
1
1
0
0
4
Z
1
0
-1
1
2
23.1
7
Balancing Nuclear Equations
  • Conserve mass number (A).

The sum of protons plus neutrons in the products
must equal the sum of protons plus neutrons in
the reactants.
235 1 138 96 2x1
  • Conserve atomic number (Z) or nuclear charge.

The sum of nuclear charges in the products must
equal the sum of nuclear charges in the reactants.
92 0 55 37 2x0
23.1
8
212Po decays by alpha emission. Write the
balanced nuclear equation for the decay of 212Po.
212 4 A
A 208
84 2 Z
Z 82
23.1
9
  • (a) a-particle emission by radon-222
  • 22288Rn ? 42He ??
  • 22288Rn ? 42He 21886Po
  • (b) ß-decay of phosphorus-32
  • 3215P ? 01 ß ??
  • 3215P ? 01 ß 3216S

10
23.1
11
Nuclear Stability and Radioactive Decay
Beta decay
Increase of protons by 1
Decrease of neutrons by 1
Positron decay
Decrease of protons by 1
Increase of neutrons by 1
23.2
12
Nuclear Stability and Radioactive Decay
Electron capture decay
Decrease of protons by 1
Increase of neutrons by 1
Alpha decay
Decrease of neutrons by 2
Decrease of protons by 2
23.2
13
n/p too large
beta decay
n/p too small
positron decay or electron capture
23.2
14
Nuclear Stability
  • Certain numbers of neutrons and protons are extra
    stable
  • n or p 2, 8, 20, 50, 82 and 126
  • Like extra stable numbers of electrons in noble
    gases (e- 2, 10, 18, 36, 54 and 86)
  • Nuclei with even numbers of both protons and
    neutrons are more stable than those with odd
    numbers of neutron and protons
  • All isotopes of the elements with atomic numbers
    higher than 83 are radioactive
  • All isotopes of Tc are radioactive

23.2
15
Nuclear binding energy (BE) is the energy
required to break up a nucleus into its component
protons and neutrons.
E mc2
BE 9 x (p mass) 10 x (n mass) 19F mass
BE (amu) 9 x 1.007825 10 x 1.008665 18.9984
BE 0.1587 amu
1 amu 1.49 x 10-10 J
BE 2.37 x 10-11J
1.25 x 10-12 J
23.2
16
Nuclear binding energy per nucleon vs Mass number
23.2
17
Electron capture decay
- 36.966776amu - .000549amu 36.965903amu -
0.001422amu
0.001422amu 1.4924E-10 J/amu 2.1222E-13 J
E/h v 2.1222E-13 J / 6.626E-34 Js 3.2028E20
1/s
1amu 931.5MeV
0.001422amu 931.5 MeV/amu 1.3246 MeV
23.2
18
Kinetics of Radioactive Decay
rate lN
N N0exp(-lt)
lnN lnN0 - lt
N the number of atoms at time t
N0 the number of atoms at time t 0
l is the decay constant
23.3
19
Kinetics of Radioactive Decay
N N0exp(-lt)
lnN lnN0 - lt
23.3
20
Selected Nuclide Half-Lives
21
Radiocarbon Dating
t½ 5730 years
Uranium-238 Dating
t½ 4.51 x 109 years
23.3
22
Radiocarbon Dating
  • 14C is formed at a nearly constant rate in the
    upper atmosphere by the bombardment of 14N with
    neutrons from cosmic radiation.
  • The 14C is eventually incorporated into
    atmospheric CO2.
  • Since atmospheric CO2 eventually finds its way
    into living tissue, the level of 14C in living
    tissue is constant (about 15 disintegrations per
    minute per gram of carbon).
  • When an organism dies, no more 14C is consumed.
  • The level of 14C decreases as the dead tissue
    ages.
  • The half-life for carbon-14 is 5,730 years. This
    dating method works well for objects up to 50,000
    years old.

23
EXAMPLE 19.4 A wooden object from an Egyptian
tomb is subjected to radiocarbon dating. The
decay rate observed for its carbon-14 content is
7.2 dis min1 per g carbon. What is the age of
the wood in the object (and, presumably, of the
object itself)? The half-life of carbon-14 is
5730 years, and the decay rate for carbon-14 in
living organisms is 15 dis min1 per g
carbon. SOLUTION First, we can determine the
decay constant, ? ? 0.693/ t1/2 0.693/5730
y 1.21 x 104 y1 Now we can use the decay
equation, substituting activity (disintegrations
per minute) for N Nt 7.2
ln ? t ln (1.21 x
104 y1) t No 15 t
6.1 x 103 y
24
Nuclear Transmutation
23.4
25
Nuclear Transmutation
23.4
26
Nuclear Fission
Energy mass 235U mass n (mass 90Sr mass
143Xe 3 x mass n ) x c2
Energy 3.3 x 10-11J per 235U
2.0 x 1013 J per mole 235U
Combustion of 1 ton of coal 5 x 107 J
23.5
27
Nuclear Fission
Representative fission reaction
23.5
28
Nuclear Fission
Nuclear chain reaction is a self-sustaining
sequence of nuclear fission reactions.
The minimum mass of fissionable material required
to generate a self-sustaining nuclear chain
reaction is the critical mass.
23.5
29
Nuclear Fission
Schematic diagram of a nuclear fission reactor
23.5
30
Nuclear Fission
Annual Waste Production
23.5
31
Nuclear Fission
Hazards of the radioactivities in spent fuel
compared to uranium ore
23.5
From Science, Society and Americas Nuclear
Waste, DOE/RW-0361 TG
32
Chemistry In Action Natures Own Fission Reactor
Natural Uranium
0.7202 U-235 99.2798 U-238
Measured at Oklo
0.7171 U-235
33
Nuclear Fusion
Fusion Reaction
Energy Released
6.3 x 10-13 J
2.8 x 10-12 J
3.6 x 10-12 J
Tokamak magnetic plasma confinement
23.6
34
Radioisotopes in Medicine
  • 1 out of every 3 hospital patients will undergo a
    nuclear medicine procedure
  • 24Na, t½ 14.8 hr, b emitter, blood-flow tracer
  • 131I, t½ 14.8 hr, b emitter, thyroid gland
    activity
  • 123I, t½ 13.3 hr, g-ray emitter, brain imaging
  • 18F, t½ 1.8 hr, b emitter, positron emission
    tomography
  • 99mTc, t½ 6 hr, g-ray emitter, imaging agent

Brain images with 123I-labeled compound
23.7
35
Geiger-Müller Counter
23.7
36
Biological Effects of Radiation
Radiation absorbed dose (rad)
1 rad 1 x 10-5 J/g of material
Roentgen equivalent for man (rem)
1 rem 1 rad x Q
Quality Factor
g-ray 1
b 1
a 20
23.8
37
Chemistry In Action Food Irradiation
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