Ch. 18: The Nucleus
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Transcript Ch. 18: The Nucleus
Ch. 18: The Nucleus
Review
21.1: Nuclear Stability and Radioactive
Decay
21.2 Kinetics of Decay
21.3 Nuclear Transformations
Review
Nucleus
contains protons and neutrons
Atomic number (Z) - # p+
Mass number (A) - # p+ + # n0
Isotopes- differ in number of neutrons
only
Same Z but different A
Nuclide- specific type of atom, member
of a group of isotopes
A
14
Nuclear symbol notation
Z
X
6
C
Radioactivity and Stability
A nucleus that decomposes forming another
nucleus and one or more particles
All nuclides are unstable with 84 p+ or more
Lightweight nuclides are stable with equal
numbers of n0 and p+
Heavy nuclides should have ratio >1 to be
stable
Radioactivity
and Stability
Types of Decay- A changes
Alpha
particle production
α particle: helium nucleus
238
4
234
92
2
90
4
2
He
U He Th
Spontaneous
fission
Splitting of a heavy nucleus into 2
lighter nuclides that are about the
same size
Types of Decay- A is Constant
Beta
Particle Production
β particle is an electron
Can assume the mass is zero
234
0
234
90
1
91
0
1
e
Th e Pa
Net effect : changing a n0 into a p+
Types of Decay- A is Constant
Gamma
Ray Production
γ ray is collection of high energy
photons
Occurs with other types of decay
238
4
234
0
92
2
90
0
U He Th 2
Helps a nucleus release extra energy
so it can relax to a lower energy state
Types of Decay- A is Constant
0
1
e
Production
Occurs for nuclides below the line of
stability
Positron is a positive particle with
same mass of electron
Also called antiparticle of electron
Positron
Th e Ne
22
11
0
1
22
10
Net effect: change p+ into n0
Types of Decay- A is Constant
0
1
Electron
Capture
e
One of the inner electrons in an atom
is captured by nucleus
Gamma rays always produced
Hg e Au
201
0
80
1
Decay Series
201
79
0
0
When several types of decay occur until a
stable nuclide is produced
Writing Equations
116C
produces a positron
21483Bi
C e B
11
6
0
1
11
5
produces a beta particle
214
83
23793Np
Bi e Po
0
1
214
84
produces an alpha particle
237
93
Np He Pa
4
2
233
91
Writing Equations
195
79
Au ? Pt
Beta particle (electron)
Electron capture
38
19
195
78
K ? Ar
38
18
Positron
Positron production
Kinetics of Decay
Rate
of decay is
directly
proportional to
number of
nuclides available
All are first order
Constant half-life
Rate kN
N
kt
ln
N0
0.693
t1/ 2
k
Example
If
the half-life of a decay is 67.0 hours,
how much of a 1.000 mg sample will
remain after 335 hours?
335 / 67 = 5 half-life’s
1.000 mg 0.500 mg
0.250 mg 0.125 mg
0.062 mg 0.031 mg
Nuclear Transformations
Change
of one element into another
Scientists have been able to use this to
make the periodic table larger by
creating new elements
Since 1940, have been able to make
transuranium elements (93-112)
18.4 Detection and Uses of Radioactivity
18.5 Thermodynamic Stability
18.6 Nuclear Fission and Fusion
18.7 Effects of Radiation
Carbon-14 Dating
Used to date items made out of natural fibers
Created by Willard Libby in 1940s
Based on the decay of naturally existing carbon14 isotope by β-particle production
It is also created
14
6
14
7
C e
0
1
14
7
N
N n H C
1
0
1
1
14
6
Carbon-14 Dating
These happen at the same
rate as long as the plant is
alive but when it dies, the
decay happens more
rapidly than the creation
Ratio of 14-C to 12-C
decreases
Most accurate for pieces
older than 10,000 years
Medical Applications
Radiotracers
Radioactive nuclides that can be traced in
people by monitoring their radioactivity
Thallium-201
For assessing heart damage from heart attacks
Is taken up by healthy heart tissue only
Medical Applications
Iodine-131
For diagnosing thyroid problems
Patients drink a solution of 131-I
and the uptake is monitored
Thermodynamic Stability
Can be determined by calculating the change
in potential energy if the nucleus is made
from individual particles
1
1
16
0
1
8
We can create energy changes by comparing
the sum of the masses: mass defect
Mass of 168O – mass of (8 10n + 8 11n)
Convert amu on periodic table to g
(1amu=1.66x10-24 g)
8 n 8 H O
2.65535x10-23 – [8(1.67493x10-24) + 8(1.67262x10-24)]
-2.269x10-25 g/nucleus = -0.1366 g/mol : lost
when 1 mol of 16-O is formed
Thermodynamic Stability
Find
energy (J) using E=mc2
E = (-1.366x10-4kg)(3.00x108m/s)2
= -1.23x1013J/mol
mass must be in kg!
Binding energy
Energy required to decompose this
nucleus into its particles
Often in MeV / nucleon
1.23 1013 J
1mol
1MeV
1nucleus
23
13
mol
6.02 10 nuclei 1.60 10 J 16nucleons
7.98MeV / nucleon
Thermodynamic Stability
Nuclear Fission and Fusion
Fission
Splitting a heavy nucleus into 2 smaller
nuclei with smaller mass numbers
Can use neutrons to create instability
1
0
n U Ba Kr 3 n
235
92
141
56
92
36
1
0
Neutrons produced are used to cause
more fission
Produces a huge amount of energy
Nuclear
Fission
and
Fusion
Nuclear Fission and Fusion
Fusion
Combination of 2 light nuclei to form
a heavier, more stable nucleus
Stars produce their energy using this
1
1
H H H e
1
1
2
1
0
1
Requires very high temperatures
Must be shot at each other to get
close enough
Effects of Radiation
Any
sort of energy transferred to cells
can break bonds and cause damage
Radioactive species are sources of
high energy particles so can be very
harmful
Types
Somatic: cause illness, cancer, death
Genetic: produce damage in
offspring
Factors in Effects of
Radiation
The
more energy, the more damage
How deep it goes into body
γ rays > β particles (1 cm) > α particles
(skin)
How easily they attract electrons from
biomolecules (ionization)
γ rays cause less than α particles
How long it stays inside body