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Chapter 13: Radioactivity Radioactivity decay is a process when an atomic nucleus spontaneously emits radiations or particles to become a more stable nucleus. As it decays, the number of atoms in a radioactive material decreases exponentially. The rate of the decay process is measured by the decay constant which is characteristic of each radioactive isotope.
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Page 1: Chapter 13: Radioactivity - YSL Physicsyslphysics.weebly.com/uploads/4/8/2/6/48261583/slides_13.pdf · Chapter 13: Radioactivity ... Derive and use half life, Learning Objectives

Chapter 13: Radioactivity

Radioactivity decay is a process when an atomic nucleus

spontaneously emits radiations or particles to become a

more stable nucleus. As it decays, the number of atoms in

a radioactive material decreases exponentially. The rate of

the decay process is measured by the decay constant

which is characteristic of each radioactive isotope.

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Overview

Radioactivity

Radioactive

Decay Decay Law

Application

(Tracers)

β-decay α-decay γ-decay

Half Life

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13.1 Radioactive Decay

Explain α, β+, β‒ and γ decays

State decay law and use

Define and determine activity, A and decay constant, λ

Derive and use or

Derive and use half life,

Learning Objectives

Nt

N

d

d

teNN 0

teAA 0

2ln

2

1 T

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Radioactive Decay

Radioactivity / Radioactive decay is disintegration of unstable nucleus to a more stable daughter nuclide with the emission of alpha, beta particles and gamma ray.

Radioactive decay is a spontaneous and random process.

Random means the time of decay of each atom cannot be predicted.

Spontaneous means it happens by itself without external stimuli (unplanned). The decay is unaffected by normal physical or chemical processes, such as heat, pressure and chemical reactions.

3 kinds of rays are produced by naturally occurring radioactivity: alpha particle (α), beta particle (β) and gamma rays (γ).

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Alpha Decay (α)

An -particle is a nucleus consists of two protons and two neutrons.

It is positively charged particle and its value is +2e with mass of 4.001502 u.

Alpha particle has least penetrating ability, can be blocked by a sheet of paper.

Its motion can be deflected by both magnetic field & electric field.

When a nucleus undergoes alpha decay it loses 4 nucleons (2 protons and 2 neutrons).

He4

2

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Alpha Decay (α)

The reaction can be represented by general equation

below:

QHeYX A

Z

A

Z 4

2

4

2

Parent Daughter α-particle Energy

released

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Beta Decay (β)

Beta particle has same mass as an electron or 0.000549 u

Beta particle can be electrically positive ( β+ or positron )

or negative ( β- or negatron )

◦ Symbol for positron:

◦ Symbol for negatron:

Beta particle has moderate penetrating ability and

blocks by a few millimeters aluminum.

Its motion can be deflected by both magnetic field &

electric field.

2 type of beta decay: negatron, β- decay and positron,

β+ decay

e0

1

0

1 or ,

e0

1

0

1 or ,

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Negatron Decay (β‒)

β- decay occurs when an unstable nucleus has too many

neutrons compared with the number of protons.

Through the β- decay, a neutron is converted into a

proton and creates a more stable daughter nucleus.

General form for β– decay is

QvYX A

Z

A

Z 0

11

Parent Daughter β-

particle Energy

released Anti

neutrino

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Negatron Decay (β‒)

Another elementary particle called antineutrino (𝒗 )

emitted in this decay.

Existence of antineutrino is a must in order to obey the

law of conservation of energy & angular momentum (to

account the missing energy in negatron decay).

Example:

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Positron Decay (β+)

Β+ decay occurs when an unstable nucleus has too many

protons compared with the number of neutrons.

Through the β- decay, a proton is converted into a

neutron and creates a more stable daughter nucleus.

General form for β+ decay is

QvYX A

Z

A

Z 0

11

Parent Daughter β+

particle Energy

released Neutrino

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Positron Decay (β+)

Another elementary particle called neutrino (𝒗) emitted

in this decay.

Existence of neutrino is a must in order to obey the law

of conservation of energy & angular momentum (to

account the missing energy in positron decay).

Example:

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Neutrino & Antineutrino

During beta-decay, it was found that the reaction does not obey the law of conservation of energy. The beta particles emitted have kinetic energy less than the values calculated from the mass difference in the reaction

In 1930, Pauli suggested the “missing” energy was carried by a particle which was later named neutrino, meaning „the little one‟ by Fermi.

Antineutrino is the anti-particle of the neutrino.

Characteristic of the neutrino:

◦ has no charge

◦ has zero mass

◦ travels at the speed of light

◦ interact very weakly with matter

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Gamma Decay (γ)

Gamma ray is a high energy photon.

It is uncharged (neutral) and zero mass (emission of

gamma ray does not change the parent nucleus into a

different nuclide).

Gamma ray has the most penetrating ability a few

centimeters in lead.

It cannot be deflected by any electric field or

magnetic field.

Gamma rays are emitted when an excited nucleus

jumps to lower energy level.

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Gamma Decay (γ)

Very often, a nucleus is left in an excited energy state

after it has undergone alpha or beta decay. This nucleus

can then undergo 2nd decay to lower energy level by

emitting a high energy photon called gamma (γ) ray.

The decay can be written as:

* XX A

Z

A

Z

Excited

energy

state

Lower

energy

state

γ-ray

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Comparison between α particle,

β particle and γ ray

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Deflection of α, β and γ Rays in

Electric Field and Magnetic Field

Alpha ray is only weakly deflected compare to

beta ray that is strongly deflected because alpha

particle is much heavier compare to beta particle

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Example 1

Write an equation to represent the decay.

What is the wavelength of the 0.186 MeV γ-ray photon

emitted by radium ? Ra226

88

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Example 1 – Solution

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Decay Law

Law of radioactive decay states that “for a radioactive

source, the rate of decay ( dN/dt ) is proportional to the

number of radioactive nuclei present (or not yet decayed),

N.”

Mathematically,

Ndt

dN

Ndt

dN

Negative sign means the number of

nuclei present decreases with time

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Decay Constant, λ

From , we get

Decay constant, λ is the ratio of rate of decay to the

number of radioactive atoms in sample.

SI unit for decay constant, λ: s-1

The decay constant is a characteristic of the radioactive

nuclide. It has different values for different nuclides.

The larger the decay constant, the greater is the rate of

decay.

Ndt

dN

N

dtdN

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Activity, A

Activity, A of a radioactive sample is defined as the

number of decays (or disintegrations) per second that

occur.

SI unit for activity, A: Becquerel (Bq)

1 Bq = 1 decay per second

Another SI unit usually used: Curie ( Ci )

1 Ci = 3.7 × 1010 Bq

dt

dNA

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Derivation

From the basic law of radioactive decay:

Rearranging the equation:

Suppose that at time t = 0 s, the number of undecayed

nuclei in the radioactive sample is No

At time t = t, let the number of undecayed nuclei left is

N

Ndt

dN

t dN

dN

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Derivation

Integrate the above equation:

N

N

t

dtN

dN

0 0

tN

N tN 00ln

tN

N

0

ln

teN

N 0

teNN 0

Exponential Law of

Radioactive Decay

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Derivation

From the law of radioactive decay, , and

definition of activity,

Thus,

and

and

Ndt

dN

dt

dNA

NA teNN 0

teNA 0

teNA 0 00 NA

teAA 0

Activity

at time t Activity at

time t = 0

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Half Life

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Half Life

Half-life T½ is defined as time required for the number

of radioactive nuclei to decrease to half of the

original number of nuclei.

The half-life of any given radioactive nuclide is

constant; it does not depend on the number of nuclei

present.

The units of the half-life are second (s), minute (min),

hour (hr), day and year (yr).

2ln2

1 T

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Example 2

The half life of the radioactive nucleus Radium,

is 1.6×103 year.

a. What is the decay constant of this nucleus ?

b. If a sample contains 3.0×1016 nuclei at t = 0 s,

determine its activity at this time.

c. What is the activity after sample is 2.0×103 year old ?

Ra226

88

Ra226

88

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Example 2 – Solution

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Example 2 – Solution

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Example 3

Initially, a radioactive sample contains of 1.0×106 nuclei.

The half-life of the sample is T1/2. Calculate the number of

nuclei present after 0.5T1/2.

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Example 3 – Solution

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Example 4

80% of a radioactive substance decays in 4 days.

Determine

a. the decay constant

b. its half life

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Example 4 – Solution

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Example 4 – Solution

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Example 5

A radioactive sample contains 3.5 µg of pure , which

has a half life of 20.4 min.

a. Determine the number of nuclei in the sample at t = 0 s.

b. What is the activity in Becquerel of the sample initially

and after 8.0 h ?

c. Calculate the number of radioactive nuclei remaining

after 8.0 h ?

C11

6

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Example 5 – Solution

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Example 5 – Solution

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Example 5 – Solution

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Example 5 – Solution

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13.2 Radioisotope as Tracers

Explain application of radioisotopes as tracers

Learning Objectives

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Radioisotope as Tracers Radioisotope is produced in a nuclear reactor where

unstable nuclei are bombarded by high speed neutrons

until they become radioactive nuclei.

Since radioisotope has the same chemical properties as

the stable isotopes then they can be used to trace the path

made by the stable isotopes

Basic Idea:

1. Prepare the diluted radioisotope solution

2. Added/ inject or swallow the solution

3. Use appropriate detectors to monitor the activity at the

designated area

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Radioisotope as Tracers 1. Medical and Health

• Detecting brain tumour with technitium-99

• Determine the enlargement of thyroid gland with iodine I-131

• Determine the location of blood clogs with 24Na

• To investigate metabolic pathways or blood flow

2. Industry

• Detecting leaks in underground pipes

• To measure the wear and tear of machine part and the effectiveness of lubricants

• To monitor the thickness of metal sheet during manufacture by passing it between gamma-ray and suitable detector

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Radioisotope as Tracers

3. Agriculture

• To enable scientist to formulate fertilizers that will

increase the production of food.

• To develop new strains of food crops that are

resistant to diseases, give high yield and are high

quality

4. Archaeology and geology

• To estimate the age of an archaeological object

found by referring to carbon-14 dating

• To estimate the geological age of rock by referring

to potassium-40 dating

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Radioisotope as Tracers

Radiation Treatment

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Radioisotope as Tracers

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Radioisotope as Tracers

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Radioisotope as Tracers

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Example 6

A small volume of a solution which contains a radioactive

isotope of sodium Na-24 has an activity of 1.5×104 Bq.

The solution is injected into the bloodstream of a patient.

The half-life of the sodium isotope is 15 hours. After 30

hours, the activity of 1.0 cm3 of blood is measured and

found to be 0.50 Bq. Estimate the volume of blood in the

patient.

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Example 6 – Solution

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