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Transcript
Name
Section
Date
Atomic Theory, Isotopes, and Radioactive
Decay
7.1
Simmary
Textbook pages 286-301
Before You Read
Radiation is used for many purposes. What uses of radiation are you already aware of?
Write your response in the lines below.
•Create a Quiz
After you have read this sec
tion, create a five-question
quiz based on what you have
learned. Answer the ques
tions until you get each one
correct.
What is radioactivity?
Radioactivity is the release of high-energy particles and
rays of energy from a substance as a result of changes in
the nuclei of its atoms. Radiation refers to high-energy
rays and particles emitted by radioactive sources, including
radio waves, microwaves, infrared rays, visible light, and
ultraviolet rays, that are found on the electromagnetic
spectrum. Light is a form of radiation that humans can see.
)
What are isotopes?
Isotopes are different atoms of a particular element that
have the same number of protons but different numbers of
neutrons. The mass number of an atom is an integer (whole
number) that represents the sum of the atom’s protons and
neutrons—so isotopes have different mass numbers. The
mass number of an isotope is found by adding the atomic
number (number of protons) to the number of neutrOns.
Mass number
Reading Check
Write the equation used to
calculate mass number.
=
atomic number + number of neutrons
To find the number of neutrons of an isotope, subtract the
atomic number from the mass number.
Number of neutrons
=
mass number
—
atomic number
How are isotopes represented?
Chemists represent isotopes using standard atomic notation
(also called the nuclear symbol), a shortened form involving
the chemical symbol, atomic number, and mass number. The
mass number is written as a superscript (above) on the left
120
MHR • Section 7.1
Atomic Theory, sotopes, and Radioactive Decay © 2008 McGraw-Hill Ryerson Limited
Section
7.1 1—
Date
Name
continued
of the symbol. The atomic number is written as a subscript
(below), also on the left.
39
K
19
The mass number of this potassium isotope is 39. The atomic
number is 19. An isotope of potassium with a mass number
of 39 can also be represented as potassium-39, or K-39
What is radioactive decay?
By emitting radiation, atoms of one kind of element can
change into atoms of another element. Radioactive atoms
emit radiation because their nuclei are unstable. Unstable
atoms gain stability by losing energy. Radioactive decay is
the process in which unstable nuclei lose energy by emitting
radiation. Unstable radioactive atoms undergo radioactive
decay and form stable, non-radioactive atoms, usually of a
different element. Radioisotopes are natural or human-made
isotopes that decay into other isotopes, releasing radiation.
-
What different types of radiation are emitted during
radioactive decay?
The three major types of radiation are alpha radiation, beta
radiation, and gamma radiation. Their properties are summed
up in the following table:
Beta Radiation
Alpha Radiation
Symbol
aorHe
Composition
Alpha particles
Beta particles
High-energy
electromagnetic
radiation
Description of
radiation
Helium nuclei,
He
4
Electrons
High energy rays
Charge
2+
ReIatie
penetrating
Blocked by paper
02008 McGraw-Hill Ryerson Limited
Name the three main types
of radiation.
Gamma Radiation
Property
power
Reading Check
or
0
Blocked by
metal foil
Partly or
completely blocked
or concrete
by lead
Section 7.1
Atomic Theory, Isotopes, and Radioactive Decay
•
MHR
121
Date
Name
How is radioactive decay expressed?
Radioactivity results when the nucleus of an atom decays.
There are three radioactive decay processes:
1. Alpha decay: The emission of an alpha particle (the
same particles found in the nucleus of a helium atom)
from a nucleus is a process called alpha decay. When
a radioactive nucleus emits an alpha particle, the atomic
number of the product nucleus is reduced by two, and its
mass number by four. However, the sum of the atomic
numbers and the sum of the mass numbers on each side of
the arrow remain equal.
4
222
226
Ra—*
Rn+a
2
86
88
2. Beta decay: In beta decay, a neutron changes into a
proton and a beta particle, an electron. The proton
remains in the nucleus while the electron leaves the
nucleus. Since the proton remains in the nucleus, the
atomic number of the element increases by one—it
has become an atom of the next higher element on the
periodic table. However, its mass number does not
change, as a proton of almost equal mass has replaced the
neutron.
0
131
131
Xe-i-fl
I-l
54
53
3. Gamma decay: Gamma decay results from a
redistribution of energy within the nucleus. Gamma
radiation consists of rays of high-energy, shortwavelength radiation. A gamma ray is given off as the
isotope changes from a high-energy state to a lower
energy state.
60.
Ni** 60.0
Ni+ y
0
28
28
means that the nickel nucleus has extra energy that is
The
released as a gamma ray.
““
122
MHR • Section 7.1
Atomic Theory, Isotopes, and Radioactive Decay
© 2008 McGraw-Hill Ryerson Limited
Name
Section
Date
7.2
Summary
Half-Life
Textbook pages 302-311
Before You Read
Write a sentence in the lines below explaining what the word decay means to you. As
you read about radioactive decay, think about how the common meaning of decay differs
from the scientific meaning.
What is radiocarbon dating?
Mark the Text
Radiocarbon dating is the process of determining the age of
an object by measuring the amount of carbon-14 remaining in
that object. Carbon’s isotopes include carbon-12 and carbon14. When an organism is alive, the ratio of carbon- 14 atoms
to carbon-12 atoms in the organism remains nearly constant.
But when an organism dies, its carbon- 14 atoms decay
without being replaced. The ratio of carbon-14 to carbon-12
then decreases with time. By measuring this ratio, the age of
an organism’s remains can be estimated. Only material from
plants and animals that lived within the past 50 000 years
contains enough carbon- 14 to be measured using radiocarbon
dating. e
In Your Own Words
After you read this section,
go back and summarize the
main concepts in your own
words.
Reading Check
1. Which carbon isotope
undergoes radioactive
decay?
What is a half-life and how is it used in radiocarbon
dating?
A half-life is a measure of the rate of radioactive decay
for a given isotope. It is equal to the time required for half
the nuclei in a sample to decay. Its value is a constant for
any radioactive isotope. For example, the half-life of the
radioisotope strontium-90 is 29 years. If you have 10.0 g of
strontium-90 today, 29 years from now you will have
5.00 g left. This is because one half-life will have passed
(10.0 g x = 5.00 g). 58 years from now, two half-lives will
have passed and 2.50 g of the sample will remain
x = 2.50 g). The shorter the half-life is, the
(10.0 g x
faster the decay rate. A decay curve is a curved line on a
graph that shows the rate at which radioisotopes decay.
© 2008 McGraw-Hill Ryerson Limited
Section 7.2
HaUf-Life
•
MHR
129
Section
7.2
Date
Name
Summary
continued
Decyof Strontium 90
O.Og
100
Number of half-lives
(1 half-life = 29 y)
This decay curve shows how the amount of strontium-90 in a
sample changes over time.
What are parent and daughter isotopes?
Reading Check
1. Which isotope decays, the
parent or the daughter?
A parent isotope is an isotope that undergoes radioactive
decay. The stable product of this decay is called the daughter
isotope. The production of a daughter isotope can be a direct
reaction or the result of a series of decays.
Each parent isotope can be paired with a specific daughter
isotope. For example, carbon-12 is the daughter isotope of
carbon-14 (the parent isotope). The chart on page 307 of
the textbook lists other common isotope pairs. It also shows
the half-life of the parent and the effective dating range the
isotope can be used for.
How does the potassium-40 clock work?
The potassium-40 clock uses radioisotopes, specifically
potassium-40 and argon-40, to determine Earth’s age.
Potassium-40 has a half-life of 1.3 billion years. Its daughter
isotope is argon-40. When rock is produced from lava, all the
gases in the molten rock, including argon-40, are driven out.
This process sets the potassium radioisotope clock to zero,
because potassium-40 (the parent) is present but no argon-40
(the daughter) is present.
As the molten rock cools over time, it traps gases that
form as a result of radioactive decay. When tested, both
potassium-40 and argon-40 are now present in the rock. As
130
MHR
•
Section 7.2
Half-Life
© 2008 McGraw-Hill Ryerson limited
V
Section
7.2
Date
Name
Summary
continued
the mass of the parent isotope drops, the mass of the daughter
isotope increases. By measuring this ratio, the age of the rock
can be estimated. For example, if analysis showed that there
were equal masses of potassium-40 and argon-40 in a rock,
the rock would be 1.3 billion years old, the amount of time it
takes half of the potassium-40 to decay into argon-40.
The Potassium-40 Clock
100
35975
90
80
:..
70
60
I
0
50
.
“if
fL4
4Q
30
f
a;
o. 20
potassium (parent)
:LLJ*
Z50
-
,::t::t ‘i2:
10 /::s::
1.3
0
0
1
3.9
5.2
2.6
6.5
Elapsed Time (billion y)
2
3
4
Half-life
5
7.8
6
The solid line shows that the parent isotope is decaying.
The dashed line shows that the daughter isotope is being
produced.
© 2008 McGraw-Hill Ryerson Limited
Section 7.2
Half-Life
•
MHR
131
Name
Section
Date
7.3
Nuclear Reactions
Summary
Textbook pages 312-325
Before You Read
Nuclear reactors supply energy to many parts of Canada. Summarize what you already
know about nuclear reactions in the lines below.
What is nuclear fission?
1
Nuclear fission is a nuclear reaction in which a nucleus
breaks apart, producing two or more smaller nuclei,
subatomic particles, and energy. For example, for Uranium235,
235
92
1
141
1
U—*
n+
Kr+
Ba+3n+energy
92
0
36
56
0
Heavy nuclei tend to be unstable because of the repulsive
forces between their many protons. In order to increase their
stability, atoms with heavy nuclei may split into atoms with
lighter nuclei. The fission of a nucleus is accompanied by a
very large release of energy. Fission is the source of energy
for all nuclear power generation used today; however, the
radioactive daughter products are a significant waste disposal
problem.
Mark the Text
Summarize
As you read this section,
highlight the main point in
each paragraph. Then write a
short paragraph summarizing
what you have learned.
Reading Check
Why do heavy nuclei tend
to be unstable?
How do nuclear reactions work?
In typical chemical reactions, the energy produced or used is
so small that there is very little change in mass. There are no
changes in the nuclei of the reactants, so the identities of the
atoms do not change. Chemical reactions involve electrons
and rearrangements in the way atoms and ions are connected
to each other.
© 2008 McGraw-Hill Ryerson Limited
Section 7.3
Nuclear Reactions
•
MHR
137
Section
Name
Date
7•3
continued
A nuclear reaction is a process in which an atom’s
nucleus changes by gaining or releasing particles or energy.
A nuclear reaction can release protons, neutrons, and
electrons, as well as gamma rays. In nuclear reactions, a
small change in mass results in a very large change in energy.
Scientists can induce, or cause, a nuclear reaction by
making a nucleus unstable, causing it to undergo a reaction
immediately. Bombarding a nucleus with alpha particles,
beta particles, or gamma rays induces a nuclear reaction. An
example of an induced reaction is given below. Nitrogen-14
is bombarded with alpha particles, producing oxygen and
protons.
4
1
a-- 14 N—* 17 O+p
2
7
1
8
When some nuclei undergo fission, they release
subatomic particles that trigger more fission reactions. This
ongoing process in which one reaction initiates the next
reaction is called a chain reaction. The number of fissions
and the amount of energy released can increase rapidly and
lead to a violent nuclear explosion. Uranium-235, which is
used in Canadian nuclear reactors, undergoes such a reaction.
Keeping the chain reaction going in a nuclear power plant,
while preventing it from racing out of control, requires
precise monitoring and continual adjusting.
What are the rules for writing nuclear equations?
A nuclear equation is a set of symbols that indicates
changes in the nuclei of atoms during a nuclear reaction.
The following rules can be used when you write a nuclear
equation.
1. The sum of the mass numbers on each side of the equation
stays the same.
2. The sum of the charges (represented by atomic numbers)
on each side of the equation stays the same.
138
MHR
•
Section 7.3
Nuclear Reactions
©2008 McGraw-Hill Ryerson Limited
j___
Section
Name
73
Date
continued
What is nuclear fusion?
Nuclear fusion is a nuclear reaction in which small nuclei
combine to produce a larger nucleus. Other subatomic
particles as well as energy are released in this process. Fusion
occurs at the core of the Sun and other stars where sufficient
pressure and high temperatures cause isotopes of hydrogen to
collide with great force. This forces two nuclei of hydrogen
to merge into a single nucleus, releasing an enormous amount
of energy. The fusion reaction that occurs in the Sun is given
below.
2
3
4
1
H+ H—*- He+ n+energy
1
1
2
0
Reading Check
We do not currently have the technology to extract energy
from fusion reactions. One of the difficulties is achieving and
containing the high temperatures and pressures required to
bring about fusion.
© 2008 McGraw-Hill Ryerson Limited
Section 7.3
identify the main differ
ence between fission and
fusion.
Nuclear Reactions
•
MHR
139
[_._-