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Radioactivity
What Is Radioactivity? What is
Radiation?
Quick Review of Radioactivity
by Anne Marie Helmenstine, Ph.D.
Unstable
atomic nuclei will spontaneously decompose to form nuclei with higher
stability. The decomposition process is called radioactivity.
The
energy and particles which are released during the decomposition process are
called radiation.
When
unstable nuclei decompose in nature, the process is referred to as natural
radioactivity.
When
the unstable nuclei are prepared in the laboratory, the decomposition is called
induced radioactivity.
There
are three major types of natural radioactivity:
Alpha
Radiation
Alpha
radiation consists of a stream of positively charged particles, called alpha
particles, which have an atomic mass of 4 and
a charge of +2 (a helium nucleus).
When
an alpha particle is ejected from a nucleus, the mass number of the nucleus
decreases by four units and the atomic number decreases
by two units.
For
example:
23892U → 42He
+ 23490Th
The
helium nucleus is the alpha particle.
Beta
Radiation
Beta
radiation is a stream of electrons, called beta particles.
When
a beta particle is ejected, a neutron in the nucleus is converted to a
proton, so the mass number of
the nucleus is unchanged, but the atomic number increases by one unit.
For
example:
23490 → 0-1e
+ 23491Pa
The
electron is the beta particle.
Gamma
Radiation
Gamma
rays are high-energy photons with a very short wavelength (0.0005 to 0.1 nm).
The emission of gamma radiation results from an energy change within the atomic
nucleus.
Gamma
emission changes neither the atomic number nor the atomic mass. Alpha and
beta emission are often accompanied by gamma emission, as an excited nucleus
drops to a lower and more stable energy state.
Alpha,
beta, and gamma radiation also
accompany induced radioactivity.
Radioactive isotopes are
prepared in the lab using bombardment reactions to convert a stable nucleus
into one which is radioactive.
Positron
(a particle with the same mass as an electron, but a charge of +1 instead of
-1) emission isn't observed in natural radioactivity,
but it is a common mode of decay in induced radioactivity.
Bombardment
reactions can be used to produce very heavy elements, including many which
don't occur in nature.
Anne
Marie Helmenstine, Ph.D.
Ph.D. in biomedical sciences from the
University of Tennessee at Knoxville - Oak Ridge National Laboratory.
Science educator with experience
teaching chemistry, biology, astronomy, and physics at the high school,
college, and graduate levels.
ThoughtCo and About Education chemistry
expert since 2001.
Widely-published graphic artist,
responsible for printable periodic tables and other illustrations used in
science.
Experience
Anne Helmenstine, Ph.D. has covered
chemistry for ThoughtCo and About Education since 2001, and other sciences
since 2013. She taught chemistry, biology, astronomy, and physics at the high
school, college, and graduate levels. She has worked as a research
scientist and also abstracting and indexing diverse scientific literature for
the Department of Energy.
In addition to her work as a science
writer, Dr. Helmenstine currently serves as a scientific consultant,
specializing in problems requiring an interdisciplinary
approach. Previously, she worked as a research scientist and college
professor.
Education
Dr. Helmenstine holds a Ph.D. in
biomedical sciences from the University of Tennessee at Knoxville and a
B.A. in physics and mathematics with a minor in chemistry from Hastings
College. In her doctoral work, Dr. Helmenstine developed ultra-sensitive
chemical detection and medical diagnostic tests.
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