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Radioactivity
Samiul Ehsan
Computer Science & Engineering
Radioactivity
▪ Radioactivity also known as radioactive decay is a process
in which unstable atomic nucleus loses energy by emitting
radiation.
▪ Radiation is released in form of particles or
electromagnetic waves.
▪ The rate of radioactive decay is described in half-lives.
▪ The main source of radiation in Earth is sun. Radiation is
going through everywhere and all the time.
Pioneers in Radioactivity
Roentgen:
Discoverer of X-
rays 1895
Becquerel:
Discoverer of
Radioactivity
1896
The Curies:
Discoverers of
Radium and
Polonium 1900-
1908
Rutherford:
Discoverer
Alpha and Beta
rays 1897
Type of Radioactivity
By the end of the 1800s, it was known that
certain isotopes emit penetrating rays.
Three types of radiation were known:
1)Alpha particles (a)
2)Beta particles (b)
3)Gamma-rays (g)
Particle Mass Charge
Gamma (g) 0 0
Beta (b) ~0.5 -1
Alpha (a) ~3752 +2
Alpha Particles (a)
Radium
R226
88 protons
138 neutrons
Radon
Rn222
This is the
atomic weight, which
is the number of
protons plus neutrons
86 protons
136 neutrons
+ n
np
p
a (4He)
2 protons
2 neutrons
 The alpha-particle (a) is a Helium nucleus.
 It’s the same as the element Helium, with the electrons
stripped off !
 A sheet of paper or human skin can stop Alpha Particles.
 These are only hazardous to human health if they are
inhaled.
Beta Particles (b)
Carbon
C14
6 protons
8 neutrons
Nitrogen
N14
7 protons
7 neutrons
+ e-
electron
(beta-particle)
We see that one of the neutrons from the C14 nucleus
“converted” into a proton, and an electron was ejected.
The remaining nucleus contains 7p and 7n, which is a nitrogen
nucleus. In symbolic notation, the following process occurred:
n  p + e ( + n )
Beta Particles (b)
 They can travel a few feet in air but can usually be
stopped by clothing or a few centimeters of wood.
 They are considered hazardous mainly if ingested or
inhaled, but can cause radiation damage to the skin
if the exposure is large enough.
 Unstable Neutron decays into a proton.
Gamma particles (g)
 In much the same way that electrons in atoms can be in an
excited state, so can a nucleus.
 A gamma is a high energy light particle. It is NOT visible by your
naked eye because it is not in the visible part of the EM spectrum.
Neon
Ne20
10 protons
10 neutrons
(in excited state)
10 protons
10 neutrons
(lowest energy state)
+
gamma
Neon
Ne20
Gamma particles (g)
 Occurs when an unstable nucleus emits electromagnetic
radiation. The radiation has no mass, and so its emission
does not change the element.
 They penetrate matter easily and are best stopped by water
or thick layers of lead or concrete.
 Gamma radiation is hazardous to people inside and outside
of the body.
 Gamma rays have the lowest ionizing power, but the highest
penetrating power.
Half-Life
 The “half-life” (h) is the time it takes for half the atoms of
a radioactive substance to decay.
 For example, suppose we had 20,000 atoms of a
radioactive substance. If the half-life is 1 hour, how many
atoms of that substance would be left after:
10,000 (50%)
5,000 (25%)
2,500 (12.5%)
1 hour (one lifetime) ?
2 hours (two lifetimes) ?
3 hours (three lifetimes)
?
Time
#atoms
remaining
% of atoms
remaining
Lifetime(t)
 The “lifetime” of a particle is an alternate definition ofthe
rate of decay.
 The lifetime of a free neutron is 14.7 minutes.
 If there were 1000 free neutrons in a box, after 14.7
minutes some number of them will have decayed.
 The number remaining after some time is given by the
radioactive decay law-
/
0
t
N N e 
 N0 = starting number
of particles
 = particle’s lifetime
Its value is 2.718
Lifetime
Not all particles have the same lifetime.
 Uranium-238 has a lifetime of about 4.5 billion
(4.5x109) years !
 Some subatomic particles have lifetimes that are
less than 1x10-12 sec !
 Given a batch of unstable particles, we cannot
say which one will decay.
 The process of decay is statistical. That is, we can
only talk about either,
1) the lifetime of a radioactive substance*, or
2) the “probability” that a given particle will decay.
Uses of radiation
• Radioactive tracers are used to locate tumors, to study the
functioning of a particular organ, or to monitor the flow of
blood. Such as iodine-131 is used for thyroid problems.
• used to treat cancer may involve the use of implanted
radioactive isotopes such as gold-198 or iridium-192.
• Radioactive particles often used to measure the thickness of
metal goods.
• Radio isotopes often used for smoke alarms.
• Nuclear fission is used to generate Electricity.
• The age of fossil or rock or anything can be determined by radio
isotopes suck as carbon-14. though it can measure only 50,000
years.
Geiger Muller Counter
• Is used to detect
radiation
• original operating
principle was
discovered in 1908
in early radiation
research.
• However, there
are limitations in
measuring high
radiation rates.
Thank You

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Radioactivity

  • 2. Radioactivity ▪ Radioactivity also known as radioactive decay is a process in which unstable atomic nucleus loses energy by emitting radiation. ▪ Radiation is released in form of particles or electromagnetic waves. ▪ The rate of radioactive decay is described in half-lives. ▪ The main source of radiation in Earth is sun. Radiation is going through everywhere and all the time.
  • 3. Pioneers in Radioactivity Roentgen: Discoverer of X- rays 1895 Becquerel: Discoverer of Radioactivity 1896 The Curies: Discoverers of Radium and Polonium 1900- 1908 Rutherford: Discoverer Alpha and Beta rays 1897
  • 4. Type of Radioactivity By the end of the 1800s, it was known that certain isotopes emit penetrating rays. Three types of radiation were known: 1)Alpha particles (a) 2)Beta particles (b) 3)Gamma-rays (g)
  • 5. Particle Mass Charge Gamma (g) 0 0 Beta (b) ~0.5 -1 Alpha (a) ~3752 +2
  • 6. Alpha Particles (a) Radium R226 88 protons 138 neutrons Radon Rn222 This is the atomic weight, which is the number of protons plus neutrons 86 protons 136 neutrons + n np p a (4He) 2 protons 2 neutrons  The alpha-particle (a) is a Helium nucleus.  It’s the same as the element Helium, with the electrons stripped off !  A sheet of paper or human skin can stop Alpha Particles.  These are only hazardous to human health if they are inhaled.
  • 7. Beta Particles (b) Carbon C14 6 protons 8 neutrons Nitrogen N14 7 protons 7 neutrons + e- electron (beta-particle) We see that one of the neutrons from the C14 nucleus “converted” into a proton, and an electron was ejected. The remaining nucleus contains 7p and 7n, which is a nitrogen nucleus. In symbolic notation, the following process occurred: n  p + e ( + n )
  • 8. Beta Particles (b)  They can travel a few feet in air but can usually be stopped by clothing or a few centimeters of wood.  They are considered hazardous mainly if ingested or inhaled, but can cause radiation damage to the skin if the exposure is large enough.  Unstable Neutron decays into a proton.
  • 9. Gamma particles (g)  In much the same way that electrons in atoms can be in an excited state, so can a nucleus.  A gamma is a high energy light particle. It is NOT visible by your naked eye because it is not in the visible part of the EM spectrum. Neon Ne20 10 protons 10 neutrons (in excited state) 10 protons 10 neutrons (lowest energy state) + gamma Neon Ne20
  • 10. Gamma particles (g)  Occurs when an unstable nucleus emits electromagnetic radiation. The radiation has no mass, and so its emission does not change the element.  They penetrate matter easily and are best stopped by water or thick layers of lead or concrete.  Gamma radiation is hazardous to people inside and outside of the body.  Gamma rays have the lowest ionizing power, but the highest penetrating power.
  • 11. Half-Life  The “half-life” (h) is the time it takes for half the atoms of a radioactive substance to decay.  For example, suppose we had 20,000 atoms of a radioactive substance. If the half-life is 1 hour, how many atoms of that substance would be left after: 10,000 (50%) 5,000 (25%) 2,500 (12.5%) 1 hour (one lifetime) ? 2 hours (two lifetimes) ? 3 hours (three lifetimes) ? Time #atoms remaining % of atoms remaining
  • 12. Lifetime(t)  The “lifetime” of a particle is an alternate definition ofthe rate of decay.  The lifetime of a free neutron is 14.7 minutes.  If there were 1000 free neutrons in a box, after 14.7 minutes some number of them will have decayed.  The number remaining after some time is given by the radioactive decay law- / 0 t N N e   N0 = starting number of particles  = particle’s lifetime Its value is 2.718
  • 13. Lifetime Not all particles have the same lifetime.  Uranium-238 has a lifetime of about 4.5 billion (4.5x109) years !  Some subatomic particles have lifetimes that are less than 1x10-12 sec !  Given a batch of unstable particles, we cannot say which one will decay.  The process of decay is statistical. That is, we can only talk about either, 1) the lifetime of a radioactive substance*, or 2) the “probability” that a given particle will decay.
  • 14. Uses of radiation • Radioactive tracers are used to locate tumors, to study the functioning of a particular organ, or to monitor the flow of blood. Such as iodine-131 is used for thyroid problems. • used to treat cancer may involve the use of implanted radioactive isotopes such as gold-198 or iridium-192. • Radioactive particles often used to measure the thickness of metal goods. • Radio isotopes often used for smoke alarms. • Nuclear fission is used to generate Electricity. • The age of fossil or rock or anything can be determined by radio isotopes suck as carbon-14. though it can measure only 50,000 years.
  • 15. Geiger Muller Counter • Is used to detect radiation • original operating principle was discovered in 1908 in early radiation research. • However, there are limitations in measuring high radiation rates.