TOPIC: RADIOACTIVITY AND NUCLEAR ENERGY
Radioactivity
Radioactivity is the spontaneous emission of radiation by an element. Such an element is called a radioactive element.
Discovery of radioactivity
Radioactivity was discovered by Henri Becquerel, a Physicist, and the phenomenon was named by Marie Curie who also discovered the elements thorium, polonium and radium. Presently more than 40 naturally occurring radioactive elements have been discovered.
Radioactive reactions are also called nuclear reactions
Differences between nuclear reactions and ordinary chemical reaction.
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Nuclear reaction |
Chemical reaction |
1. |
It involves the nucleus (nuclear particles) of the atom
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It involves the valence electrons of the atom |
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Large amount of energy change is involved
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It involves low amount of energy change |
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It involves the decomposition of the nucleus |
It involves the transfer, loss, gain and sharing of electrons
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The rates of reactions are not affected by temperature and pressure
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The rates of reactions are affected by temperature and pressure
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Does not involve the breaking or forming of bonds involved |
It involves the breaking of old bonds and formation of new ones
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The reactions are irreversible |
They could be reversible or irreversible
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TYPES OF RADIATION
There are three major types of Radioactive radiation
1. alpha(α-) radiation
2. beta(β-) radiation and
3. gamma(γ) radiation/rays.
1. Alpha rays/radiation
These are fast moving stream of positively charged particles, that resembles the helium nucleus.
Properties of alpha rays
1. They are positively charged particles
2. They have low penetrating power (they can be stopped by a thin sheet of paper)
3. They have strong ionizing power (ionizing any gas through which they pass).
4. They cause fluorescence in some materials e.g ZnS
5. They have a mass number of 4 and atomic number of 2
2.Beta Rays
These are very fast moving streams of electrons.
They have velocities close to that of visible light.
Properties
1. They are negatively charged.
2. They have higher penetrating power than alpha particles ( can be blocked by a thin sheet of aluminum foil)
3. They have lower ionizing power than alpha particles.
4. They cause florescence in substances like anthracence but not zinc sulphide.
5. They are deflected toward the positive plates in an electrostatic field
Gamma Rays
Gamma rays/radiations are electromagnetic waves similar to visible light but with shorter wavelengths.
Properties
1. They have the highest penetrating power of the three particles ( they can be blocked by a thick block of Lead)
2. They travel with the speed of light.
3. They are not affected by an electrostatic field.
4 They do not have charge nor mass.
5. They have the least ionizing power among the three particles.
Summary of the properties of alpha, beta and gamma rays
Alpha ray |
Beta ray |
Gamma ray |
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Nature Electrical Charge Mass Velocity Relative penetration Absorber |
Helium nuclei 42He +2 4 units About 1/20 the speed of light 1 Thin paper |
Electron o-1e -1 1/1840 units Varies (from 3 – 99% of the speed of light) 100 Metal plate |
Electromagnetic radiation No charge No mass Speed of light 10,000 Large lead Block |
Other types of radiations include
X – rays
X – rays are electromagnetic waves, that resembles visible light, but with a shorter wavelength. They are produced when fast moving electron knock out electrons from the inner shells of metal atoms and electrons from a higher/outer shell then falls down to replace the knocked – out electrons. This movement of electrons is accompanied by the emission of x – rays.
Properties and uses of x – rays
1. X – rays can penetrate readily through most solid substances such as wood, foils, flesh and paper, which are opaque to visible light.
Hard x – rays have greater penetrating power than soft x – rays.
2. Soft x – rays are used in medicine to photograph human parts while hard x – rays are used for destroying cancerous cells.
3. X – rays are used to study the arrangement of particles in crystal lattices in chemistry and in big organic molecules like proteins.
DETECTION OF RADIATIONS
Different types of devices have been developed over the years for detecting radiation. The most commonly used detectors are:
i. Geiger-Muller counter,
ii. the scintillation counter and
iii. photographic plate or solution,
iv. Diffusion cloud chambers
Others include:
4. The pulse (wulf) electroscope
5. Solid state detector
6. Photographic plate or solution
7. Dekatron counter.
When a certain quantity of a radioactive material disintegrates spontaneously the word decay is used. During the decay, there is usually an emission of alpha – or beta particles. Sometimes, gamma rays also accompany the emission of these particles. The outcome of the disintegration is that the parent nucleus (nucleus undergoing disintegration) undergoes a change in the atomic number and become the nucleus of a different element.
TYPES OF DECAY
Alpha Decay: When the nucleus of an atom loses an α-particle. i.e. a helium nucleus (42He) during disintegration, the atomic number of the atom is reduced by two units and its mass number by four units, e.g.
when an atom of uranium 238, loses an alpha particle, it will become an atom of thorium Tℎ. The nuclear reaction is written thus:
23892U →23490Th + 42He (α-partcle)
The atom undergoing decay is called the parent cell while the new element (atom) formed is called the daughter cell.
Beta Decay: this kind of radioactive change is equivalent to the splitting of a neutron in the atomic nucleus of the radioactive element into an electron and a proton. The proton remains in the nucleus while the electron is expelled out of the nucleus as beta particles. The mass number does not change but the atomic number increases by one.
For example, if a thorium nucleus Th emits a β particle, its nucleus changes into a nucleus of the element protactinium whose mass number is the same as that of thorium but whose atomic number is increased by one unit from 90 to 91.
23490Tℎ →23491Pa + 0-1β-particle
Gamma Decay: Gamma decay involves only the release of large amount of energy and does not involve change in the mass number or atomic number. It always accompanies an α or β decay.
Radioactive decay series
The nucleus of the daughter element formed most times by transmutation is itself unstable, and will undergo further disintegration after some time. This time may vary from few microseconds to millions of years and it is known as HALF-LIFE. This series of changes may occur until a stable nucleus is finally formed. Examples is the uranium series, the thorium series and actinium series, each of which is named after the longest-lived element in the series.
Element and radiation emitted Isotope Half-life
Uranium
↓ α 4.5×106years
Thorium
↓ β ℎ 24.1 days
Protactinium
↓ β 1.18 minutes
Uranium
↓ α 2.5×105years
Thorium
↓ α ℎ 8.0×104years
Radium
↓ α 1622 years
Radon
↓ α 3.8 days
Half Life as a Factor of Stability of Nucleus
The half-life of a radioactive element is the time taken for half of the total number of atoms in a given sample of the elements to decay.
For example, the half-life of radium-226 is 1622 years. This means that if we have one thousand radium atoms at the beginning, then at the end of 1622 years, 500 atoms would have disintegrated, leaving 500 undecayed radium atoms. In the next 1622 years, half the remaining atoms i.e. 250 would have disintegrated, leaving 250 undecayed atoms of radium and so on.
The stability of an atomic nucleus is related to the ratio of neutrons to protons in the nucleus. Atoms with neutron-proton ratio less than 1 or greater than 1.5 tend to be unstable and undergo radioactive radiation.
Nuclear Chemistry and Reactions
Nuclear chemistry is concerned with reactions that involve the nucleus. When nuclear particles like proton, neutrons, alpha and beta particles as well as electrons and gamma rays are used as bullets for bombarding the nuclei of some atoms, one or two of the following events may take place:
a) Artificial radio isotopes may be created
b) Atomic transmutation may occur
This transmutation is the process by which radioactive elements change into different elements.
Artificial Transmutation
Because large amount of heat is released from radioactive disintegration, scientists, devised a means of tapping, harnessing, controlling, and using this large amount of energy. This results in artificial transmutation since the natural transmutation is not subject to human control i.e. spontaneous. In 1919, Ernest Rutherford succeeded in transmuting a nitrogen isotope into an oxygen isotope by bombarding the nitrogen isotope with alpha particles.
147N+ 42α → 178O + 11P
Proton
Many atomic transmutations can be carried out by bombarding different elements with fast-moving atomic particles like neutrons, protons, deuterons (nuclei of deuterium atoms) and alpha particles. The neutron is a very effective bombarding particle because it is heavy and has no charge.
Generally, when light elements are bombarded by neutrons, new elements are formed by ejecting charged particles.
But, if the nucleus being bombarded is heavy, it captures the neutron to produce an isotope of the original
element. +
Nuclear Fission
Nuclear fission is a process in which the nucleus of a heavy element is split into two nuclei of nearly equal mass with a release of energy and radiation.
Nuclear Fusion
Nuclear fusion is a process in which two or more light nuclei fuse or combine to form a heavier nucleus with the release of energy and radiation.
It is the opposite of nuclear fission. The energy released during nuclear fusion is greater than the energy released during nuclear fission because of the differences in the binding energies of the isotope.
This principle is applied in the making of hydrogen bombs. The sun and stars also obtain their energy from nuclear fusion reactions.
1n 1939, a German nuclear scientist (Halm) discovered that atomic nucleus of isotopes of uranium could absorb a neutron and then break into two (atomic fission) e.g.
He noticed that the total products of fission have a slightly different mass from that of the total initial material. This difference in mass is radiated as energy, and the amount of energy is given by Einstein in the equation E = mc2
where E= energy in joules,
m= mass in Kg
and c = velocity of light in s-1.
A large amount of energy is released during nuclear fission This energy released can now be harnessed during nuclear reactions and are used in power stations to generate electricity and nuclear submarines.
Uses Of Radioactive Isotopes
1. Medical Uses:
a. It is used for the treatment of cancer, radioactive isotopes like
(i). cobalt 60 for treating tumors and destroying cancerous cells
(ii). Iodine – 131 for treating cancer of the thyroid gland and
(iii). phosphorus -32 for treating leukemia
b. Alpha rays are used in the sterilization of hospital equipment and in the pasteurization of foods.
2. Agricultural purposes: radiation is used in insect and pest control. This is done by sterilizing the male pupae of an undesirable insect by radiation, so that sterile male adults are produced. They are then released in large numbers to mate with the native female adults which will lay unfertilized eggs.
3. Radioactive tracers: due to continuous emission of radiation by a radioactive isotope it is possible to trace its position and also to measure its concentration using a sensitive counter. And so when a small quantity of a radioactive isotope is mixed with its stable isotope it is possible to follow its path through a series of changes or reactions . This technique has been used to study many metabolic processes in both plants and animals e.g.
(i). the uptake of iodine by the thyroid gland using iodine-131
(ii). photosynthesis using carbon-14 in the form of carbon (IV)oxide.
(iii). In medicine for tracing the movement of materials or food through the alimentary canal.
4. It is used in generating electricity from nuclear reaction occurring in nuclear power stations/ plants.
5. In Radiological Dating: Radioactive carbon-14 isotope (with half-life of about five thousand years) is used for determining the age of organic materials. The process involves measuring the amount of carbon-14 present in the specimen and the age is determined from this value and the half-life of the isotope.
The presence of very long – lived radioisotope ( e.g uranium 238 with a half-life of 4.5×109 years) present in the earth crust is utilized by geologists to estimate the age of rocks and archaeological objects. It is also used in distinguishing genuine antiquities from fake ones.
OBJECTIVE QUESTIONS
1. Equation? 23490Th → yxPa + β- particle
X Y
a. 91 234
b. 92 235
c. 89 235
d. 88 238
2. A radioactive solid is best stored
a. Under paraffin oil
b. Under ultraviolet light
c. In a cool, dark cupboard
d. In a box lined with lead
3.
Briefly discuss the following
- Atomic pile and atomic bomb
- Binding energy
- Nuclear energy for power