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radioactive isotopes a boon or curse wikipedia
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Radioactive isotpesWhat Are Radioactive Isotopes?
Before we go into discussing radioactive isotopes, let's recall what an isotope is. Let's look at the picture of an atom below - it has a nucleus made up of protons and neutrons, with electrons around the nucleus. All the atoms of an element have the same number of protons, but the number of their neutrons can differ. If this happens, then we can call these isotopes of an element. Isotopes have the same number of protons, but they differ in the number of neutrons.

Nucleus: Made of Protons and Neutrons

For instance, below, we have the isotopes of hydrogen. Here, you can see that the number of protons and electrons are the same, but for the three isotopes of hydrogen, the number of neutrons differ.

Isotopes of Hydrogen

Now that we recalled what isotopes are, what makes them radioactive? When I think about the word 'radioactive', I think about a unique and unstable type of energy. If an isotope has an unstable nucleus that breaks down to emit radiation, then these are what we call radioactive isotopes, also known as radioisotopes.

Radioactive isotopes have an unstable nucleus that decays or emits excess energy or radiation until the nucleus becomes stable. They can be naturally occurring or artificial isotopes of an element.

Uses of Radioactive Isotopes
There are about 50 naturally occurring radioactive isotopes, and the rest are artificial. We probably don't know all of the many uses these radioactive isotopes have, or the benefits they bring in various fields. What are the uses of these radioactive isotopes? Let's find out.

There are many radioactive isotopes that are very beneficial in applications in medicine. For instance, radioactive isotopes are used for radiation therapy, and for locating brain tumors.

If for instance, you need to keep track of activities of your organs, radioactive isotopes are also used here. Below is a table of some radioactive isotopes and their applications in medicine.

Some Radioactive Isotopes Used in Medicine

Food Safety
Have you ever experienced food poisoning? It is very unpleasant, so to minimize food borne illnesses and food poisoning experiences, food needs to be treated. To do this, it has to undergo irradiation, which commonly uses radioactive isotopes of cobalt-60.

Symbol Indicating Food was Treated with Radiation

Besides preventing illness, irradiating food can help it stay fresher longer because it gets rid of microorganisms and bacteria that cause early spoilage. The good news is, the irradiated food doesn't come in direct contact with the radioactive isotope, so the food won't be radioactive.

Industrial Applications
Do you ever notice when you buy paper that the thickness is uniform? Have you also ever wondered how people know where oil wells should be drilled? Different industries like steel, paper and oil industries, among others, make use of radioactive isotopes as well.

Below are some radioactive isotopes and how they are used industrially.

Industrial Uses of Some Radioactive Isotopes
Science and industry use radioisotopes in a variety of ways to improve productivity and, in some cases, to gain information that cannot be obtained in any other way.
Sealed radioactive sources are used in industrial radiography, gauging applications and mineral analysis.
Short-lived radioactive material is used in flow tracing and mixing measurements.
Various radioactive decay series are used to measure the ages of materials incorporating them.
Gamma sterilisation is used for medical supplies, some bulk commodities and, increasingly, for food preservation.
Nuclear techniques are increasingly used in science, industry and environmental management. The continuous analysis and rapid response of nuclear techniques, many involving radioisotopes, mean that reliable flow and analytic data can be constantly available. This results in reduced costs with increased product quality.
Neutron Techniques for Analysis
Neutrons from a research reactor can interact with atoms in a sample causing the emission of gamma rays which, when analysed for characteristic energies and intensity, will identify the types and quantities of elements present. The two main techniques are Thermal Neutron Capture (TNC) and Neutron Inelastic Scattering (NIS). TNC occurs immediately after a low-energy neutron is absorbed by a nucleus, NIS takes place instantly when a fast neutron collides with a nucleus.
Most commercial analysers use californium-252 neutron sources together with sodium iodide detectors and are mainly sensitive to TNC reactions. Other use Am-Be-241 sources and bismuth germanate detectors, which register both TNC and NIS. NIS reactions are particularly useful for elements such as C, O, Al & Si which have a low neutron capture cross section. Such equipment is used for a variety on on-line and on-belt analysis in the cement, mineral and coal industries.
A particular application of NIS is where a probe containing a neutron source can be lowered into a bore hole where the radiation is scattered by collisions with surrounding soil. Since hydrogen (the major component of water) is by far the best scattering atom, the number of neutrons returning to a detector in the probe is a function of the density of the water in the soil.
To measure soil density and water content, a portable device with an americium-241-beryllium combination generates gamma rays and neutrons which pass through a sample of soil to a detector. (The neutrons arise from alpha particles interacting with Be-9.) A more sophisticated application of this is in borehole logging.
Gamma & X-ray Techniques in Analysis
Gamma ray transmission or scattering can be used to determine the ash content of coal on line on a conveyor belt. The gamma ray interactions are atomic number dependant, and the ash is higher in atomic number than the coal combustible matter. Also the energy spectrum of gamma rays which have been inelastically scattered from the coal can be measured (Compton Profile Analysis) to indicate the ash content.
X-rays from a radioactive element can induce fluorescent x-rays from other non-radioactive materials. The energies of the fluorescent x-rays emitted can identify the elements present in the material, and their intensity can indicate the quantity of each element present.
This technique is used to determine element concentrations in process streams of mineral concentrators. Probes containing radioisotopes and a detector are immersed directly into slurry streams. Signals from the probe are processed to give the concentration of the elements being monitored, and can give a measure of the slurry density. Elements detected this way include iron, nickel, copper, zinc, tin and lead.
X-ray Diffraction (XRD) is a further technique for on-line analysis but does not use radioisotopes.
Gamma Radiography
Gamma Radiography works in much the same way as x-rays screen luggage at airports. Instead of the bulky machine needed to produce x-rays, all that is needed to produce effective gamma rays is a small pellet of radioactive material in a sealed titanium capsule.
The capsule is placed on one side of the object being screened, and some photographic film is placed on the other side. The gamma rays, like x-rays, pass through the object and create an image on the film. Just as x-rays show a break in a bone, gamma rays show flaws in metal castings or welded joints. The technique allows critical components to be inspected for internal defects without damage.
Gamma sources are normally more portable than x-ray equipment so have a clear advantage in certain applications, such as in remote areas. Also while x-ray sources emit a broad band of radiation, gamma sources emit at most a few discrete wavelengths. Gamma sources may also be much higher energy than all but the most expensive x-ray equipment, and hence have an advantage for much radiography. Where a weld has been made in an oil or gas pipeline, special film is taped over the weld around the outside of the pipe. A machine called a "pipe crawler" carries a shielded radioactive source down the inside of the pipe to the position of the weld. There, the radioactive source is remotely exposed and a radiographic image of the weld is produced on the film. This film is later developed and examined for signs of flaws in the weld.
X-ray sets can be used when electric power is available and the object to be x-rayed can be taken to the x-ray source and radiographed. Radioisotopes have the supreme advantage in that they can be taken to the site when an examination is required – and no power is needed. However, they cannot be simply turned off, and so must be properly shielded both when in use and at other times.
Non-destructive testing is an extension of gamma radiography, used on a variety of products and materials. For instance, ytterbium-169 tests steel up to 15 mm thick and light alloys to 45 mm, while iridium-192 is used on steel 12 to 60 mm thick and light alloys to 190 mm.
The radiation that comes from a radioisotope has its intensity reduced by matter between the radioactive source and a detector. Detectors are used to measure this reduction. This principle can be used to gauge the presence or the absence, or even to measure the quantity or density, of material between the source and the detector. The advantage in using this form of gauging or measurement is that there is no contact with the material being gauged.
Many process industries utilise fixed gauges to monitor and control the flow of materials in pipes, distillation columns, etc, usually with gamma rays.
The height of the coal in a hopper can be determined by placing high energy gamma sources at various heights along one side with focusing collimators directing beams across the load. Detectors placed opposite the sources register the breaking of the beam and hence the level of coal in the hopper. Such level gauges are among the most common industrial uses of radioisotopes.
Some machines which manufacture plastic film use radioisotope gauging with beta particles to measure the thickness of the plastic film. The film runs at high speed between a radioactive source and a detector. The detector signal strength is used to control the plastic film thickness.
In paper manufacturing, beta gauges are used to monitor the thickness of the paper at speeds of up to 400 m/s.
When the intensity of radiation from a radioisotope is being reduced by matter in the beam, some radiation is scattered back towards the radiation source. The amount of 'backscattered' radiation is related to the amount of material in the beam, and this can be used to measure characteristics of the material. This principle is used to measure different types of coating thicknesses.
Gamma sterilisation
Gamma irradiation is widely used for sterilising medical products, for other products such as wool, and for food. It kills bacteria and does not damage packaging. Cobalt-60 is the main isotope used, since it is an energetic gamma emitter. It is produced in nuclear reactors, sometimes as a by-product of power generation.
Large-scale irradiation facilities for gamma sterilisation are used for disposable medical supplies such as syringes, gloves, clothing and instruments, many of which would be damaged by heat sterilisation. Such facilities also process bulk products such as raw wool for export from Australia, archival documents and even wood, to kill parasites. Currently ANSTO in Australia sterilises up to 25 million Queensland fruit fly pupae per week for NSW Agriculture by gamma irradiation. See also The Peaceful Atom.
Smaller gamma irradiators are used for treating blood for transfusions and for other medical applications. They often use caesium-137, with gamma rays about half as energetic as cobalt’s.
Food preservation is an increasingly important application, and has been used since the 1960s. In 1997 the irradiation of red meat was approved in USA. Some 41 countries have approved irradiation of more than 220 different foods, to extend shelf life and to reduce the risk of food-borne diseases.
Scientific Uses
Radioisotopes are used as tracers in many research areas. Most physical, chemical and biological systems treat radioactive and non-radioactive forms of an element in exactly the same way, so a system can be investigated with the assurance that the method used for investigation does not itself affect the system. An extensive range of organic chemicals can be produced with a particular atom or atoms in their structure replaced with an appropriate radioactive equivalent.
Using tracing techniques, research is conducted with various radioisotopes which occur broadly in the environment, to examine the impact of human activities. The age of water obtained from underground bores can be estimated from the level of naturally occurring radioisotopes in the water. This information can indicate if groundwater is being used faster than the rate of replenishment. Trace levels of radioactive fallout from nuclear weapons testing in the 1950s and 60s is now being used to measure soil movement and degradation. This is assuming greater importance in environmental studies of the impact of agriculture.
Analysing the relative abundance of particular naturally-occurring radioisotopes is of vital importance in determining the age of rocks and other materials that are of interest to geologists, anthropologists and archaeologists. Dating techniques include: K-Ar (potassium-argon and its more recent variant Ar-40/Ar-39), Rb-Sr (rubidium-strontium), Sm-Nd (samarium-neodymium), Lu-Hf (lutetium-hafnium), and U-Pb (uranium-lead and its variant Pb-Pb).

One common application is in determining the age of carbon-containing materials up to about 20,000 years by measuring the abundance of carbon-14, or its beta signature. This is a naturally-occurring radioisotope formed in the upper atmosphere by cosmic rays converting nitrogen into C-14, also known as radiocarbon. Living organisms are constantly incorporating CO2 with this C-14 into their bodies along with other carbon isotopes (mostly C-12). When the organisms die, they stop incorporating new C-14, and the constituent C-14 starts to turn back into N-14 by beta decay. Carbon dating of groundwater works similarly, the decay timer starting when the water with dissolved CO2 leaves the atmosphere. The half-life of C-14 is 5730 years.
Tracing/Mixing Uses
Even very small quantities of radioactive material can be detected easily. This property can be used to trace the progress of some radioactive material through a complex path, or through events which greatly dilute the original material. In all these tracing investigations, the half-life of the tracer radioisotope is chosen to be just long enough to obtain the information required. No long-term residual radioactivity remains after the process.
Sewage from ocean outfalls can be traced in order to study its dispersion. Small leaks can be detected in complex systems such as power station heat exchangers. Flow rates of liquids and gasses in pipelines can be measured accurately, as can the flow rates of large rivers.
Mixing efficiency of industrial blenders can be measured and the internal flow of materials in a blast furnace examined. The extent of termite infestation in a structure can be found by feeding the insects radioactive wood substitute, then measuring the extent of the radioactivity spread by the insects. This measurement can be made without damaging any structure as the radiation is easily detected through building materials.
Industries and scientific establishments utilise radioactive sources for a wide range of applications. When the radioactive sources used by industry no longer emit enough penetrating radiation for them to be of use, they are treated as radioactive waste. Sources used in industry are generally short-lived and any waste generated can be disposed of in near-surface facilities.
Some industrial activities involve the handling of raw materials such as rocks, soils and minerals that contain naturally occurring radioactive materials. These materials are known by the acronym "NORM". Industrial activity can sometimes concentrate these materials and therefore enhance their natural radioactivity (hence the further acronym: TENORM - technically-enhanced NORM). This may result in:
A risk of radiation exposure to workers or the public
Unacceptable radioactive contamination of the environment
The need to comply with regulatory waste disposal requirements
See also NORM information paper.
The main industries that result in NORM contamination are:
Oil and gas operations
Oil and gas exploration and production generates large volumes of water containing dissolved minerals. These minerals may be deposited as scale in piping and oil field equipment or left as residues in evaporation lagoons. Occasionally the radiation dose from equipment contaminated with mineral deposits may present a hazard. More significantly contaminated equipment and the scale removed from it may be classified as radioactive waste. Oil and gas operations are the main sources of radioactive releases to waters north of Europe for instance.
Coal burning
Most coal contains uranium and thorium, as well as other radionuclides. The total radiation levels are generally about the same as in other rocks of the Earth's crust. Most emerge from a power station in the light flyash. Some 99% of flyash is typically retained in a modern power station (90% in some older ones) and this is buried in an ash dam. Many hundred million tonnes of coal ash is produced globally each year.
Phosphate Fertilisers
The processing of phosphate rock to produce phosphate fertilizers (one end product of the phosphate industry) results in enhanced levels of uranium, thorium and potassium.
Process and Waste Water Treatment
Radionuclides are leached into water when it comes into contact with uranium and thorium bearing rocks and sediments. Water treatment often uses filters to remove impurities. Hence, radioactive wastes from filter sludges, ion-exchange resins, granulated activated carbon and water from filter backwash are part of NORM.
Scrap metal industry
Scrap metal from various process industries can also contain scales with enhanced levels of natural radionuclides. The exact nature and concentration of these radionuclides is dependent on the process from which the scrap originated.
Metal smelting sludges
Metal smelting slags, especially from tin smelting, may contain enhanced levels of uranium and thorium series radionuclides.
Following the operation of a particle accelerator, the facility will generally be decommissioned. As radioactive materials will be present in the facility, these must be treated as radioactive wastes and handled accordingly. Following a 40 year operation of one of the new generation of particle accelerators, the volume of decommissioning waste and activity is expected to be within the same order of magnitude as for a 1 GW(e) nuclear power plant which has operated over 40 years. However, it should be noted that the concentration of radioactivity is more evenly distributed in the case of such an accelerator facility.
Radiation sources utilised within universities and research institutions also require appropriate management and disposal. Many sources are of low activity and/or short half-life. However some exceptions include high-level long-lived sources such as Radium-226 and Americium-241 used in biological and or agricultural research. These require long-term management and disposal as Intermediate-Level Wastes (ILW).
Industrial Radioisotopes
Naturally-occurring radioisotopes:
Carbon-14: Used to measure the age of wood and other carbon-containing materials (up to 20,000 years) and subterranean water (up to 50,000 years).
Chlorine-36: Used to measure sources of chloride and the age of water (up to 2 million years).
Lead-210: Used to date layers of sand and soil up to 80 years.
Tritium (H-3): Used to measure 'young' groundwater (up to 30 years).
Artificially-produced radioisotopes:
Used in backscatter gauges, smoke detectors, fill height detectors and in measuring ash content of coal.
Used for radiotracer technique for identification of sources of soil erosion and deposition, in density and fill height level switches. Also for low-intensity gamma sterilisation.
Used to label sand to study coastal erosion, also a tracer in study of blood.
Cobalt-60, Lanthanum-140, Scandium-46, Silver-110m, Gold-198:
Used together in blast furnaces to determine resident times and to quantify yields to measure the furnace performance.
Widely used for gamma sterilisation, industrial radiography, density and fill height switches.
Gold-198 & Technetium-99m:
Used to study sewage and liquid waste movements, as well as tracing factory waste causing ocean pollution, and to trace sand movement in river beds and ocean floors.
Used to label sand to study coastal erosion.
Hydrogen-3 (Tritiated Water): Used as a tracer to study sewage and liquid wastes.
Used in gamma radiography to locate flaws in metal components.
Used for industrial gauging.
Used to predict the behaviour of heavy metal components in effluents from mining waste water.
Used in light sensors in cameras and plasma display, also electronic discharge prevention and in electron capture detectors for thickness gauges.
Used in gamma radiography and non-destructive testing.
Used for industrial gauging.
Used for industrial gauging.
Used in gamma radiography and non-destructive testing.
Used to predict the behaviour of heavy metal components in effluents from mining waste water.
What Are Radioisotopes?
Many of the chemical elements have a number of isotopes. The isotopes of an element have the same number of protons in their atoms (atomic number) but different masses due to different numbers of neutrons. In an atom in the neutral state, the number of external electrons also equals the atomic number. These electrons determine the chemistry of the atom. The atomic mass is the sum of the protons and neutrons. There are 82 stable elements and about 275 stable isotopes of these elements.
When a combination of neutrons and protons, which does not already exist in nature, is produced artificially, the atom will be unstable and is called a radioactive isotope or radioisotope. There are also a number of unstable natural isotopes arising from the decay of primordial uranium and thorium. Overall there are some 1800 radioisotopes.
At present there are up to 200 radioisotopes used on a regular basis, and most must be produced artificially.
Radioisotopes can be manufactured in several ways. The most common is by neutron activation in a nuclear reactor. This involves the capture of a neutron by the nucleus of an atom resulting in an excess of neutrons (neutron rich).
Some radioisotopes are manufactured in a cyclotron in which protons are introduced to the nucleus resulting in a deficiency of neutrons (proton rich).
The nucleus of a radioisotope usually becomes stable by emitting an alpha and/or beta particle. These particles may be accompanied by the emission of energy in the form of electromagnetic radiation known as gamma rays. This process is known as radioactive decay.
Radioisotopes have very useful properties: radioactive emissions are easily detected and can be tracked until they disappear leaving no trace. Alpha, beta and gamma radiation, like x-rays, can penetrate seemingly solid objects, but are gradually absorbed by them. The extent of penetration depends upon several factors including the energy of the radiation, the mass of the particle and the density of the solid. These properties lead to many applications for radioisotopes in the scientific, medical, forensic and industrial fields.
Radioactivity is the spontaneous emission of energy from unstable atoms. Atoms are found in all natural matter. There are stable atoms, which remain the same forever, and unstable atoms, which decay or 'decay' into new atoms. It is said that these unstable atoms are "radioactive", since they emit radioactivity from the nucleus as they decompose.
The isotopes of an element are all atoms that have in their nucleus the number of protons (atomic number) that correspond to the chemical behavior of that element. However, the isotopes of a single element vary in the number of neutrons in their nuclei. Since they still have the same number of protons, all these isotopes of an element have an identical chemical behavior. But since they have different numbers of neutrons, these isotopes of the same element may have different radioactivity.
Some important uses of radioisotopes (usually called radionuclides) are:
• Radioisotopes are widely used in medicine, as tracers that appear in X-ray film, and sometimes to destroy cancerous growths.
• They are also widely used in the industry. The radiation emitted by different radio isotopes can be used for fast and high-precision measurement of the thickness of the material, including the thickness of the plates or coatings. The purity or composition of the materials can be established by means of radioisotopes. Radioisotopes are used as sources of gamma rays to irradiate and sterilize materials.
• In agriculture, radioisotope tracers can be used to verify the proper distribution of insecticides.
• Radioisotopes are used to detect pipe leaks and trace groundwater.
• Natural radioisotopes can be detected in forensic science to help solve crimes.
• Radioisotopes of natural origin are also used by archaeologists and related specialists to help establish the authenticity and age of the specimens.
• Naturally occurring radioisotopes are often used by geologists to establish the ages of rocks.

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