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RADIOISOTOPE METHODS



THREE TYPES OF RADIOACTIVE DECAY
There are three main types of radiation:
o                Alpha radiation
o                Beta radiation
o                Gamma radiation

Alpha Decay
The reason alpha decay occurs is because the nucleus has too many protons which cause excessive repulsion. In an attempt to reduce the repulsion, a Helium nucleus is emitted. The way it works is that the Helium nuclei are in constant collision with the walls of the nucleus and because of its energy and mass, there exists a non zero probability of transmission. That is, an alpha particle (Helium nucleus) will tunnel out of the nucleus.

Properties of Alpha Radiation
·                α-particles are no particularly dangerous unless they are swallowed or breathed in.
·                since  α radiations cannot pass through clothing.
·                But cells they are very damaging.


Alpha Decay of Americium-241 to Neptunium-237

Beta Decay
Beta decay occurs when the neutron to proton ratio is too great in the nucleus and causes instability. In basic beta decay, a neutron is turned into a proton and an electron. The electron is then emitted. Here's a diagram of beta decay with hydrogen-3:


Alpha Decay of Hydrogen-3 to Helium-3. 

There is also positron emission when the neutron to proton ratio is too small. A proton turns into a neutron and a positron and the postiron is emitted. A positron is basically a positively charged electron. Here's a diagram of positron emission with carbon-11:


Positron Decay of Carbon-11 to Boron-11. 
The final type of beta decay is known as electron capture and also occurs when the neutron to proton ratio in the nucleus is too small. The nucleus captures an electron which basically turns a proton into a neutron. Here's a diagram of electron capture with beryllium-7:


Electron Capture of Beryllium-7. 

Properties of Beta Radiations
·                Beta radiations have much greater range.
·                Hard beta could pass through a few centimeter of lead and have considerable range in air.
·                So beta emissions can produce dangerous radiation even at distances from the source.

Gamma Decay
Gamma decay occurs because the nucleus is at too high an energy. The nucleus falls down to a lower energy state and, in the process, emits a high energy photon known as a gamma particle. Here's a diagram of gamma decay with helium-3:
Properties of Gamma Radiations
·                Gamma radiations are the most penetrating of all and can pass through many metres of even concrete.
·                Since their ionizing power is the least of all and many will go through the body without effect.
Gamma Decay of Helium-3




HALF LIFE AND RADIOACTIVITY

Atoms
An atom is smallest particle of an element capable of entering into a chemical reaction. It consists of a nucleus and orbital electrons. The Nucleus which contains neutrons and protons, small, central, positively charged region of an atom that carries essentially all the mass. Except for the nucleus of ordinary (light) hydrogen, which has a single proton, all atomic nuclei contain both protons and neutrons.

The number of protons determines the total positive charge, or atomic number; this is the same for all the atomic nuclei of a given chemical element. The total number of neutrons and protons is called the mass number.

A nuclide is a species of atom characterized by its mass number, atomic number, and energy state of its nucleus, provided that the atom is capable of existing for a measurable time.

Isotopes
Isotopes are nuclides having the same number of protons (same atomic number) in their nuclei, but differing in the number of neutrons (different mass number). Isotopes of a particular element exhibit almost identical chemical properties.

Radioisotopes
 A radioisotope is an atom with an unstable ratio of neutrons to protons in its nucleus. In an attempt to reorganize to a more stable state, it may undergo various types of rearrangement that involve the release of radiation. A radioisotope is a radioactive material. Radioactive material is any material that emits radiation spontaneously. Radioisotopes provide an easily traced “label” in various chemical compounds. Radioactive decay is the disintegration or transformation of the nucleus of an unstable nuclide by the spontaneous emission of charged particles and photons.

Units of Radioactivity
The curie is the quantity of any radioactive material in which the number of nuclear transformations is 3.7 x 1010 per second. The unit is abbreviated Ci. The becquerel is the international (SI) unit for radioactivity. One becquerel is equal to one nuclear transformation per second. A becquerel is about 2.7 x 10-11 curies. Common metric prefixes are used to denote multiples of the curie and the becquerel. A thousandth of a curie is known as a millicurie (mCi). A millionth of a curie is known as a microcurie (µCi). A microcurie is 3.7 x 104 or 37 kilobecquerels.

Radioactivity and Half life

          Radioactive materials have an associated half-life, or decay time characteristic of that isotope. As radiation is emitted, the material becomes less radioactive over time, decaying exponentially. Since it is impossible or impractical to measure how long one atom takes to decay, the amount of time it takes for half of the total amount of radioactive material to decay is used to calculate half-life. Some radioisotopes have long half-lives; for example, Carbon-14 takes 5,730 years for any given quantity to decay to half of the original amount of radioactivity. Other radioactive materials have short half-lives; Phosphorus-32 has an approximately two-week half-life, and Technetium-99m (used in human and animal nuclear medicine diagnostic procedures) has a half-life of 6 hours. Half-life is important for many reasons. When deposited in the human body, the half-life of the radioactive material present in the body affects the amount of the exposure. Materials with shorter half-lives typically cause less dose for a given activity than materials with longer half-lives. If the radioactive material contaminates a workbench or equipment, and is not removable, the amount of time before the contaminated items may be used again is determined by the radioactive half-life. Radioisotope decay (using shorter half-life isotopes) helps to minimize costs in radioactive waste management.
The equation used to calculate radioactive decay is shown below.
A = A0 e-λt
Where:
A = Current amount of radioactivity
A0 = Original amount of radioactivity
e = base natural log (approximately 2.718)
λ = decay constant = 0.693/t1/2 (where t1/2 = half-life)
t = the amount of time elapsed from A0 to A

Half life

The radioctive isotopes are characterized by their half life. The decay of radioisotopes is irreversible and is independent of any physical parameters such as temperature and pressure. The rate of decay always follows the exponential law. That is, the number of atoms disintegrating at any given time is directly proportional to the total number of atoms present at that time.

Half life (T1/2) is the time required for the radioactivity to be reduced to one half of its original value. This is also known as physical half life (Tp)

(T1/2)  =  0.693/λ
Where λ is radioactive decay constant

Biological half life (Tb)

Biological half life is defined as the normal amount of time required for the turnover of one half of the body content of a given radioactive or non radioactive element.

Effective half life (Te)

When radioactive isotopes are used in in vivo experiments, the turnover rate of the element in the body must also be considered. Therefore the rate of decay of radioactivity will be a function of both radioactive decay and metabolic turnover which is known as effective half life and denoted as Te.
                             Effective half life (Te)   =   (Tb) x  (Tp)  /  (Tb)  +  (Tp)  



GEIGER-MULLER COUNTER (GM COUNTER)
The radioactivity of isotopes can be measured either by using counting devices or by photographic method (autoradiography). The quantity determination of radioactivity is based on the ionization or excitation of matter induced by radiations emanated from radioactive elements. GM counter is an important instruments used to determine radioactivity of substances.

This instrument works on the principle of ionization of gases & is suitable for all kinds of radiations. The basic advantage of GM counter is derived from the amplification (each primary ion pair yields close to 100 million secondary ion pairs). The amplification is so great that an extremely simple external electronic amplifier is sufficient. This simplicity imparts stability to GM counter.

It consists of a simple & very compact ionization chamber made of glass with two electrodes. It is filled with a gas usually argon, neon or air.The outer electrode (cathode) is a metal tube formed by brass or nickel with 1-5 cm diameter & 10-50 cm length.The inner electrode (anode) is a fine wire of tungsten with 0.1-0.5 mm thickness. The anode is stretched along the axis of the tube & well-insulated by ebonite plugs. When radiation enters the tube, the gas is ionized rapidly under a high voltage power supply resulting in an electric pulse. But, the discharge of the pulse terminates when large quantity of positive ions get collected around the negative electrode & this prevents the occurrence of further ionization.

To accelerate the process of ionization, GM tubes contain a quenching gas. However, presence of a quenching gas & the window through which the particles pass into the tube restrict sthe entrance of radiation thereby reducing the efficiency of the detector. To overcome this problem, GM tubes with very thin windows or with no windows have been developed. But the windowless GM tubes require a continuous flow of special quenching gas through the tube.


Counter Tubes
The choice of counter tubes to be used depends on the nature of the sample to be counted (whether the sample is solid or liquid, whether it is soft or high energy β-emitter etc.)

Proportional Counter
It is a modified GM tube which operates in a region of applied current where the charge produced is proportional to the initial ionization. This device is more advantageous than GM counter because it has greater stability & reproducibility & can operate at reduced voltage.
The consumption of quenching gas is lesser in proportional counter than in GM tube. This device produces continuous pulses which enable very fast counting. The most popular proportional counter is the ‘flow counter‘ in which a gas like argon or indane is continuously.

Optimum voltage
          The GM counter should be operated only in the voltage region known as “Geiger – Muller region”. It is the voltage range where a small increase or decrease in voltage does not affect the counting rate. When the applied voltage is plotted against cout rate, the first region is known as “recombination region”. As the voltage is low, the ionized gas molecules recombine. When the voltage is increased further, the gas molecules ionize and stay in their ionized state without showing any increase in the count rate. This region is called “simple ionization region”. As the voltage is increased still further, the count rate increases proportionately with increase in voltage and hence this region is known as the “proprrtional region”. The counters based on the region are known as proportional counters.

          A further increase in voltage does not affect the count rate. At this threshold voltage, the rise in count rate begins to level off into plateau and is stable for about 300 volts length(the precise length depends on a particular tube). This region is known as “Geiger muller region” at which the Geiger muller counter is operated. Still higher voltages lead to a sudden sharp rise in the count rate. At this voltages the potential across electrodes is so high that spontaneous discharges occur in the tube which are not due to radioactivity. This region is known as “continuous discharge region”. The tube should never be operated at the continuous discharge region because the tube will get irreparably damaged.







SCINTILLATION COUNTING METHODS
Scintillation counting is based on the observation that certain chemical substances emit flashes of light on exposure of radiation. The measurement of these flashes of light is the basis of the method called scintillation counting. Depending upon the type of scintillator used for counting the radioactivity, they are classified into two types:
i.               solid scintillation counting
ii.             liquid scintillation counting



i.               Solid scintillation counting
Solid scintillation counter is ideal for gamma emitters. The counter consists of a large crystal of sodium iodide containing small amount of thallium iodide and an assembly of photomultiplier, preamplifier, a source of high voltage and a scaler encased in an aluminum casing. The radioactive sample is placed into a well shaped opening drilled into the crystal surface. The crystal absorbs much of the energy of the gamma rays which causes excitation of electrons of the atoms composing the crystal. The excited electrons rise to higher energy orbital. As these electrons return to normal level, the absorbed energy is discharged as flashes of light or scintillation.

The light (photons) is converted into electrical signals by the photomultiplier tube, amplified and is registered es counts by the scaler.

ii.             Liquid scintillation counting
Liquid scintillation counters are especially useful in measuring soft β emittors such as 3H, 35S and 14C, as these compounds cannot be measured efficiently using a G-M counter or a gamma counter.

A liquid scintillation counter consists of two photomultiplier tubes one on either side of a scintillation vial and enclosed in a light tight lead shield. The photomultiplier tubes are connected to a scaler through a high voltage power supply, a coincidence counting circuit and a pulse height analyzer.

The radioactive sample to be counted is mixed in a glass or plastic vial with “scintillation fluid”. The scintillation fluid contains three components:
i.               An organic solvent
ii.             A primary flour and
iii.           A secondary flour
The energy of the β particle is first transferred to the organic solvent which causes excitation of solvent molecules. When the excited solvent molecules returned to ground state, energy is transferred to the primary flour viz., 2,5 diphenyl oxazole (PPO) causing excitation of PPO. On returning to ground state, the primary flour emits photons in the UV region. The photocathodes of the photomultiplier tube are not sensitive enough to capture these photons. Hence a secondary flour viz., 1,4 bis (5-phenyloxazole-2)benzene (POPOP), is used to absorb the energy from the primary flour and reemit it as light of longer wavelength, which is close to the maximum sensitivity region of the photomultiplier tube. The size of the electrical pulse produced by the photomultiplier tube is proportional to the energy of β-particle absorbed by the scintillation fluid. The sequence of transfer of radiation energy from the radioactive material.

Liquid scintillation counters are ideal for low energy β-emitters e.g. 3H, 35S, 14C, 32P, etc. These counters can also be used for counting dual or triple labeled samples.

Composition of Scintillation fluid

The scintillation fluid contains 0.5% PPO and 0.01% POPOP in Analar scintillation grade toluene. The fluid (̴ 10 ml) is used per vial for counting. The radioactive samples to be counted are usually spotted (1-50 µl) on Whatman No.3 discs and are dried in a hot air oven or under infrared lamp. Then these discs are placed inside the vials containing the scintillation fluid and counted. The radioactive samples in small volume 1-5 µl can also be counted, by directly pipetting the volume inside the scintillation fluid. Large volumes cannot be counted directly because water quenches the counting. Hence larger volumes (upto 100 µl) can be spotted on Whatman No.3 discs, dried and then counted.



Cerenkov counting
Radioactive isotopes which produce β-particles with >265 KeV can be counted directly in liquid scintillation counter without the help of scintillation fluid. Modern photomultipliers accept about one third of the light energy emitted by these isotopes and is known as cerenkov radiation.

Background radiation
In liquid scintillation counting, even in the absence of any radioactive material added to the vials, some counts are always registered by the counter (̴ 50 counts). This is known as background counts. The background counts are derived from a number of sources such as
i.               Low aptitude signals arising spontaneously within the photomultiplier tubes.
ii.             Naturally occuring radio isotopes in the vial and in the scintillation fluid the organic solvents may contain small amounts of 3H and 14C.
iii.           Due to cosmic radiations.

Advantages of scintillation counting
§    The rapidity of fluorescence decay (10-9 s), which when compared to dead time in a Geiger-Muller tube (10-4 s), means much more count rates are possible.
§    Much higher counting efficiencies particularly for low energy β emitters; over 50% efficiency is routine in scintillation counting and efficiency can rise to over 90% for high energy emitters. This is partly due to the fact that the negatrons do not travel through air or pass through an end window of a Geiger-Muller tube but interact directly with the flour; energy loss before the event that is counted is therefore minimal.
§    The ability to accommodate samples of any type, including liquids, solids, suspensions and gels.
§    The ability to count separately different isotopes in the same sample, which means dual labeling experiments, can be carried out.
§    Scintillation counters are highly automated, hundreds of samples can be counted automatically and built in computer facilities carry out many forms of data analysis, such as efficiency correction, graph plotting, radioimmunoassay calculations, etc.


Disadvantages of scintillation counting
·                The cost per sample of scintillation counting is not insignificant; however, other factors including versatility, sensitivity, ease and accuracy outweigh this factor for most applications.
·                The greatest disadvantage of scintillation counting is quenching. This occurs when the energy transfer process. It can be any one of three kinds.
Ø   Optical quenching
Ø   Colour quenching
Ø   Chemical quenching

Optical quenching
This occurs if inappropriate or dirty scintillation vials are used. These will absorb some of the light being emitted, before it reaches the photomultiplier.


Colour quenching
This occurs if the sample is coloured and results in light emitted being absorbed within the scintillation cocktail before it leaves the sample vial. When colour quenching is known to be a major problem, it can be reduced, as outlined later.

Chemical quenching
It occurs when anything in the sample interferes with the transfer of energy from the solvent to the primary flour or from the secondary flour, is the most difficult form of quenching to accommodate. In a series of homogenous samples, chemical quenching may not vary greatly from sample to sample. In this case relative counting using sample counts per minute can be compared directly. However in the majority of biological experiments using radioisotopes, such homogeneity of samples is unlikely and is not sufficiently accurate to use relative counting. Instead an appropriate method of standardization must be used. This requires the determination of the counting efficiency of each sample and the conversion of counts per minute to absolute counts. It should be noted that quenching is not such a great problem in solid scintillation counting.

Chemiluminescence: This can also cause problems during liquid scintillation counting. It results from chemical reactions between components of the samples to be counted and the scintillation cocktail, and produces light emission unrelated to excitation of the solvent and flour system by radioactivity. These light emissions are generally low energy events and are rejected by the threshold setting of the photomultiplier in the same way as is photomultiplier noise.

Phospholuminescence : This results from components of the sample, including the vial itself, absorbing light and re-emitting it. Unlike chemiuminescence, which is a once only effect, phospholuminescence will occur on each exposure of a sample to light. Samples that are pigmented are most likely to phosphoresce. If this is a problem, samples should be adapted to dark prior to counting and the sample holder should be kept closed through the counting process.


AUTORADIOGRAPHY
          Ionizing radiation acts upon a photographic emulsion to produce a latent image much as does visible light. For an autoradiograph, a radiation source, (i.e. radioactivity) emanating from within the material to be imaged (the object) is required, along with a sensitive emulsion. Autoradiography is very sensitive and has been used in a wide variety of biological experiments.  These unusually involve a requirement to locate the distribution of radioactivity in biological specimens of different types. For instance, the sites of location of a radiolabelled drug throughout the body of an experimental animal. The techniques of autoradiography have become more important with recent development in molecular biology. In general, weak β-emitting isotopes (e.g. 3H, 14C and 35S) are most suitable for cell and tissue localization experiments.



Choice of emulsion and film
A variety of emulsion is available with different packing densities of the silver halide crystals. Care must be taken to choose an emulsion suitable for the purposes of the experiment, since the sensitivity of the emulsion will affect the resolution obtained.  X-ray film is generally suitable for macroscopic samples. Liquid emulsions are prepared by melting strips of emulsion by heating them to around 60°C. Then either the emulsion is poured onto the sample or the sample attached to a support is dipped into the emulsion. The emulsion is then allowed to set before being dried. Such a method is often referred to as a dipping film method and is preferred when very thin films are required.

Background
Accidental exposure to light, chemicals in the sample, natural background radioactivity (particularly 40K in glass) and even pressure applied during handling and storage of film will cause a background fog (i.e. latent image) on the developed film. This can be problematic, particularly in high resolution work and care must be taken at all times to minimize its effect. Background will always increase during exposure time, which should therefore always be kept to a minimum.

Time of exposure and film processing
The time of exposure depends upon the isotope, sample type, level of activity, film type and purpose of the experiment. The sample applies to the processing of the film in order to display the image. Generally the process must be adapted to a given purpose, and a great deal of trial and error is often involved in arriving at the most suitable procedures.

Direct autoradiography
In direct autoradiography, the X-ray film or emulsion is placed as close as possible to the sample and exposed at any convenient temperature. Quantitative images are produced until saturation is reached. The approach provides high resolution but limited sensitivity.

Intensifying screens
When 32P-labelled or γ-isotope-labelled samples, [e.g. (32P) DNA or 125I labelled protein fractions in gels] are to be located, the opposite problem to that presented by low energy isotopes prevails. These much more penetrating particles and rays cause little reaction with the film as they penetrate right through it, producing a poor image. The image can be greatly improved by placing, on the other side of the film from the sample, thick intensifying screen consisting of the solid phosphor.

Preflashing
The response of a photographic emulsion to radiation is not linear and usually involves a slow initial phase (lag) followed by a linear phase. Sensitivity of films may be increased by preflashing. This involves a millisecond light flash prior to the sample being brought into juxtaposition with the film and is often used where high sensitivity is required or if results are to be quantified.



Quantification
Autoradiography is usually used to locate rather than to quantify radioactivity. However, it is possible to obtain quantitative data directly from autoradiography by using a densitometer, which records the intensity of the image. This in turn is related to the amount of radioactivity in the original sample. There are many varieties of densitometers available and the choice made will depend on the purpose of the experiment.




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