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Chapter I
Fundamental Radiation Concepts

  1. The Radioactive Atom

  2. All matter is composed of elements and all elements are composed of atoms. The atom contains a nucleus consisting of protons and neutrons with electrons revolving in circular and elliptical orbits about the nucleus. Electrons carry a negative charge, protons carry positive charge, and the neutrons have no electrical charge. An atom normally has one electron in orbit for each proton in the nucleus, leaving the atom electrically neutral.

                                                               A
        The atomic structure of an element is denoted as        X
                                                               Z
    
    where:
    A
    is the Mass Number, defined as the sum of the number of protons and neutrons in the nucleus. Thus, A minus Z gives the number of neutrons. An element may have different numbers of neutrons and still be chemically the same.
    X
    is the chemical symbol of the element:
    Z
    is the Atomic Number, defined as the number of protons in the nucleus. This determines the chemical identity of the element:

    Each individual arrangement of protons and neutrons is referred to as a Nuclide. Nuclides which have the same number of protons are called Isotopes. Shown below are examples of isotopes of Hydrogen:

    Hydrogen Isotopes

    Many nuclides, but not all, are unstable or "radioactive". In the above examples, only tritium is radioactive. Radioactivity is defined as the spontaneous disintegration of unstable nuclei with the resulting emission of radiation that results in the formation of new nuclei. Stability of the nucleus is related to its ratio of neutrons to protons. For low atomic numbered elements, approximately equal numbers of neutrons and protons in the nucleus are necessary for stability. For elements of higher atomic number, the ratio rises to approximately 1.6 to 1. As a nuclide departs from this stable ratio, changes in the nucleus occur which tend to bring the product to a more stable arrangement. This approach to stability is accomplished by one or more of 5 "radioactive decay modes".

  3. Radioactive Decay Modes
    1. Beta Decay
    2. When the neutron to proton ratio is too high, a neutron "transforms"into a proton and electron with the electron being ejected from the nucleus. The ejected electron is called a "beta particle". Beta particles are not emitted with a single energy but are emitted with a spectrum of energies up to some maximum value. This is due to a division of the total energy of each disintegration between the beta particle and a neutrino. The Neutrino is a massless, chargeless particle that carries off varying amounts of the released energy. The neutrino has a negligibly small mass and no charge. It therefore travels great distances, losing little energy in nearby materials and causes no biological damage.

      The energy of the ejected beta particle is characteristic of each nuclide and is one criterion used for identification purposes. In general, the average energy per particle is about 1/3 of the maximum energy.

      The generalized atomic equation for beta decay is as follows:

      	   A          A
                  X   --->   Y  + beta-  + v    X = Original (parent) atom
                 Z        Z+1                     Y = New (daughter) atom
                                                 beta- = Beta particle (electron)
                                                  v = Neutrino
      Examples of  Beta decay:
      
              3      3
               H ->   He + 0.0186 MeV beta --max      MeV = 1 million electron volts
              1      2                            beta- max = maximum beta particle energy 	
      
      
               14      14
                 C ->    N + 0.156 MeV beta-max
                6       7

    3. Positron Decay
    4. When the neutron to proton ratio is too low, the nucleus emits a beta particle with a positive charge (positron) resulting from the transformation of a proton into a neutron.

      The positron behaves exactly as an electron except that when the positron comes in contact with a free electron, the two particles combine and are annihilated. This gives rise to two gamma rays whose energies correspond to the rest mass equivalence of the particles (0.511 MeV/gamma). See page 13 for a description of annihilation radiation.

      The generalized atomic equation for positron decay is as follows:

              A      A
               X ->   Y  + beta+  +  v    beta+ = positron  (positive electron)
              Z    Z-1
      Example of Positron decay:
      
               19       19
                 Ne ->    F  +  2.22 MeV beta- + v
               10        9

    5. Electron Capture
    6. In this decay mode, one of the orbital electrons is captured by the nucleus and combines with a proton to form a neutron. Electron capture competes with positron decay when there is a low neutron to proton ratio. If the atom is unable to meet the energy requirements of positron decay, then decay occurs by electron capture. Whenever an atom decays by electron capture, X-rays (page 10) are emitted that are characteristic of the newly formed nuclide. No particles are emitted during electron capture decay.

      The generalized atomic equation for electron capture is:

      
              A            A
               X  +  e ->   Y  +  X-rays +  v           e = electron
              Z          Z-1	 
      
      Example of electron capture decay:
      
             54               54
               Mn  +  e ->      Cr  +  0.835 MeV X-rays +  v
             25               24

    7. Alpha Decay
    8. Alpha decay occurs for those nuclides that have an atomic number greater than 82. Such heavy nuclides have no stable configuration of neutrons and protons and as a result emit an alpha particle consisting of 2 protons and 2 neutrons. Generally, a series of alpha (as well as beta) decays are required until a lighter, more stable element is reached. Unlike beta particles, alpha particles are emitted with a discrete energy.

      The generalized atomic equation for alpha decay is:

      
              A         A-4                           4
                X  ->      Y  +   alpha              alpha =  He  (Helium nucleus)
              Z         Z-2                           2
      
      Example of alpha decay:
      
            210          206
               Po  ->       Pb  +  5.3 MeV alpha
             84           82

    9. Nuclear Transition - Gamma Ray Emission
    10. Gamma rays (page 8) are emitted when the emission of a particle leaves the product nucleus in a partially excited or "metastable" state. The gamma rays carry away the excess energy of the partially excited nucleus after a decay event. Such gamma rays are of discrete energy, are characteristic of the particular nuclide involved and can be used for identification purposes.

      Nuclear transition can occur after beta decay, positron decay, electron capture and alpha decay.

      	
      Example of radionuclides that undergo nuclear transition are shown below:
      
              60       60
                Co ->    Ni + 0.318 MeV beta- + 1.17 MeVgamma; + 1.33 MeVgamma
              27       28 
                                                 gamma = gamma ray
      
               22         22
                  Na ->    Ne + 0.546 MeV beta+ + 1.27 MeVgamma
               11         10
      
               125      125
                    I ->  Te + 0.035 MeV gamma (6.67%) + X-rays
                53       52
      
               226        222
                  Ra ->      Rn + 4.78 MeV alpha (93.4%) + 4.59 alpha (5.7%) +  0.186 MeVgamma  +  X-rays
                88         86
      
      The Chart of The Nuclides (Appendix I) list all known nuclides and is a useful reference for radioactive decay and energy data.

  4. The Radioactive Decay Equation
  5. A radioactive nuclide disintegrates or decays spontaneously at a rate depending on the number of original atoms present and upon its decay constant, lambda (gamma). This constant gamma is defined as the instantaneous fraction of atoms decaying per unit time. Each radioactive nuclide has its own characteristic decay constant.

    The instantaneous time rate of change of the number of atoms, N, for a radionuclide is given by:

               dN = - gamma N
               dt  
    
    If we started with No radioactive atoms at some time t=0, the number of atoms at some other time Nt, can be obtained by integrating:

    Equations

    The e-t term indicates that the radioactive atoms decay exponentially. This equation, is called the decay equation.

                    Nt = N 0e-gamma t
    
    If we were to substitute into the decay equation the time, T, it takes for the reduction of a quantity of radioactive atoms to half of the original, we get:
               NT=1No
                  2
    
               1No = Noe-gamma1/2
               2  
    
               1 = e-gammat 1/2
               2
    
               ln 1/2 = -gammaT1/2 Therefore (ln 1/2=ln1-ln2; ln1=0)
    
               Therefore -ln2 = -gammaT1/2
    
               T1/2=ln2 > (ln2=0.693)
    
               Therefore gamma = 0.693
                               T1/2   
    

    Thus, the decay constant, gamma, can be calculated for any radioactive nuclide from its half-life.

  6. Radioactivity Units
  7. The instantaneous number of atoms, N, remaining at a particular instant in time is given by :

    A = gamma N

    A is the activity, defined as the instantaneous number of atoms decaying per unit time. The activity determines the quantity of radioactive material in a sample. The special unit for activity is called the Curie (Ci).

    	1 Curie = 3.7 X 1010 disintegrations per second (DPS)
                    = 3.7 X 1010 becquerels
         		        or
    	1 Curie = 2.22 X 1012 disintegrations per minute (DPM)	
    

    The International System (SI) of units has defined the Becquerel (Bq) as the unit of activity, equal to 1 disintegration per second. The Becquerel is already in use in some parts of the world and will eventually replace the Curie.

    Because the Curie is a very large quantity, fractions of the Curie are often used:

    	1 millicurie = (mCi) = 2.22 X 109 dpm = 10-3 Curies
    	1 microcurie = (µCi) = 2.22 X 106 dpm = 10-6 Curies
    	1 nanocurie  = (nCi) = 2.22 X 103 dpm = 10-9 Curies
     	1 picocurie  = (pCi) = 2.22 dpm = 10-12 Curies

    Since radioactive material is measured in units of activity, the decay equation now takes the form:

    A = Aoe-gammat

    Where:  A = Activity after some time t
            Ao = Original activity of the sample
            gamma = The radioactivity decay constant equal to 0.693
                                                            T1/2
            T1/2 = Half-life of isotope
            t = Decay time
    
    Note: The decay time and half-life must be expressed in the same units of time.

  8. Interactions of Radiations with Matter
  9. Radiation interacting with matter can be either scattered or absorbed. The mechanisms of the absorption of radiation is of interest because:

    The transfer of energy from emitted radiations to matter occurs in two major ways: Ionization and Excitation.

    Ionization:
    The process resulting in the removal of an electron from an atom, leaving the atom with a net positive charge.

    Excitation:
    Addition of energy to an atomic system, transferring it from the ground state to an excited state.

    Radiation can be classified into two groups:

    1. Interaction of Charged Particles
    2. All atoms are normally electrically neutral. When a charged particle strikes an orbital electron, it ejects it from the atom resulting in the formation of an ion pair. Since the removal of the electron from the atom decreases the total number of negative charges by one, it leaves the atom with a net positive charge. The ion pair consists of:

      1. The positively charged atom.
      2. The negatively charged electron.

      Such particles capable of creating ion pairs in this manner are called ionizing radiation.

      The term used to compare and relate the ionizing powers of different types of charged particles is called the "specific ionization" Specific ionization is defined as the number of ion pairs per unit path length formed by ionizing radiation in a medium:

           Specific Ionization = # of ion pairs formed
                                     cm of path
      The specific ionization is dependent on the velocity of the charged particle (and therefore its energy), and the density of the absorbing material (the number of atoms available for ionization).

      1. Alpha Particles
      2. An alpha particle is a helium nucleus stripped of its orbital electrons. It is emitted from a radioactive atom with a velocity of about 1/20 that of the speed of light and with energies ranging from 4 to 9 MeV. Alpha particles cause ionizations in matter when they are deflected by the positive charge of a nucleus and pull the orbital electrons (attracted by the alpha's positive charge) along with them. Alpha particles also cause excitation along their path by pulling inner orbital electrons to outer orbits. No ion pair is formed, but energy is lost from the alpha particle and added to the atom. The added energy is then given off by the atom as fluorescent radiation or low energy X-Rays when the electrons drop back down to the inner orbital vacancies.

        Because of its relatively large mass (2 neutrons and 2 protons), high electrical charge (+2) and low velocity, the specific ionization of an alpha particle is very high. That is, it creates many ion pairs in a very short path length. Because of this, it loses all of its energy in a very short distance. The range in air is only several centimeters even for the most energetic alpha particles.

        Since the alpha particle has a very limited range in matter, it presents no external radiation hazard to man. Many alpha particles cannot penetrate the protective layer of skin. However, once inside the body, surrounded by living tissue, damage will be to the local area in which the alpha emitter is deposited. Thus, alpha emitters are an internal hazard and intake to the body must be prevented. (See Chapter IV, "Radiation Protection Techniques").

      3. Beta Particles
      4. Beta particles are emitted from the nucleus of a radioactive atom with a wide range of energies up to some maximum value. When a beta is emitted that is below the maximum value, the neutrino carries away the rest of the energy.

        Beta particles, like alpha particles, lose their energy by ionization and excitation, but because of their small mass (1/7300 of an alpha) and lower charge (1/2 of that of an alpha) the interactions take place at less frequent intervals. Therefore, the beta particles do not produce as many ion pairs per centimeter of path as alpha particles, and thus, have a greater range in matter. The beta particle's range in matter depends on the energy and the composition of the material. (See Appendix III, "Penetration Ability of Beta Radiation").

        Beta particles can interact with a nucleus of an element and give rise to X-rays by a method called Bremsstrahlung. Bremsstrahlung (German for "Breaking Radiation") occurs when high speed beta particles approaches the nucleus of an atom. The electrical interaction between the negative beta particle and the positively charged nucleus causes the beta particle to be deflected from its original path or stopped all together. Their stoppage or deflection results in a change in velocity of the beta particle with the emission of X- rays of various energies The likelihood of Bremsstrahlung production increases with increasing atomic number of the absorber. For this reason, beta shields are made from low atomic numbered material, like aluminum or plastics.

        Beta particles require an energy of greater than 70 keV to penetrate the protective layer of the skin, and thus, are somewhat of an external hazard. The beta can also constitute an internal hazard. A beta particle has a greater range in tissue compared to an alpha particle due to its low specific ionization. The beta particle gives up less energy per unit volume of tissue and, therefore, is not as effective in causing damage as an alpha particle.

    3. Interaction of X-Rays and Gamma-Rays
    4. From a practical radiation protection point of view, X-rays and gamma rays are identical, differing only in their place of origin. Gamma rays are emitted from excited nuclei with a discrete energy. X-rays are emitted when the extra-nuclear atomic structure undergoes a transition; i.e., an outer shell electron replaces a missing lower shell electron and an X-ray is produced. The energy of the X-ray is approximately equal to the difference in the electron energy levels.

      Since X and gamma rays are chargeless, they do not interact by electrostatic forces as in the case of charged particles, which cause ionization of matter directly along their path of travel. However, X and gamma rays do have sufficient energy to release high energy secondary charged particles (electrons) from matter through one of three basic interactions:

      The high speed electrons resulting from these interactions then cause ionization of the medium.

      1. The Photoelectric Effect
      2. The Photoelectric Effect is the interaction of X or -gamma-ray photons** as well as other photons (such as light), whereby all of the energy of the photon is transferred to an inner shell electron (usually the K shell), ejecting it from the atom and leaving the atom with an inner shell vacancy. This shell vacancy creates an excitation energy which corresponds to the Binding Energy (BE) of the ejected photoelectron.

        shell

        The Kinetic Energy (KE) of the photoelectron is equal to the energy of the X or gamma-ray photo minus the BE of the electron ejected.

        If the X or gamma-ray photon does not have sufficient energy to knock the inner shell electron loose, the reaction will not occur.

        The resultant atom is now in an excited state and will decay to the ground state by emission of X-rays and fluorescent radiation with the total energy equal to the BE of the photoelectron. The energies of the secondary radiations are usually much lower than the primary X or gamma-ray energies.

        Application of the Photoelectric Effect

        Gamma rays emitted from excited nuclei, and X-rays emitted from excited atoms, have discrete energy characteristics of the specific nuclides and elements, respectively. Thus, the energy of these gamma or X photons can be used as "finger prints" to identify unknown nuclides and elements.

        ** A photon, as described by the Quantum Theory, is a "particle" or "quantum" that contains a discrete quantity of electromagnetic energy which travels at the speed of light, or 3 X 108 meters per second.

      3. The Compton Effect
      4. Photons with energies much greater than the BE of the electrons in an atom may interact through essentially elastic scattering interactions in which the total KE of the system is conserved. In this interaction, the electron appears to the photon as a free electron.

        compton

        The primary gamma loses part of its energy to the Compton electron which gets scattered at an angle from the original direction of the incident gamma, while the compton scattered gamma (gamma') is scattered as an angle. In this process, the scattered photon and Compton electron share the energy of the incident gamma.

        The KE carried off by the Compton electron may be deposited locally (i.e., absorbed immediately by the surroundings). However, the energy carried off by the Compton scattered photon is not deposited locally. Therefore, this scattered photon can significantly contribute to the dose outside a shielding apparatus.

        Application of the Compton Effect

        Due to its characteristic peaks, the Compton Effect aids in the identification of unknown nuclides. However, in a detecting system, the Compton scattered electron can mask lower energy photons interacting by the photoelectric effect making interpretation of results difficult.

      5. Pair Production
      6. High energy gamma photons transfer their energy primarily by pair production. A high energy X or gamma-ray passing close to a nucleus suddenly disappears and an electron and a positron appear in its place. This interaction must take place in the neighborhood of a nucleus to conserve momentum.

        Pair production

        Since both particles are created from energy supplied by the incident photon, the process is energetically possible only if Egamma or EX is greater than 1.02 MeV.

        When the positron slows down (i.e., loses its KE), it will annihilate itself by combining with an electron. This produces two photons with an energy of 0.51 MeV each. This "annihilation radiation" represents the energy equivalent of the rest mass of two electrons which is converted to pure energy according to the principles of Einstein's theories, in particular, E = mc2; where

        E = energy of two 0.51 MeV photons
        m = the rest mass of two electrons (1/1840 amu)
        c = the velocity of light (3 X 108 m/sec)

        App. Of Production

        Applications of Pair Production

        Again, due to characteristic peaks observed for various known nuclides, Pair Production is an aid is an aid in the identification of unknowns.

  10. Radiation Dose Units
  11. Radiations are measured in four basic units - the gray, the rad, the rem and the sievert:

    The gray (Gy) is the SI unit of absorbed dose. One gray is equal to an absorbed dose of 1 Joule/kilogram (100 rads).

    The rad (radiation absorbed dose) is a measure of energy deposition in any medium by all types of radiation. The rad is equal to 100 ergs/gram.

    The rem (radiation equivalent man) is a unit of dose equivalent used for radiation safety purposes. The rem is defined as the dose (in rads) multiplied by appropriate Quality Factor (QF). The Quality Factor is a term used to derive dose equivalent from absorbed dose and takes into account the different abilities of radiation types to cause damage in a biological system. Below is a table listing Quality Factors for various types of radiations:

    The Sievert is the SI unit of any of the quantities expressed as dose equivalent. The dose equivalent in rems is equal to the absorbed dose in grays multiplied by the quality factor.

    Quality Factor
    Absorbed dose equal to a unit Quality dose

                                                   Quality      dose
                 Radiation                          Factor     equivalent *
    
                 X, gamma or beta                           1            1
                 Neutrons of unknown energies        10           0.1
                 Alpha particles                     20           0.05
                 High-energy protons                 10           0.1   
    

    Thus, the rem allows us to add doses of different radiation types to obtain total effective dose. * Absorbed dose in rad equal to 1 rem or the absorbed dose in gray equal to 1 sievert.

    Example: What is an individual's dose equivalent from 10 mrad of gamma rays, 5 mrads of beta- particles and 10 mrads of neutrons? (m = milli = 1/1000)

                Dose Equivalent         = mrads X QF = mrems
    
                Gamma dose equivalent      =  10   x 1       =  10
                Beta dose equivalent       =   5   x 1       =   5
                Neutron dose equiv.        =  10   x 10      = 100
                                                    Total      115 mrems

    The SI unit for dose equivalent is the Sievert (Sv) and is equal to 1 Joule/kg. 1 Sievert = 100 rem.


Problem Set 1

Multiple choice questions may have more than one correct response. Refer to Appendix IV for reference data.

  1. The structural difference between various nuclides of an element are due to different numbers of:

    1. electrons

    2. protons

    3. neutrinos

    4. neutrons

  2. Beta decay results in:

    1. decrease in atomic number and mass number of nucleus

    2. decrease in atomic number

    3. increase in atomic number

    4. increase in atomic number and mass number

    5. increase in atomic number and decrease in mass number

  3. One millicurie equals:

    1. 3.7 x 107 dps

    2. 3.7 x 1010 dps

    3. 2.22 x 109 dpm

    4. 2.22 x 106 dpm

    5. none of the above

  4. The decay constant, gamma, is equal to:

    1. A/N

    2. 0.693/T1/2

    3. 0.693/t

    4. e-NT

  5. Gamma rays interact directly with matter by:

    1. ionization and excitation

    2. compton scattering

    3. pair production

    4. photoelectric effect

  6. A charged particle interacts with matter by:

    1. compton scattering

    2. photoelectric effect

    3. excitation and ionization

    4. pair production

  7. The activity of a radioactive sample is measured by:

    1. Roentgens.

    2. Curies.

    3. Rems.

    4. Rads.

  8. The rem is equal to:

    1. Rads x Quality Factor

    2. Rads x X-Rads

    3. Rads ÷ Quality Factor

    4. Rads - Quality Factor

  9. An exposure to 1 mrad of gamma, 10 mrad of beta- particles, and 5 mrad of fast neutron radiations would give an individual a dose equivalent of:

    1. 16 mrem

    2. 16 µ Ci

    3. 61 mrem

    4. 61 mrads

  10. List the names and give specific examples for the types of radioactive decay processes in which particles are emitted:

              Name of Process                        Example
    
                  a)__________________________     _________________________
    
                  b)__________________________     _________________________
    
                  c)__________________________     _________________________
    

  11. Now, do the same for two types of decay which do not emit particles:
                  a)__________________________     _________________________
    
                  b)__________________________     _________________________
    

  12. A particular radioisotope sample with a half-life of 30 minutes is determined to have an activity of 10,000 dpm at noon.

    a) What is the value of its decay constant, gamma? Show units ____________
    
    b) How many radioactive atoms must have been present in the sample at noon? ____________
    
    c) How many dpm will it exhibit at 1:30 PM?   _____________
    

  13. At 9:00 AM Tuesday, you assay an unknown radioactive sample and get 15,000 dpm. The next day at 9:00 AM you assay the sample again and find it has decayed to 3,885 dpm. What is the half-life of the isotope? What is the isotope?

  14. Assume that you have converted an ancient piece of wood to benzene for Carbon-14 dating. You obtained 3 grams of benzene. The disintegration rate of this sample you found to be 18 dpm. Your modern carbon sample has a disintegration rate of 9 dpm per gram of benzene. Calculate the age of the wood sample.

  15. A user requires 2 mCi of Cu-64 for his experiments. If the delivery time is three days, what activity must the Vendor ship in order for the user to receive the correct activity?



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