Page 21 - Professorial Lecture - Prof Oyedele
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6.  STUDIES ON THE RADIOACTIVITY IN DIFFERENT CITIES AND
              TOWNS IN NAMIBIA.

           6.1  MEASUREMENT OF THE CONCENTRATIONS OF RADIONUCLIDES IN SOILS

           As I said earlier, if the concentration of radionuclides in the soil of a particular
           area is high, it could lead to a higher level of ionizing radiation in the area.
           In  fact,  it  is  well  known  that  the  radionuclides  in  the  soil  are  the  main
           contributors to natural radioactivity in a given area (IAEA, 1987). Areas with
           high level of radiation are called high background radiation area (Ghiassi-
           nejad et al., 2002; Ramli et al., 2005). High background radiation area could
           be  a  threat  and it is  not  desirable  to  live in  such  areas.  It is  therefore  of
           interest to check whether or not our towns and cities - where we live - are
           high background radiation areas. In fact, as I indicated earlier, a number of
           citizens in different towns - especially those close to Mines – have asked (my
           research group) if their towns have normal or “safe” background radiation.

           A  way  to  determine  the  level  of  radiation  or  assess  the  background
           radiation  in  a  given  town  is  to  determine  the  concentrations  of
           radionuclides in the soil of that town (Sahin and Cavas, 2008; Mujahid and
           Hussain, 2010; Kapdan et al., 2012). More specifically, we take a relatively
           small amount of soil – which we call a soil sample – in a place in the town
           and  we  process  the  sample  and  subsequently  measure  the  amount  of
           radiation emitted by each of the three radionuclides Uranium-238, Thorium-
           232 and Potassium-40 (in the sample) using a radiation detector such as
           HPGe (Knoll, 2000; L’Annunziata, 2004; Tsoulfanidis, 2011). We then calculate
           the  concentrations  of  the  radionuclides  from  the  amount  of  radiation
           emitted. These concentrations will be substituted into some well-established
           formulas to obtain the level of radiation and the hazards of radiation at the
           point where the sample was collected (Oyedele, 2006a; Cam et al., 2013;
           Oyedele and Shimboyo, 2013).

           The above procedure is repeated for about 50 to 100 samples in a town
           and the average concentrations (of  238 U,  232 Th and  K), average radiation
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           level and average hazard indices are subsequently calculated for the town.
           From  these  average  values,  we  can  know  if  the  town  is  having  a  high
           background radiation (and therefore hazardous) or if it is normal (Oyedele,
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