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280                 Radiochemistry atut Nuclear Chemistry

               of the cyclone,  since the HTO  concentration  in the normal atmosphere is different  from that
               of  surface  ocean  water  due  to  isotopic  effects.
                Radioactive  tracers  like T20,  24Na+,  82Br-  (/~-y tt h  1.471  d)  and 51Cr-EDTA  (EC-y tv2
               27.704  d),  are used  in hydrology  to  determine  the volume  of natural  water  reserves  (even
               underground)  and  to  map  the  movement  of  ground  and  surface  water  as  well  as  effluent
               pathways,  Figure  9.17.  Also  the  consumption  of  water  and  water  flow  in  industries  are
               readily  determined,  and  leaking  dams  and  pipes  checked  by  radiotracers.
                In order to avoid hazardous pollution  it is important to discharge communal and industrial
               waste  (silts,  liquids,  gases)  so  that  the  wastes  are  properly  dispersed.  The  mapping  of
               different dispersal  sites is conveniently  and commonly carried out by injecting  a radioactive
               tracer  at  a  testing  spot,  and  then  following  its  distribution  at various  depths,  heights,  and
               directions.  In  such  a  test  it  was  found  that  sludge  emptied  into  the  River  Thames  at  one
               point  traveled  upstream,  which  led  to  a  repositioning  of  the  sludge  pipe  exit.  The  simple
               technique  of identifying  hidden  pipe  leaks is illustrated  in Figure  9.17  left.  This  technique
               is  used  not  only  for  liquids,  but  also  for  checking  the  seal  of  underground  electric  cable
               hoses  in  which  case  gas  tracers  like  85Kr  (/T'y  t~  10.72  y)  or  133Xe  (B-3~ ttA  5.24  d)  are
               used.
                Westermark and  co-workers have developed  a unique  method  of revealing  environmental
               history  of natural  rivers  during  the last  100  - 200  years.  It is based  on  the  freshwater pearl
               mussel Margaritana margaritifera living  in these fiver.  The mussel adds  a new  outer  layer
               to  its  shell  each  year,  incorporating  into  it  trace  metals  (and  also  to  some  extent  organics)
               dissolved  in  the water.  The shell  is cut and  sectioned  into  small pieces,  which  are analyzed
               by  cz-track  autoradiography,  INAA  and/~-PIXE.  The  latter  is  a  "microprobe"-PIXE,  i.e.
               the  proton  beam  is  focused  by  lenses  to  a  resolution  of  a  few  microns.  To  get  sufficient
               information  the  shell  sample  usually  covers  3  -  15  years.  With  these  techniques
               concentrations  of some  30 elements have been  determined  retrospectively  for  >  100  years
               in  a  number  of  Swedish  rivers.  Several  unexplained  trends  have  been  observed,  e.g.
               decreases  in  Ag,  Au,  Fe  and  Co.  This  is  believed  to  be  related  to  increasing  air
               concentrations  of  SO 2.  The  observation  of  an  increase  in  Br  beginning  in  the  1940's  is
               believed  to  be  due  to  Br-additions  to  gasoline  fuel.  The  technique  has  great  potentials  for
               increasing  our  knowledge  on  environmental  changes  of  trace  elements  in  nature.  It  could
               also  be used as a  long  term biochemical  control  system at environmentally  strategic places.


                                              9.8.  Exercises

                9.1. The blood volume of a patient is to be determined by means of 32p.  For this purpose 15.0 ml of blood is
               withdrawn from the patient and mixed with a very small volume of Na2H32po4 of high specific activity. In  1 h
               the erythrocytes (red blood cells) take up all the 32p; 1 ml is found to have an activity of 216 000 cpm in the
               detector system used. Exactly 5.00 ml of this tagged sample is reinjected into the patient, and 30 min later a new
               sample is withdrawn; 10 ml of this gives 2300 cpm. Calculate the blood volume.
                9.2. A mixture of amino acids is to be assayed  for cysteine. A 1.0 ml sample (density 1 g ml "z) is withdrawn,
               and 2.61 nag of 35S labeled cysteine of specific activity 0.862/~Ci nag "l is added. From this mixture pure cysteine
               is isolated by liquid-partition chromatography; 30.6 nag is isolated and measured to give 169 000 cpm in 27 %
               detection efficiency. What is the percentage of cysteine in the original mixture?
                9.3. In order to determine the lead content of a color pigment, 8.9871 g was dissolved in cone.  HNO 3, and 5.00
               ml 21~  solution added. After excess acid had been removed through evaporation, excess 1 M NaCI was added,
               the solution heated and filtered. ARer cooling and crystallization, the PbCI 2 was washed and recrystallized, 0.3276
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