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Radionuclides  in Nature                    121



                                             5.11.  Exercises

                5.1.  Cosmic-ray irradiation of the atmosphere yields 0.036  1~  atoms cm -2 s -l.  If this l~   is rapidly carried
               down into sea water, which is assumed to have a volume of 1.4  x  10 Is m 3, what will the equilibrium radioactivity
               of l~   in  1 m 3 sea water be? The  earth's surface area is 510  x  106 km 2.
                5.2.  In Greenland ice the  l~   radioactivity has been measured to be 0.0184 dpm m -3.  How old is this ice if it
               was  formed out of water in equilibrium with cosmic-ray  l~   (see previous question)?
                5.3.  The  CO 2 in  the  atmosphere  is  in  exchange  with  carbon  in  living  organisms,  humus,  dissolved  organic
               compounds, and carbonate in the sea water, the latter being the main reservoir (88 %) of all exchangeable carbon.
               The amount of such exchangeable carbon is estimated to be 7.9 gcm -2 of the earth. When cosmic-ray produced
               14C is mixed  into this exchangeable carbon,  what will the  specific activity become?
                5.4.  On  the  label  of a  bottle  of cognac  bought  in  1976  it is  stated  that  the  cognac  is  over  20  years  old.  An
               analysis showed  a  tritium content of 80 TU.  Discuss the trustworthiness  of the  statement.
                5.5. 0.11  cm 3 helium gas at NTP was isolated from  100 g of uranium mineral containing 5 ppm uranium.  How
               old is the mineral  ?
                5.6.  A  mineral was  found  to contain 39. I  g  K and  87.2  x  10 -6 liter Ar at NTP.  How  old  is the  mineral?
                5.7.  A uranium mineral was found to contain the lead isotopes 2~   :~b,  and 2~   in the ratio  1:1087:388,
               as determined with  a  mass spectrometer.  Estimate the age of the  mineral.
                5.8.  The  heat flow from the earth's crust is 0.060 W  m -2.  The  mean thickness of the crust is  17 km and the
               earth's radius is 6371  km. The average concentration of uranium, thorium, and potassium in granite is estimated
              to be 4 ppm (by weight)  18 ppm,  and 3.6 %,  reSl~ectively. Assuming that 7 % by volume of the crust is made up
               of granite (feldspar +  quartz, density 2.6 g cm-~), what will the heat flow at the earth's surface be from each of
              these elements?  Assume/~-heat as  1/3 Ensx;  for a-decay assume E,~  =  Q~.  Each 4~  decay by  the  EC-branch
               emits one  1.46 MeV  3'. Discuss the  results.
                5.9.  A  1 GW 9  nuclear power  station uses  annually  about  30 t uranium  enriched  to  3 %  235U. (a)  How  much
               natural  uranium  has  been  produced  to  keep  it  running?  Assume  waste  stream  from  isotope  separation plant to
              contain 0.3 % ~35U. Co) How much low grade ore (assume 0.06 % uranium) must be mined, if the uranium recovery
              efficiency in the process  is 70%?
                5.10. The assumed uranium resources in Japan are 4 kt, in Argentina 12 kt and in France 48 kt U30 s. How many
               1 GW e reactor years can these uranium amounts sustain in each country at the uranium consumption rate  (a) of
              the previous exercise?


                                             5.12.  Literature

              E. K. HYDE, Natural Radioactivity of the Heavy Elements: A Comprehensive Review, Univ. of California Radiation
              Laboratory, Report  UCRL-10612.
              W.  F.  Lmnv, Radiocarbon  Dating,  University of Chicago Press,  1956.
              C.  E.  IUNGE, Air Chemistry and Radioactivity,  Academic  Press,  1963.
              H.  CILM(;, S.  L.  MILLER, and G. J.  WASSERBURG (Eds.), Isotopic and Cosmic Chemistry, North-Holland,  1963.
              E.  I.  HAMILTON and  L.  H.  AHRENS, Applied Geochronology,  Academic Press,  1965.
              B.  KEISCH, Dating  works of art through their natural radioactivity: improvements and applications,  Science  160
              (1968)  413.
              D.  YORK and R.  M.  FARQUHAR, The Earth's Age and Geochronology,  Pergamon Press,  1972.
              P.  K.  KUROD^, Fossil nuclear reactor and plutonium-244 in the early history of the solar system.  In IAEA,  The
              Oklo-phenomenon,  Vienna,  1976.
              Ionizing Radiation:  Sources  and Biological Effects,  United  Nations  1982.
              P.  S.  ZURER, Archeological Chemistry,  Chem. & Eng.  News Febr. 21,  1983, p.21.
              P.  J.  D.  LLOYD, p.  772 in T.  Lo,  M.  BAIRD and C.  HANSON, (Eds.),  Handbook of Solvent Extraction,  J.  Wiley
              &  Sons  1983.
              G.  FAURE, Principles  oflsotope  Geology,  2nd  Ed.  ]  Wiley &  Sons  1986.
              M.  EISENnUD, Environmental  Radioactivity,  3rd  Ed.,  Academic  Press  1987.
              M.  A.  GEYH and  H.  SCHLEICHER,  Absolute Age Determination,  Springer-Verlag  1990.
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