Page 176 - Geochemical Remote Sensing of The Sub-Surface
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Light hydrocarbons for petroleum and gas prospecting                  15 3

                  l
              NmW                       2,3"  RAIN.  5 ~ RAIN.   W   4.8"  RAIN
                                                                      /
                                                               RAIN
                          1,4"  RAIN.
              2 ~  RAIN
                           N
                                          MI
                                                                      N
                                              |
                                                               N
                                                                     ,//<.
                                               J
                                                               N
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                               ,.  _, ..-..-N"     "         ',e
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                     ~ m m
             g  I~o   1 1'112  I 13  1 IAr 1 Is  I I~  1 1T  ~8  Ig12012rl  2zi  2312412s12~12r  128
           Fig. 5-10. Changes in flux of propane concentration (dashed lines) with barometric pressure (solid
           line) and rainfall (shaded bars) at two surface sample sites over an underground propane-storage
           reservoir; horizontal scale shows days of month.



           escape  occurs despite  the extensive  microbiological  activity that has developed over this
           cavem.
              As shown in Fig. 5-11, a propane profile collected over the top of the cavem requires
           a log scale to illustrate the enormous range  in gas leakage  flux.  An interesting secondary
           observation  taken  from  this  example  is  the  obvious  colour  changes  noted  on  the  soil
           cores.  These chemical  changes are related  to hydrocarbon seepage  and might be used as
           an additional  exploration tool to provide evidence  of where the  gas leakage has occurred
           around  any  type  of  storage  cavern.  The  soil  changes  from  red-brown  to  green-black
           directly over the top of the cavern, where the largest seepage anomalies occur.
              Thus  the  main  difficulty  with  atmospheric  sampling  is  created  by  meteorological
           changes  which  can  greatly displace  and  dilute  the  seepage  emissions.  In  addition,  it  is
           clear that the stress fields in the Earth can also influence this gas flux significantly.



           Earthquakes

              The fact that earthquakes may sometimes be preceded by geochemical anomalies was
           discovered  at about the  same  time  in Japan  (Okabe,  1956)  and  the  then  USSR  (Fursov,
           1968).  Earthquake  prediction  studies  in  Russia,  Japan  and  China  include  extensive
           geochemical  measurements.  Chinese  geochemical  data  are  reported  to  have  contributed,
           at  least  partly,  to  the  successful  prediction  of  several  strong  earthquakes  (Allen  et  al.,
           1975).  In  contrast,  the  Earthquake  Hazards  Reduction  Program  in  the  United  States
           emphasises mainly geophysical data.
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