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Light hydrocarbons for petroleum and gas prospecting                 149

           hydrocarbons  into  the  near-surface  environment  above  the  water  table  must  involve
           transport  through  both  water-filled  and  air-filled  pores.  Sampling  these  pore  gases  is
           obviously one  of the  most  fundamental  concepts.  However,  gases  can  be  bound  in  the
           sediment matrix.  This latter possibility leads to the  development of some disaggregation
           and desorption extraction techniques.
              Discussion of sampling  techniques  must involve both "flee"  and  "bound"  gases.  To
           facilitate  this  discussion  the  collection,  measurement  and  analysis  of  light  (C1-C4)
           hydrocarbons will be broken into two main categories  each with two subcategories:  (1)
           free  gas,  which  can  be  vapour  or  dissolved  gas;  and  (2)  bound  gas,  which  can  be
           adsorbed gas or chemi-adsorbed gas.



           Free gas

              Gases  in  the  free  pore  space  can  be  found  either  in  the  vapour  state  or  dissolved  in
           water.  Extensive  research  at  Gulf  Research  and  Development  Company  has
           demonstrated  that  the  "free"  and  "dissolved"  gas  seeps  yield comparable  compositional
           results,  both  to  one  another  and  to  their  associated  reservoirs  when  they  are  properly
           collected  and  analysed  (Teplitz  and  Rodgers,  1935;  Jones,  1979;  Janezic,  1979;
           Mousseau  and  Williams,  1979;  Weismann,  1980;  Drozd  et  al.,  1981;  Williams  et  al.,
           1981;  Jones  and  Drozd,  1983;  Richers,  1984;  Price  and  Heatherington,  1984;  Matthews
           et  al.,  1984;  Jones  et  al.,  1984).  This  documentation  even  extends  to  numerous
           observations over artificial underground gas generation and storage reservoirs (Jones and
           Thune,  1982; Jones,  1983; Pirkle and Drozd,  1984).
              Sampling of vapour can be extended to any depth above the water table by analysing
           the  exhaust  air  from an  air-drilled  well.  Complications  occur because  of dilution  effects
           by  the  air  injected  for drilling  and  by  the  additional  fact  that  the  drill  bit  disaggregates
           and liberates rock or matrix gas in the process of drilling the hole.
              Dissolved  gases  must be  extracted  from the  aqueous  system before  analysis.  This  is
           usually  accomplished  by  a  simple  gas-water  partition  into  a  vapour  phase  followed  by
           standard  headspace  measurement  techniques  (McAuliffe,  1966).  Alternatively  a  so-
           called  "stripper"  continuously partitions  the  dissolved  gases  into  a  carrier  gas  which  is
           then  sent to  a gas  chromatograph  for analysis  (Mousseau  and  Williams,  1979;  Aldridge
           and  Jones,  1987).  These  separations  are  aided  by  the  very  low  solubility  of  the  light
           hydrocarbon gases.
              Standard  mud  gas  logging  is  one  variant  of  dissolved  gas  analysis  conducted  on
           deeper  drill  holes.  A  gas  trap  is  deployed  in  the  return  mud  system  for  extracting  the
           dissolved  and  free  gases.  Compositional  information  obtained  from mud  logging gas  is
           useful  for predicting  the  composition of a potential  reservoir (Pixler,  1969).  These  same
           ratios  have  been  found  to  be  indicative  of oil  versus  gas  potential  from  surface  seeps
           observed  from  4  m  (12  feet)  deep  soil-gas  measurements  or  from  analysis  of  gases
           dissolved in the shallow groundwater (Jones and Drozd,  1983).
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