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P. 145

-  THE  NEUTRON  LOG  -

                                     Sem
                       }=-—-  23cm                        Table  10.3  Thermal  neutron  capture  cross-sections  of  some
                                                          elements,  (note  the  values  for  H  and  C1  as  well  as  B  and  Gd).
                                      water
                                                          Element    Capture  cross-section,   cross-section
                                                                     barns
                                                                                           atomic  weight
                                         =16              oO  Cc     0.0034                0.00028
                  N=132
                                                                                           0.33
                                                          H
                                                                     0.33
                                                                     0.00027
                                                                                           0.000017
                limestane  0%                             Na         0.53                  0.023
                                                          Mg
                                                                     0.063
                                                                                           0.0027
                                                                                           0.0085
                                                         Al
                                                         Si          .23                   0.0057
                                                                     16
       Figure  10.3  Schematic  trajectories  of  a  neutron  in  a  Lime-
                                                          cl         33.2                  0.94
       stone  with  no  porosity  and  pure  water.  The  slowing  down
                                                          K          2.10                  0.084
       length  in  the  limestone  is  far  greater  than  in  water  (modified
       from  Ellis,  1987),                               Ca         0.43                  0.011
                                                          B          759                   70.3
       Table  10.2  Neutron  slowing-down  parameters  (*number  of
                                                          Gd         49,000                312
       collisions  involved  during  change  from  4.2  Mev  to  |  eV).
       (from  Ellis  1987).                               Cd  (shield
                                                         material)    2,450                21.9
              Moderator          *no.  of  collisions

                                                          ~  cross-section/atomic  weight  gives  a  guide  to  the  effect  of
              H                  14.5                     a  thermal  absorber  relative  to  the  volume  of  formation  it
              Cc                 91.3                     occupies.
              0                  121                      -  Cadmium  is  separated  on  the  list  as  it  is  rarely  encountered
              Ca                 305                      naturally  but  is  used  in  tool  construction  as  a  thermal]
              H,O                15.8                     absorber.
                                                          from  Dunlap  and  Coates,  1988.
              Limestone  20%  b   29.7
              Limestone  0%      132
                                                          cross-section  of  the  absorbing  nuclei  of  the  formation,

                                                          which  is  a  measure  of  how  effective  it  is  at  capturing
       penetration  capabilities  but  after  a  few  microseconds  and
                                                          neutrons.  Gadolinium  and  boron  have  large  thermal
       successive  collisions  (100  or  so),  the  original  fast  neu-
                                                          neutron  cross-sections  but  are  quite  rare:  chlorine,
       trons  have  slowed  down  through  epithermic  to  thermic
                                                          common  in  saline  formation  fluids,  has  a  moderate  cross-
       levels  with  about  0.25  eV  of  energy  and  a  velocity  of
                                                          section  (Table  10.3).
       around  0.22  cm/sec  (Figure  (0.2).  To  reduce  a  neutron
                                                            As  far  as  logging  is  concerned,  the  dominant  effect  on
       from  2  MeV  (2200  cm/sec)  to  0.025  eV  (0.22  cm/sec)
                                                          neutrons  during  the  collision  and  scattering  phase,  is  the
       requires  18  (elastic)  collisions  with  hydrogen  nuclei
                                                          mass  of  the  (formation)  nuclei,  hydrogen  dominating:  the
       but  257  (non-elastic)  collisions  with  silicon  and  368  with
                                                          dominant  effect  during  the  absorption  phase  is  the  capture
       calcium  nuclei  (Serra,  1979).  Expressed  in  another  way,
                                                          cross-section  of  the  thermal]  neutron  absorbers,  the  effect
       elastic  collision  with  hydrogen  can  take  all  a  neutron’s
                                                          of  hydrogen  being  much  less  marked  (Table  10.3).
       energy  but  in  non-elastic  collisions  with  heavier  elements,
       the  energy  reduction  is  typically  around  10%  to  25%:  the
                                                          10.3  Tools
       effect  of  hydrogen  is  seen  as  dominant  (Table  10-2).
         At  the  lower  energy,  thermic  levels,  the  neutron  is   The  neutron  tool  today  generally  consists  of  a  fast  neutron
       thought  of  as  diffusing,  rather  than  having  a  velocity.  For   source  and  two  detectors  (Figure  10.4).  The  source
       example,  in  a  vacuum,  a  thermal  neutron  will  diffuse   bombards  the  formation  with  neutrons  and  the  detectors
       randomly  for  13  minutes,  but  in  earth  materials  the  time   measure  their  loss  of  energy  as  they  pass  through  it.
       varies:  5  psec  in  rock  salt,  450  «sec  in  a  limestone  with-   Toot  sources  are  mostly  chemical,  such  as  plutonium-
       out  porosity  and  900  wsec  in  a  quartzite  (Serra,  1979).   beryllium  (PuBe)  or  americum-beryllium  (AmBe),  which
       The  period  of  diffusion  comes  to  an  end  as  the  neutrons   produce  fast  neutrons  with  a  peak  energy  level  around
       undergo  absorption  interactions.  That  is,  they  are  cap-   4  Mey.  These  are  the  most  common.  Infrequently,  high
       tured  by  other  nuclei  which  then  change  energy  state  and,   energy  neutrons  at  up  to  14  MeV  are  produced  using
       mostly,  become  unstable.  For  example,  some  nuclei,  on   accelerometers,  in  which  the  neutrons  are  created  by
       capturing  a  neutron,  spontaneously  de-excite  and  emit   bombarding  a  target  with  charged  particles.
       gamma  rays  of  capture,  the  so-called  n,y  capture  radiation   Historically,  the  first  neutron  tools  consisted  of  a
       (an  effect  used  in  pulsed  neutron  logging)  (Figure  10.2).   source  and  just  a  single  detector  but  these  were  quite
       The  rapidity  of  neutron  absorption  depends  on  the  capture   affected  by  borehole  environment  and  most  tools  now
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