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LABORATORY EXPERIMENT № 1

                         DETERMINATION OF THE ABSOLUTE  POROSITY
                                               FACTOR  OF  ROCKS


                        1.1  The  objective  of  the  experiment  is:  to  determine  the
                  imaginary  (apparent)  density  of  the  rock  and  the  absolute  porosity

                  factor  of  the rock sample.

                                                     1.2 Definitions


                        Porosity of rock is a measure of  storage capacity of  a reservoir
                  (pore  volume  of  the  rock).  It    defines    the    ability    of    the  rock  to
                  contain liquids and gases. There are two types  of  porosity: absolute

                  or total  and effective porosity. Quantitatively porosity is characterized
                  by porosity factor. In general porosity  factor  is  the  ratio of  the pore

                  volume  to  the  bulk  volume  of  the  rock.

                        The absolute porosity  factor m          ab.p.  is the ratio of  the  volume of
                  all  pores  available  in  the  rock  sample  V            all p.  to the  bulk  volume
                  of  the rock sample V       b.r.s.  :

                                                       V all  p.
                                               m            .                                         (1.1)
                                                 ab.p.
                                                       V
                                                         b.r.s.
                        Porosity factor is determined in fractions or per cents.
                        Taking into account that

                                            V all  p.      V    V gr. ,                               (1.2)
                                                       b.r.s s
                                                           .
                  we’ll get:
                                           V all  p.    V   V gr.       V gr.
                                 m                  b.r.s.        1         ,                          (1.3)
                                   ab.p.
                                           V            V               V
                                            b.r.s.        b.r.s.          b.r.s.
                  where  V  is the volume of grains which form the rock.
                             gr.
                                   Taking into account  that  the  weight  of  the  rock  sample  is


                  equal to the weight of grains forming it the equation (1.3) can be given
                  in the following form:
                                                           
                                               m       1   r.s   ,                                      (1.4)
                                                 ab.p.
                                                            gr.
                  where   is the imaginary (apparent) density of  the rock sample, kg /
                             r.s.
                    3                                                                     3
                  m ;    gr.    is the density of grains forming the rock, kg / m .


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