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LABORATORY EXPERIMENT № 2



                        DETERMINATION OF  THE EFFECTIVE POROSITY


                        FACTOR  OF   ROCK  BY I.A.PREOBRAZHENSKY’S

                            METHOD (BY MEANS OF INSTALLATION FOR


                                            VACUUMING IV-3 (ВУ-3) )




                        2.1 The objective of the experiment is: to study the concept of
                  effective  porosity  of  rock  and  to  determine  the  effective  porosity
                  factor of  the rock sample by means of  the  method of saturation of

                  the  rock sample with kerosene by vacuuming.



                                                     2.2 Definitions


                        Effective porosity of rock is the volume of pores (voids) which
                  are  linked  between  themselves  and  with  outer  medium  (without
                                                                                                   3
                                                                                                          3
                  isolated pores). The effective porosity of rock is measured in m , cm .
                        Effective  porosity  factor  is  the  ratio  of the  volume  of

                  interconnected  pores V              to  the  bulk volume  of  the rock sample
                                                 int.  p.
                  V b.r.s. :
                                                         V
                                               m          int.  p.    .                                  (2.1)
                                                 ef.p.   V
                                                           b.r.s.

                        I.A.Preobrazhensky’s  method  is  most  commonly  used  for
                  determining the effective porosity factor (that is the method of the rock



                  sample  saturation  with  liquid,  usually  kerosene).  According  to  this
                  method the  volume  of  interconnected  pores  is  determined  as  the

                  volume of kerosene filling the pore space of the rock sample after its


                  saturation  in  vacuum  and  the  bulk  volume  of  the  rock  sample  is
                  determined by weighing the rock sample saturated with kerosene in air
                  and  in  kerosene.  Thus  for  determining  the  bulk  volume  of  the  rock

                  sample Archimede’s law is used (the bulk volume of the rock sample





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