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Chapter 2


          VOLUMETRY / MANOMETRY



          Abstract The physical  principles and  experimental  techniques of  pure  gas- and  multi-
                 component gas adsorption measurements by the volumetric (or manometric) method
                 are outlined.  Examples are  given.  Thermovolumetric and combined  volumetric–
                 calorimetric measurements are presented. Pros and cons of the method are discussed.
                 References. List of Symbols.



          1.       INTRODUCTION

             Volumetry or, preferably “Manometry”, cp. Sect. 2.1, is the oldest method
          to investigate sorption of gases in solids. Early experiments had already been
          performed by C. W. Scheele (1777), Chappuis (1881), W. Ostwald (1905) and
          J. Langmuir  (1912),  [1.1]. Some  of  these  experiments  were designed  to
          determine the volume of geometrically complicated objects like cauliflower or
          sea-urchins. A special instrument for this purpose was designed by R. W. Pohl
          about 1940 and was called a “volumimeter”  [2.1]. It served as a prototype of
         many of today’s volumetric instruments.

             The physics of volumetric gas adsorption  experiments is  simple:  a given
         amount  of sorptive gas is expanded  into a  vessel  which includes  a  sorbent
          sample and which initially has been evacuated. Upon expansion the sorptive
         gas is  partly  adsorbed on the  (external and  internal) surface  of the  sorbent
         material,  partly remaining  as gas  phase  around the  sorbent.  By  a mass
         balance, the  amount of  gas being  adsorbed can be  calculated if  the  void
         volume of the sorbent, i.  e. the  volume  which  can not be penetrated by the
          sorptive gas molecules is known – at least approximately.

             The adsorbed mass per unit mass of sorbent is a characteristic quantity for
          a porous  solid.  Assuming a  characteristic area per single molecule adsorbed
         on the surface of a solid – for   at 77 K this area is   for Kr at 87 K
          it is         [2.2, p.  173] – the surface area of the solid can be calculated
         and from  this the  porous  solid  can be  “characterized”.  Actually,  many
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