Page 181 - Gas Adsorption Equilibria
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3. Gravimetry                                                    167


          5.       PROS AND CONS OF GRAVIMETRY

             This section is devoted to the advantages and disadvantages of gravimetric
          measurement of gas adsorption equilibria. It reflects experiences we made in
          our experimental work in this  field during the last 15  years using both two
          beam and magnetic suspension balances.

          5.1      Advantages

             1. Accuracy
                All microbalances which are commercially available today, cp.  Tab.
                3.1, [3.7-3.9]  normally exhibit  high reproducibility,  sensitivity, and
                accuracy (up  to      of measurements.  Hence they  allow one to
                determine  adsorbed gas  masses on  porous solids  much  more
                accurately than manometric measurements. The gain in accuracy often
                is about one order of magnitude; at very low pressures it may be two
                orders of magnitude or even more.

             2. Amount of sorbent material
                For highly  sensitive microbalances (Thermo  Cahn, Hiden, Mettler-
                Toledo, Rubotherm, Setaram, TA Instruments, VTI) only tiny amounts
                of sorbent materials are needed to measure gas adsorption equilibria.
                This is  advantageous for  investigations in  newly  developed  sorbent
                materials where  often  only  small  amounts are  available. However,
                results may  be misleading  as the sorbent  sample  used does not
                represent a  “statistically averaged”  sample of a technical sorbent and
                thus may exhibit considerable statistical deviations.

             3. Approach to equilibrium
                Microbalances with alphanumerical  display and  electronic data
                recording systems  allow one  to  observe the  approach to  equilibrium
                for gas  adsorption  processes in porous  sorbent samples.  Typical
                relaxation times can be one or several seconds, minutes, hours, and –
                sometimes – even days, cp. helium adsorption data Sect. 2 of Chap. 1.
                Hence gravimetric  measurements do  allow one to  check whether an
                adsorption system actually has reached its equilibrium state, i. e. these
                measurements deliver in  principle also  information concerning the
                kinetics of  the adsorption  process, represented  for example  by
                (phenomenological)  diffusion coefficients, cp.  Sect.  2.3  and Sect. 4.4
                and [3.27, 3.48).
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