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Practice of Kinetics (Comprehensive Chemical Kinetics, Volume 1)

Practice of Kinetics (Comprehensive Chemical Kinetics, Volume 1)

Practice of Kinetics (Comprehensive Chemical Kinetics, Volume 1)

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100 EXPERIMENTAL METHODS FOR SLOW REACTIONSing gas that was present. Moseley and R ~bb~~' have made use <strong>of</strong> the pressurechange occurring in a gas resulting from the adiabatic temperature rise in the initialstages <strong>of</strong> a photochemical reaction The technique was used to determine therate constant for methyl radical combination3 31. The small pressure changes weremeasured by means <strong>of</strong> a very sensitive diaphragm manometer as a change in capacitybetween the diaphragm and a small brass probe A (Fig. 69).An important method (already mentioned, p. 11) for determining the extent<strong>of</strong> a heterogeneous contribution to a homogeneous reaction is that <strong>of</strong> differential~alorimetry~~. Two fine-gauge wire thermocouples enclosed in thin Pyrex or silicacapillaries are mounted at the centre and close to the wall <strong>of</strong> the RV (Fig. 70).L YFig. 70. Differential calorimetry. From ref. 47a.The difference in readings <strong>of</strong> these thermocouples gives a measure <strong>of</strong> the temperaturerise <strong>of</strong> the gas at the centre <strong>of</strong> the RV relative to the walls. For an entirelyhomogeneous reaction, the initial temperature rise for a cylindrical RV is given bywhere qg is the heat liberated per second and h is the coefficient <strong>of</strong> thermal conductivity<strong>of</strong> the gas. For an entirely heterogeneous reaction, the initial temperaturerise ATw is given byAT, = q,r In (R/r)/2nh(R+r)(R')where qw is the heat liberated at the walls per second, R is the radius <strong>of</strong> the RVand r is the radius <strong>of</strong> the capillary. For both heterogeneous and homogeneouscontributions we have2r In (R/r)AT = qg+qw * 14n.hR+rIf the rates <strong>of</strong> the homogeneous and heterogeneous reactions are We and W,respectively, the overall rate W = W.+ W,.

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