LECTURES ON GEOCHEMICAL !N1 ERPRETATION OF ...

- 11 -TABLE 1. Equations expressing the temperature dependence of various equilibriumconstants and other coefficients that are described in the text.T is temperature in kelvins, and t is temperature in ·C. The respectiveconstants for equations (a) through (k) are given in Table 2. The dataused in the derivation of these equations are shown in Table 3.2 - 1• a + bT ... eT + dT + e log T (a)k2 3a + bT + eT + dT + e log T Cb)-1:a a ... bT ... eT .. d log T (c)2 - 1== a ... bT ... eT + dT + e log T (d)2 - 1a + bT + eT + dT + e log T (e)2 3 4 5 - 1 - 2== a + bt + et + dt + et + ft + gt + ht + i log t ( g)- log K c2 3 - 1== a ... bT + eT + dT + eT Ch)A2 3 4 - 1a + bY ... eT + dT .. eT + fT + g log T ( 1)B2 3 4 -1.. a .. bT + eT + dT + eT + fT ( j )2 3 - 1 2== a + bT + eT + dT + eT + fT - (k)- 1log PC0 2 (Total)= 0.0053 - 621.4 T(m)