Dynamics of silicate exchange in highly alkaline potassium silicate solutions
The problem of measuring the kinetics of Si exchange between aqueous silicate species by 29Si NMR has been revisited, using highly alkaline KOH solutions (2.8 mol SiIV per kg solvent, [SiIV]/K2O = 0.43) at 60-90°C to minimize the number of silicate species present. Longitudinal 29Si relaxation times T1 and apparent rate constants estimated from line-shape analysis (LSA) varied markedly with the degree of purity of the KOH used, but rate constants k obtained by selective inversion-recovery (SIR) using the CIFIT data-fitting program were independent of the source of KOH and were smaller than those obtained from LSA by at least an order of magnitude. Although only four kinetically significant silicate anions (monomer M, dimer D, linear trimer L, and cyclic trimer C) were present, overlap of the D and L resonances prevented complete analysis of the SIR data. True rate constants could therefore be obtained only for the M-D exchange (for formation of D, k1 (90°C) = 0.13 ± 0.01 kg mol -1 s-1, Δ H1dagger = 67.4 kJ mol-1, Δ S1dagger = -78 J K-1 mol-1; for dissociation of D, k-1 (90°C) = 1.4 ± 0.1 s-1, Δ H-1dagger = 64.7 kJ mol-1, and Δ S1dagger = -66 J K-1 mol-1). Models that included L as the precursor of C (MDLC mechanism) showed, within the limitations imposed by D-L band overlap, that the reactivities of M, D, L, and C in Si-O-Si link formation or dissociation were all roughly comparable. Good fits of the experimental data, however, and equally reliable rate constants for the M-D exchange, could be obtained with models that ignored the presence of L entirely (MDC mechanism). The simple MDC model also provides consistent apparent rate constants kC and k-C for the overall formation of C from M + D and the reverse process, respectively, by SIR of either M or C ( Δ HCdagger = 76.5 kJ mol-1, Δ SCdagger = -57 J K-1 mol-1; Δ H-Cdagger = 88.6 kJ mol-1, and Δ S-Cdagger = -7 J K-1 mol-1).Key words: kinetics, silicates, 29Si NMR.