Thermal stability of organic monolayers chemically grafted to minerals

The thermal degradation of monolayers of alkylsilicon hydrides (RSiH(3)), alkylphosphonic acids (RP(O)(OH)(2)), and alkyldimethylchlorosilanes (R(CH(3))(2)SiCl) supported on silica, alumina, titania, zirconia, and calcium hydroxyapatite particles was investigated using thermal gravimetric analysis (TGA). The common feature in the TGA was a dramatic weight loss between approximately 200 and approximately 600 degrees C (N(2) atmosphere), which was not present for bare minerals, and, thus, was assigned to the degradation of the surface grafted organic species. The onset of weight loss and the temperature of maximal weight loss rate (T(MAX)) showed no dependence on the mineral and were determined by the nature of the chemical group directly attached to the surface. The T(MAX) values were approximately 400-450 degrees C (monolayers of RSiH(3) and RP(O)(OH)(2)) and approximately 250 degrees C (monolayers of RSi(CH(3))(2)Cl). The activation energies (E(A)) of the degradation processes were determined using TGA at multiple heating rates. Surprisingly, the substrate material did not show a significant effect on E(A). For example, all the monolayers of octadecyl groups (R=C(18)H(37)) supported on silica, alumina, titania, and zirconia showed closed E(A) values approximately 265+/-15 kJ/mol. The weight loss, IR, MS, and chemical analysis data suggested that monolayer degradation occurred through pyrolysis of the hydrocarbon moieties (R groups) via cleavage of the CC and SiC (monolayers of silanes) or CC and PC bonds (monolayers of phosphonic acids). The inorganic portion of the molecule remained attached to the surface of the mineral (presumably as silicates or phosphates).