Thermal stability of organic monolayers chemically grafted to minerals

Abstract

The thermal degradation of monolayers of alkylsilicon hydrides (RSiH 3), alkylphosphonic acids (RP(O)(OH) 2), and alkyldimethylchlorosilanes (R(CH 3) 2SiCl) 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 ∼200 and ∼600 °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 ∼ 400 – 450 °C (monolayers of RSiH 3 and RP(O)(OH) 2) and ∼250 °C (monolayers of RSi(CH 3) 2Cl). 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 18H 37) supported on silica, alumina, titania, and zirconia showed closed E A values ∼ 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 C C and Si C (monolayers of silanes) or C C and P C bonds (monolayers of phosphonic acids). The inorganic portion of the molecule remained attached to the surface of the mineral (presumably as silicates or phosphates).