Proton mobility in solids. Part 3.—Proton magnetic relaxation in boehmite

Abstract
Proton magnetic resonance and pulse magnetic spectroscopy measurements performed on boehmite in the temperature range from +350°C to –145°C permit two spin populations, Pn and Pw, to be differentiated. The Pw population belongs to the ordered domain of the oxygen-hydroxyl zig-zag chain whilst the Pn population represents either extrinsic lattice defects (below ∼50°C) or extrinsic and intrinsic defects occurring at a higher temperature. In both these defects the longitudinal relaxation rate is attributed to fast proton jumps between H2O+ units and free orbitals of adjacent oxygen atoms: vD= 1.6 × 1010 exp (–1800 cal/RT) sec–1. The transverse relaxation rate is due to the rotation of these H2O+ units (vR= 107 exp (–935 cal/RT) sec–1). At room temperature, the Pn population is represented in the n.m.r. absorption spectrum by a narrow band ( text-decoration:overlineΔH 2 < 0.2 gauss2) whilst the wide band ( text-decoration:overlineΔH 2≃ 16.5 gauss2) is due to the Pw spin collection. The relationship between these results and those obtained from previous conductivity and dielectric measurements is discussed.