The increase in specific surface of kaolinite (K) and pyrophyllite (P) indu
ced by dry grinding in an oscillator), mill. proceeded during storage in wa
ter vapour. The average particle thickness, delta. changed from 42 nm (K) a
nd 66 nm (P) in the original materials to 12 nm (Kf and 20 nm (P) after wat
er sorption (20 days at relative humidity RH = 1.01 at room temperature and
pressure) and to similar values of 13 nm (K) and 16 nm (P) after grinding
for 10 min tin agreement with some published data). The action of water mol
ecules on ground clays (at the conditions indicated) resulted in a further
decrease in a. In pyrophyllite, prolonged grinding (30 min) and prolonged a
ction of water molecules (36 days) caused a particle collapse. After pre-st
oring at RH = 0.5 the successive decrease in delta at RH = 1.0 was smaller.