Three sarnples of c a l c i~~~n oxide, designated as .A, B, ancl C, \\.ere preparecl from c a l c i~~m carbonate labelled with calci~~m-45. : \ \vas heated to constant weight a t 700°C.; B was hcated an additiollal three hours a t 1400 to l55OoC.; and C was heated six hours a t the same temperature. 'The samples \\.ere hydratetl in a supersaturated lime solution a t 21°C., the develop~llent of activity and the changes in collcentratiol~ of thc solution being deterlnined. l'he activity cnterillg the solution accourlted, according to theory, for the f~l l o \ \~i~l g percentages of the sanlples passing through the solutioll during the hydration: r \ , 27'5;; R , 57%; C, 94%. These results indicate that samplc C ("clead-burnt" lime) hydratcd by a "through-solutior~" mechanism, but that .\ and B cither hydrated partly according to some other mechanisrn, such as a vapor phase process ill the pore> of the particles of lirnc, or the c a l c i~~m ions failed to reach the bull; of thc hyclrating liq~lid bcfore precipitation as calci~lrn hyclroxicle.
INTRODUCTIOK