[Pg513]

which, taken between the limits s = S′ and s = S, becomes

E″ = a log.Sb(S − S′).(12.)
S′

But by (11.) we have

E′ = abS′,
E = abS;
∵ E′ − E = b(S − S′);
∵ E″ = a log. S − E′ + E;
S′
E = E″ + E′ = a log. S + E.(13.)
S′

Or,

E = a (1 + log. S) − bS.(14.)
S′

Hence it appears that the mechanical effect of a cubic foot of water evaporated under the pressure P may be increased by the quantity a log. S/S′, if it be first evaporated under the greater pressure P′, and subsequently expanded to the lesser pressure P.