[Pg513]
which, taken between the limits s = S′ and s = S, becomes
| E″ = a log. | S | − b(S − S′).(12.) |
| S′ |
But by (11.) we have
| E′ = a − bS′, |
| E = a − bS; |
| ∵ 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.