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See also:GRAVIMETRIC See also:DENSITY OF PRODUCTS OF See also:EXPLOSION in. of See also:water at this temperature weighs 62.35 lb, and therefore I lb of water bulks 1728+62.35=27.73 cub. in . Thus if a See also:charge of P lb of See also:powder is placed in a chamber of See also:volume C cub. in., the (6) G.D . = 27.73P/C, G.V.=C/27•73 P . 30 30 28- ZB 28 26 Sometimes the See also:factor 27.68 is employed, corresponding to a See also:density of water of about 62.4 lb per cub. ft., and a temperature 12° C., or 54° F . With metric See also:units, measuring P' in kg., and C in litres, the G.D . =P/C, G.V . =C/P, no factor being required . From the Table I., or by See also:quadrature of the See also:curve in fig . 9, the See also:work E in See also:foot-tons realized by the expansion of I lb of the powder from one See also:gravimetric volume to another is inferred; for if the See also:average pressure is p tons per sq. in., while the gravimetric volume changes from v-80v to v±ZAv, a See also:change of volume of 27.73 AV cub. in., the, work done is 27.73 p w See also:inch-tons, or (7) DE=2.31 pOv foot-tons; and the See also:differences AE being calculated from the observed values of p, a summation, as in the ballistic tables, would give E in a See also:tabular See also:form, and conversely from a table of E in terms of v, we can infer the value of p . On See also:drawing off a little of the See also:gas from the explosion See also:vessel it was found that a gramme of See also:cordite-gas at o° C. and See also:standard atmospheric pressure occupied 700 CCs., while the same gas compressed into 5 ccs. at the temperature of explosion had a pressure of 16 tons per sq. in., or 16X2240÷14•7 =2440 atmospheres, of 14.7 lb per sq. in.; one ton per sq. in. being in See also:round See also:numbers 150 atmospheres . The See also:absolute centigrade temperature T is thence inferred from the gas See also:equation (8) R = pv/T = 001273, which, with p=2440, v=5, p0-i, v0=700, makes T=4758, a temperature of 4485° C. or 8105 ° F . |
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