 | Arnold Guyot - Meteorology - 1858 - 658 pages
...the Greenwich Meteorological Observations for 1842, pages xlvi. and li. ; the first containing the weight of a cubic foot of dry air, under a barometric...air, on which the tables are based, is assumed to be 563 grains Troy, being a mean value, in round numbers, between the determinations of Shuckburgh, which... | |
 | Science - 1862 - 786 pages
...the Greenwich Meteorological Observations for 1842, pages xlvi. and li. ; the first containing the weight of a cubic foot of dry air, under a barometric...air, on which the tables are based, is assumed to be 563 grains Troy, being a mean value, in round numbers, between the determinations of Shuckburgh, which... | |
 | Karl Theodor Anger - 1862 - 718 pages
...different authorities. Table XIII., page 264, gives the weight of a cubic foot of dry air and of saturated air under a barometric pressure of 30 inches, at temperatures between 0° and 90° F. The weight of a cubic foot of dry air is assumed to be 563 grains troy at a temperature • of 82° F.,... | |
 | Elias Loomis - Meteorology - 1868 - 328 pages
...different authorities. Table XIII., page 264, gives the weight of a cubic foot of dry air and of saturated, air under a barometric pressure of 30 inches, at temperatures between 0° and 90° F. The weight of a cubic foot of dry air is assumed to be 563 grains troy at a temperature • of 82° F.,... | |
 | Elias Loomis - Meteorology - 1872 - 324 pages
...different authorities. Table XIII., page 264, gives the weight of a cubic foot of dry air and of saturated air under a barometric pressure of 30 inches, at temperatures between 0° and 80° F. The weight of a cubic foot of dry air is assumed to be 563 grains troy at a temperature of... | |
 | Henry F. Blanford - India - 1877 - 308 pages
...the pressure of the air acting on it, is no longer an exact measure of its weight. The weight of one cubic foot of dry air, under a barometric pressure of 30 inches and at 32° Fahrenheit, is 565 grains. From these data it follows that, if the atmosphere were throughout... | |
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X 4.56 = 4«r>.49, the weight of vapor required. TABLE XVII. FOR COMPARING THE WEIGHT OF A CUBIC FOOT OF DRY AND OF SATURATED AIR. THIS table is composed of two tables found in the Greenwich Meteorological Observations for 1842, pages xlvi. and li. ;... 