 | 1803 - 922 pages
...would effectually prevent any vapour from arising under 212°: but it is caused by the vis inertice of the particles of air, and is similar to that which...The theory of evaporation being thus manifested from * This refers to experiments on the evaporation of water at »ne ; for which see the -Essay. experiments... | |
 | 1820 - 496 pages
...atmosphere, for that would prevent any vapour from rising under 212"; but, as Mr. Dalton observes, is caused by the vis inertia of the particles of air,...of water meets with in descending amongst pebbles. In ascertaining this point, at ordinary atmospheric temperatures, regard must be had to the force of... | |
 | 1820 - 450 pages
...that would prevent any vapour from arising under 212°; but, as Mr. Dalton observers caused by the DM inertia of the particles of air, and is similar to...of water meets with in descending amongst pebbles. In ascertaining this point at ordinary atmospheric temperatures, regard must be had to the force of... | |
 | John Frederic Daniell - 1823 - 528 pages
...prevent any vapour from rising under 212°; but, as Mr. Dalton observes, is caused by the vis inertias of the particles of air, and is similar to that which...of water meets with in descending amongst pebbles. In ascertaining this point at ordinary atmospheric temperatures, regard must be had to the force of... | |
 | Thomas Forster - 1823 - 490 pages
...would effectually prevent any vapour from arising under 212°; but it is caused by the vis inertice of the particles of. air, and is similar to that which a stream of water meets with in descending among pebbles. " The theory of evaporation being thus manifested from experiments in high temperatures,... | |
 | Friedrich Christian Accum - 1824 - 386 pages
...prevent any vapour from arising under 212° ; but, as Mr. Dalton observes, is caused by the vis inertice of the particles of air, and is similar to that which...of water meets with in descending amongst pebbles. In ascertaining this point at ordinary atmospheric temperatures, regard must be had to the force of... | |
 | Luke Howard - 1833 - 462 pages
...would effectually prevent any vapour from rising under 212°; but it is caused by the vis inertice of the particles of air, and is similar to that which...of water meets with in descending amongst pebbles. force of vapour actually existing in the atmosphere at the time. For instance, if water of 59° were... | |
 | Luke Howard - 1833 - 570 pages
...would effectually prevent any vapour from rising under 212°; but it is caused by the vis inertioe of the particles of air, and is similar to that which...of water meets with in descending amongst pebbles. force of vapour actually existing in the atmosphere at the time. For instance, if water of 59° were... | |
 | John Frederic Daniell - 1845 - 456 pages
...prevent any vapour from arising under 212°; but, as Dr. Dalton observes, is caused by the vis inertice of the particles of air, and is similar to that which...of water meets with in descending amongst pebbles. In ascertaining this point at ordinary atmospheric temperatures, regard must be had to the force of... | |
 | Leonard Blomefield - 1858 - 440 pages
...212° ; but it is by the vis ine^tie of the particles of the air. Dalton describes the obstruction as " similar to that which a stream of water meets with in descending amongst pebbles." t Climate of London, vol. ip 85. most favour evaporation are heat, dry air, and a diminished pressure... | |
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... of the particles of air, and is similar to that which a stream of water meets with in descending amongst pebbles. 
