The Dynamical Theory of the Formation of the Earth
The Dynamical Theory of the Formation of the Earth
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In our eReader you can find the full English version of the book. Read The Dynamical Theory of the Formation of the Earth Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Dynamical Theory of the Formation of the Earth
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The height to which the air will have to ascend before it be cold enough to form clouds is a variable quantity, depending on the number of degrees which the dew point is below the temperature of the air ; . . . . and the difference between the dew point and the temperature of the air is called the complement of the dew point."f * Princiides of Meteorology, Hutchinflon, pp. 17» 21, 27.
t Philosophy of Storms, Synopsis, Introduction, pp. viii. ix.
Y Digitized by Google 322 DYNAMICAL THEORY OF THE... Dr. Thomson informs us, that ** Dalton has demonstrated, that the elasticity of water at the hoiling point, under mean pressure, and that of our atmosphere at the same pressure, are equal ; that aqueous vapour possesses exactly the same repulsive force in the atmosphere which it assumes in a vacuum, the temperature being the same ; and that as its elasticity depends upon the increase of heat, so it is possible to ascertain the amount of vapour floating in the air, at any temperature, by mea- suring the elasticity of the aerial fluid He reasoned upon evaporation as we do on the inertia of matter, and by experimental research discovered in it a conformity with the laws of mechanics.
What to read after The Dynamical Theory of the Formation of the Earth?
You can find similar books in the "Read Also" column, or choose other free books by Archibald Tucker Ritchie to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The height to which the air will have to ascend before it be cold enough to form clouds is a variable quantity, depending on the number of degrees which the dew point is below the temperature of the air ; . . . . and the difference between the dew point and the temperature of the air is called the complement of the dew point."f * Princiides of Meteorology, Hutchinflon, pp. 17» 21, 27.
t Philosophy of Storms, Synopsis, Introduction, pp. viii. ix.
Y Digitized by Google 322 DYNAMICAL THEORY OF THE... Dr. Thomson informs us, that ** Dalton has demonstrated, that the elasticity of water at the hoiling point, under mean pressure, and that of our atmosphere at the same pressure, are equal ; that aqueous vapour possesses exactly the same repulsive force in the atmosphere which it assumes in a vacuum, the temperature being the same ; and that as its elasticity depends upon the increase of heat, so it is possible to ascertain the amount of vapour floating in the air, at any temperature, by mea- suring the elasticity of the aerial fluid He reasoned upon evaporation as we do on the inertia of matter, and by experimental research discovered in it a conformity with the laws of mechanics.
What to read after The Dynamical Theory of the Formation of the Earth?
You can find similar books in the "Read Also" column, or choose other free books by Archibald Tucker Ritchie to read onlineMoreLess
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