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Home > History and Archaeology > History > Smithsonian Meteorological Tables [Based on Guyot's Meteorological and Physical Tables] Volume 69: (English)
Smithsonian Meteorological Tables [Based on Guyot's Meteorological and Physical Tables] Volume 69: (English)

Smithsonian Meteorological Tables [Based on Guyot's Meteorological and Physical Tables] Volume 69: (English)

          
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About the Book

This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1918 edition. Excerpt: ...Table 72. Pressure of aqueous vapor over water. Metric measures. The pressures, computed by equation (1) above, are given for each tenth of a degree to 0.001 mm. from oo to509, and toooi mm. from 50o to loofg. They are given for each degree to 0.1 mm. from 1000 to 1890, and in millimeters from 1900 to 374. TABLES 73, 74. Table 73. Weight of cubic foot of saturated aqueous vapor--English measures. Table 74. Weight of a cubic meter of saturated aqueous vapor--Metric measures. For many years it has been customary to assume that the specific gravity of water vapor relative to dry air is a constant whose theoretical value computed from the accurately known densities of its constituent gases is 0.6221. Direct experimental determinations of the specific volume of dry saturated steam (as yet but few observations are available at moderate temperatures) show conclusively (1) that this theoretical specific gravity is true only for saturated vapor at very low temperatures or when the vapor is in a very attenuated state of partial saturation; (2) that at increasingly higher temperatures the specific gravity is increasingly greater than 0.6221. These assertions are in accord with the values of weight per cubic foot of water vapor tabulated by Marks & Davis l from the most recent determinations of the specific volume of water vapor. However, owing to the paucity of data, and its inaccuracy for the range of atmospheric temperatures and conditions, the values derived from densities given by Marks and Davis between io and 500 are probably too low and require revision. The basis on which this assertion is made is the generalization that the theoretical value 0.6221 is probably a minimum specific gravity towards which actual values asymptotically tend at...


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Product Details
  • ISBN-13: 9781236998347
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 48
  • Series Title: English
  • Weight: 104 gr
  • ISBN-10: 1236998340
  • Publisher Date: 13 Sep 2013
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Spine Width: 3 mm
  • Width: 189 mm

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Smithsonian Meteorological Tables [Based on Guyot's Meteorological and Physical Tables] Volume 69: (English)
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