Scientific American Supplement, No. 363, December 16, 1882 by Various
page 41 of 145 (28%)
page 41 of 145 (28%)
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227 deg. 0.395
232 deg. 0.355 236 deg. 0.310 240 deg. 0.267 245 deg. 0.226 250 deg. 0.183 255 deg. 0.140 261 deg. 0.097 266 deg. 0.060 271 deg. 0.023 290 deg. 0.000 [Footnote 1: _Vide_ Burgh, "Modern Marine Engineering," page 176 _et seq._ M. Couste, _Annales des Mines_ V 69. _Recherches sur Vincrustation des Chaudieres a vapour_. Mr. Hugh Lee Pattison, of Newcastle-on-Tyne, at the meeting of the Institute of Mechanical Engineers of Great Britain, in August, 1880, remarked on this subject that "The solubility of sulphate of lime in water diminishes as the temperature rises. At ordinary temperatures pure water dissolves about 150 grains of sulphate of lime per gallon; but at a temperature of 250 deg. Fahr., at which the pressure of steam is equal to about 2 atmospheres, only about 40 grains per gallon are held in solution. At a pressure of 3 atmospheres, and temperature of 302 deg. Fahr., it is practically insoluble. The point of maximum solubility is about 95 deg. Fahr. The presence of magnesium chloride, or of calcium chloride, in water, diminishes its power of dissolving sulphate of lime, while the presence of sodium chloride increases that power. As an instance of the latter fact, we find a boiler works much cleaner which is fed alternately with fresh water and with brackish water pumped from the Tyne when the tide is high than one which is fed with fresh water constantly."] |
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