 | British Association for the Advancement of Science. Meeting - Science - 1903 - 1176 pages
...of the atmosphere, and its condensation has been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the pressure of the remaining uncondcnsed gases, and as these are slightly soluble they dissolve to some extent in the fluid. The... | |
 | Smithsonian Institution - Chemistry - 1901 - 478 pages
...the atmosphere, and its. condensation has been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the pressure of the remaining uncondenscd gases, and as these are slightly soluble they dissolve to some extent in the fluid. The... | |
 | Smithsonian Institution. Board of Regents - Discoveries in science - 1903 - 1122 pages
...earth's surface. This resulting ocean is subjected to the pressure of the remaining uneondensed gases, and as these are slightly soluble they dissolve to...volume with the volume of the water as steam, we should lind about 1'voluhie of air in 60,000 volumes of steam. This would then be about the rough proportion... | |
 | Smithsonian Institution. Board of Regents - Discoveries in science - 1903 - 902 pages
...the atmosphere, and its condensation lias been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the pressure of the remaining uncondensed gases, and as these are slightly soluble they dissolve to some extent in the fluid. The gases in solution... | |
 | British Association for the Advancement of Science. Meeting - Science - 1903 - 1174 pages
...of the atmosphere, and its condensation has been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the pressure of the remaining uncondensed gases, and as these are slightly soluble they dissolve to some extent in the fluid. The gases in solution... | |
 | British Association for the Advancement of Science - Science - 1903 - 1174 pages
...of the atmosphere, and its condensation has been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the pressure of the remaining uncondensed gases, and as these are slightly soluble they dissolve to some extent in the fluid. The gases in solution... | |
 | George Downing Liveing, Sir James Dewar - Spectrum analysis - 1915 - 646 pages
...of the atmosphere, and its condensation has been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the...slightly soluble they dissolve to some extent in the liquid. The gases in solution can be taken out by distillation or by exhausting the water, and if we... | |
 | James Dewar - Chemistry - 1927 - 840 pages
...of the atmosphere, and its condensation has been brought about by the gradual cooling of the earth's surface. This resulting ocean is subjected to the pressure of the remaining uiicondensed gases, and as these are slightly soluble they dissolve to some extent in the fluid. The... | |
 | Smithsonian Institution. Board of Regents - Discoveries in science - 1903 - 960 pages
...resulting ocean is subjected to the pressure of the remaining uncondensed gases, and as these are clightly soluble they dissolve to some extent in the fluid....taken out by distillation or by exhausting the water, ami if we compare their volume with the volume of the water as steam, we should h'rul about 1 volume... | |
 | Smithsonian Institution. Board of Regents - 1903 - 892 pages
...earth's surface. This resulting ocean is subjected to the pressure of the remaining uncondensed gases, and as these are slightly soluble they dissolve to...some extent in the fluid. The gases in solution can l>e taken out by distillation or by exhausting the water, and if we compare their volume with the volume... | |
| |
This resulting ocean is subjected to the pressure of the remaining uncondensed gases, and as these are slightly soluble they dissolve to some extent in the fluid. The gases in solution can be taken out by distillation or by exhausting the water, and if... 
