Principles of Chemical Geology a Review of the Application of the Equilibrium T
Principles of Chemical Geology a Review of the Application of the Equilibrium T
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In our eReader you can find the full English version of the book. Read Principles of Chemical Geology a Review of the Application of the Equilibrium T 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 Principles of Chemical Geology a Review of the Application of the Equilibrium T
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To quickly assess the difficulty of the text, read a short excerpt:
D. K. Akad. D. Wiss. , p. 570, 1900.
VAPOUR PRESSURE 85 form of anhydrite as is got by heating gypsum in dry air. At a still higher temperature namely, 525 C. This soluble anhydrite passes into the insoluble form of natural anhydrite. Calcium sulphate in solu- tion in water, therefore, cannot be deposited as anhy- drite unless the vapour pressure of the gypsum exceeds that of the solution in contact with it. To secure this result, either the vapour pressure of the gypsum must be increased by ra...ising the temperature or the vapour pressure of the solution must be reduced, since at all temperatures below 107 C. The hydrate has a lower vapour pressure than pure water. In the natural formation of anhydrite, however, we are not dealing with a simple solution, but with a complex solution of soluble salts. We have to consider, therefore, the influence of co-solutes.
The presence of any substance in solution which lowers the vapour tension of water will lower the inversion temperature of gypsum.
What to read after Principles of Chemical Geology a Review of the Application of the Equilibrium T?
You can find similar books in the "Read Also" column, or choose other free books by James Vincent Elsden to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
D. K. Akad. D. Wiss. , p. 570, 1900.
VAPOUR PRESSURE 85 form of anhydrite as is got by heating gypsum in dry air. At a still higher temperature namely, 525 C. This soluble anhydrite passes into the insoluble form of natural anhydrite. Calcium sulphate in solu- tion in water, therefore, cannot be deposited as anhy- drite unless the vapour pressure of the gypsum exceeds that of the solution in contact with it. To secure this result, either the vapour pressure of the gypsum must be increased by ra...ising the temperature or the vapour pressure of the solution must be reduced, since at all temperatures below 107 C. The hydrate has a lower vapour pressure than pure water. In the natural formation of anhydrite, however, we are not dealing with a simple solution, but with a complex solution of soluble salts. We have to consider, therefore, the influence of co-solutes.
The presence of any substance in solution which lowers the vapour tension of water will lower the inversion temperature of gypsum.
What to read after Principles of Chemical Geology a Review of the Application of the Equilibrium T?
You can find similar books in the "Read Also" column, or choose other free books by James Vincent Elsden to read onlineMoreLess
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