A Preliminary Study of the Waters of the Jemez Plateau New Mexico
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In our eReader you can find the full English version of the book. Read A Preliminary Study of the Waters of the Jemez Plateau New Mexico 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 A Preliminary Study of the Waters of the Jemez Plateau New Mexico
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It is evident that the waters of the sulphate-car- Ixmate class have primarily come up through the Car- boniferous strata, and, since sodium carbonate and cal- cium sulphate are readily soluble in water, have dissolved a large quantity of these alkalies and carried them along in solution. Further on in its course this alka- line water has probably come in contact with some form of granite, such as rhyolite, and dissolved some of the silica. This silica in solution will then act on a car- bonate... producing a silicate and freeing carbon dioxide, as shown by the equation.
CaCO, 4- Si0 2 CaSiO, + ' CO 2 .
This would partly account for the carbon dioxide coming from the springs, though it is not probable 46 Bulletin University of New Mexico ;Chem. Scr. , Vol. 1 that all of the carbon dioxide issuing from the springs is formed by this reaction alone. Possibly some of this gas is formed by the decomposing of carbonate rocks by highly heated steam formed by water coming in contact with heated rocks deep under the surface of the earth.
What to read after A Preliminary Study of the Waters of the Jemez Plateau New Mexico?
You can find similar books in the "Read Also" column, or choose other free books by Clyde Kelly to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
It is evident that the waters of the sulphate-car- Ixmate class have primarily come up through the Car- boniferous strata, and, since sodium carbonate and cal- cium sulphate are readily soluble in water, have dissolved a large quantity of these alkalies and carried them along in solution. Further on in its course this alka- line water has probably come in contact with some form of granite, such as rhyolite, and dissolved some of the silica. This silica in solution will then act on a car- bonate... producing a silicate and freeing carbon dioxide, as shown by the equation.
CaCO, 4- Si0 2 CaSiO, + ' CO 2 .
This would partly account for the carbon dioxide coming from the springs, though it is not probable 46 Bulletin University of New Mexico ;Chem. Scr. , Vol. 1 that all of the carbon dioxide issuing from the springs is formed by this reaction alone. Possibly some of this gas is formed by the decomposing of carbonate rocks by highly heated steam formed by water coming in contact with heated rocks deep under the surface of the earth.
What to read after A Preliminary Study of the Waters of the Jemez Plateau New Mexico?
You can find similar books in the "Read Also" column, or choose other free books by Clyde Kelly to read onlineMoreLess
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