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A portion of the system silica-water
Abstract
Other| November 01, 1950 A portion of the system silica-water George Clayton Kennedy George Clayton Kennedy Search for other works by this author on: GSW Google Scholar Author and Article Information George Clayton Kennedy Publisher: Society of Economic Geologists First Online: 02 Mar 2017 Online ISSN: 1554-0774 Print ISSN: 0361-0128 GeoRef, Copyright 2006, American Geological Institute. Abstract, Copyright, Society of Economic Geologists. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States Economic Geology (1950) 45 (7): 629–653. https://doi.org/10.2113/gsecongeo.45.7.629 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation George Clayton Kennedy; A portion of the system silica-water. Economic Geology 1950;; 45 (7): 629–653. doi: https://doi.org/10.2113/gsecongeo.45.7.629 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEconomic Geology Search Advanced Search Abstract The solubility of quartz plates in water has been measured at temperatures ranging to 610 degrees C and at pressures ranging to 1,750 bars. Rate of solution of the quartz plates depends on temperature, orientation of the quartz plate and on minute compositional differences in quartz. The solubility determinations have been made along the three-phase boundary, quartz-gas-liquid; and in two two-phase fields, quartz-liquid and quartz-gas. No break is encountered in the solubility curves as they cross the boundary between the quartz-gas and quartz-liquid fields, provided that the specific volume of the fluid phase is held constant.The solubility of quartz in water is much lower than is the solubility of quartz glass or colloidal silica in water. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Citations
Cited by
Pressure solution and the force of crystallization: a phenomenological theory
Weyl, P. K. (1959) · Journal of Geophysical Research · doi:10.1029/jz064i011p02001 · Cited by 593
Gunnarsson, I., & Arnórsson, S. (2000) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(99)00426-3 · Cited by 466
Synthesis of Metal Oxide Nanostructures by Direct Sol–Gel Chemistry in Supercritical Fluids
Sui, R., & Charpentier, P. (2012) · Chemical Reviews · doi:10.1021/cr2000465 · Cited by 313
Correlating quartz dissolution kinetics in pure water from 25 to 625°C
Tester, J. W., Worley, W. G., Robinson, B. A., Grigsby, C. O., & Feerer, J. L. (1994) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(94)90020-5 · Cited by 287
Fluids in the Continental Crust
Yardley, B. W. D., & Bodnar, R. J. (2014) · Geochemical Perspectives · doi:10.7185/geochempersp.3.1 · Cited by 276
Metadata
- Authors
- Kennedy, G. C.
- Venue
- Economic Geology
- Publisher
- Society of Economic Geologists, Inc.
- Published
- 1950-11-01
- Volume
- 45
- Issue
- 7
- Pages
- 629-653
- ISSN
- 0361-0128 (ISSN-L)
- 1554-0774
- OpenAlex
- W2160835451
- Cited by
- 416
- References
- 0
- FWCI
- 5.27
- Type
- journal article
- Language
- en
- Open access
- closed
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