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American Journal of Science

Aagaard, P. and H. C. Helgeson, 1982, Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions, I. Theoretical considerations. American Journal of Science 282,237-285. [Pg.509]

Brady, J. B., 1975, Chemical components and diffusion. American Journal of Science 275,1073-1088. [Pg.512]

Brown, T. H. and B. J. Skinner, 1974, Theoretical prediction of equilibrium phase assemblages in multicomponent systems. American Journal of Science 274, 961-986. [Pg.513]

Eugster, H. P. and B. F. Jones, 1979, Behavior of major solutes during closed-basin brine evolution. American Journal of Science 279, 609-631. [Pg.515]

Fournier, R. O. and J. J. Rowe, 1966, Estimation of underground temperatures from the silica content of water from hot springs and wet-steam wells. American Journal of Science 264, 685-697. [Pg.515]

Garven, G. and R. A. Freeze, 1984, Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits, 2, quantitative results. American Journal of Science 284, 1125-1174. [Pg.516]

Haas, J.L., Jr. and J.R. Fisher, 1976, Simultaneous evaluation and correlation of thermodynamic data. American Journal of Science 276,525-545. [Pg.516]

Helgeson, H. C., 1969, Thermodynamics of hydrothermal systems at elevated temperatures and pressures. American Journal of Science 267,729-804. [Pg.517]

Helgeson, H. C., D. H. Kirkham and G. C. Flowers, 1981, Theoretical prediction of the thermodynamic behavior of aqueous electrolytes at high temperatures and pressures, IV. Calculation of activity coefficients, osmotic coefficients, and apparent molal and standard and relative partial molal properties to 600 °C and 5 kB. American Journal of Science 281, 1249-1516. [Pg.518]

Hostettler, J. D., 1984, Electrode electrons, aqueous electrons, and redox potentials in natural waters. American Journal of Science 284,734—759. [Pg.518]

Kulik, D. A., 2002, Gibbs energy minimization approach to model sorption equilibria at the mineral-water interface Thermodynamic relations for multi-site-surface complexation. American Journal of Science 302,227-279. ... [Pg.521]

Lasaga, A. C. and D. M. Rye, 1993, Fluid flow and chemical reaction kinetics in metamorphic systems. American Journal of Science 293, 361 104. [Pg.522]

Lee, M.-K. and C. M. Bethke, 1996, A model of isotope fractionation in reacting geochemical systems. American Journal of Science 296,965-988. [Pg.522]

Merino, E., D. Nahon and Y. Wang, 1993, Kinetics and mass transfer of pseudo-morphic replacement, application to replacement of parent minerals and kaoli-nite by Al, Fe, and Mn oxides during weathering. American Journal of Science 293,135-155. [Pg.524]

Morse, J. W. and W. H. Casey, 1988, Ostwald processes and mineral paragenesis in sediments. American Journal of Science 288, 537-560. [Pg.524]

Ortoleva, P. J., E. Merino, C. Moore and J. Chadam, 1987, Geochemical selforganization, I., Reaction-transport feedbacks and modeling approach. American Journal of Science 287, 979-1007. [Pg.526]

Steefel, C. I. and A.C. Lasaga, 1994, A coupled model for transport of multiple chemical species and kinetic precipitation/dissolution reactions with application to reactive flow in single phase hydrothermal systems. American Journal of Science 294, 529-592. [Pg.530]

Berner, R.A. Morse, J.M. 1974. Dissolution kinetics of calcium carbonate in seawater. IV. Theory of calcite dissolution, American Journal of Science, 274,108-134. [Pg.62]

Hedges, J.I., F.S. Hu, A.H. Devol, H.E. Hartnett, and R.G. Keil. 1999. Sedimentary organic matter preservation A test for selective oxic degradation. American Journal of Science 299 529-555. [Pg.118]

Figure 2J Enthalpy, entropy, heat capacity, and volume modification in a-quartz/ /3-quartz transition region. Reprinted from H. C. Helgeson, J. Delany, and D. K. Bird, American Journal of Science, 278A, 1-229, with permission. Figure 2J Enthalpy, entropy, heat capacity, and volume modification in a-quartz/ /3-quartz transition region. Reprinted from H. C. Helgeson, J. Delany, and D. K. Bird, American Journal of Science, 278A, 1-229, with permission.
Figure 5.48 Extrinsic stability limits of muscovite, based on equilibrium 5.140 for variable amounts of H2O component in fluid. Also shown are incipient melting curves of granite for various h20 isopleths and stability curves of Al2Si05 polymorphs, according to Holdaway (1971) From Kerrick (1972), American Journal of Science, 212, 946-58. Reprinted with permission of American Journal of Science. Figure 5.48 Extrinsic stability limits of muscovite, based on equilibrium 5.140 for variable amounts of H2O component in fluid. Also shown are incipient melting curves of granite for various h20 isopleths and stability curves of Al2Si05 polymorphs, according to Holdaway (1971) From Kerrick (1972), American Journal of Science, 212, 946-58. Reprinted with permission of American Journal of Science.
Figure 8,6 (A) P-T regions of H2O stability. (B) Extended P-T field showing location of the critical region. The critical isochore is p = 0.322778 g/cm. From Johnson and Norton (1991), American Journal of Science, 291, 541-648. Reprinted with permission of American Journal of Science. Figure 8,6 (A) P-T regions of H2O stability. (B) Extended P-T field showing location of the critical region. The critical isochore is p = 0.322778 g/cm. From Johnson and Norton (1991), American Journal of Science, 291, 541-648. Reprinted with permission of American Journal of Science.
Figure 8.33 Reaction mechanism contribution to the total rate of calcite dissolution reaction as a function of pH and Pco2 25 °C. From L. N. Plummer, T. M. L. Wigley, and D. L. Pankhurst (1978), American Journal of Science, 278, 179-216. Reprinted with permission of American Journal of Science. Figure 8.33 Reaction mechanism contribution to the total rate of calcite dissolution reaction as a function of pH and Pco2 25 °C. From L. N. Plummer, T. M. L. Wigley, and D. L. Pankhurst (1978), American Journal of Science, 278, 179-216. Reprinted with permission of American Journal of Science.
American Journal of Science, 275, 353-76. Reprinted with permission of American Journal of Science. [Pg.628]

Figure 9.8 Speciation of volcanic gases with different C/H and C/S relative amounts as a function of /q at T = 1250 °C. From Gerlach and Nordlie (1975a), American Journal of Science, 275, 353-76. Reprinted with permission of American Journal of Science. Figure 9.8 Speciation of volcanic gases with different C/H and C/S relative amounts as a function of /q at T = 1250 °C. From Gerlach and Nordlie (1975a), American Journal of Science, 275, 353-76. Reprinted with permission of American Journal of Science.
Ramezani, J. Tucker R.D. 2003. The Saghand region. Central Iran U-Pb geochronology, petrogenesis and implications for Gondwana tectonics. American Journal of Science, 303, 622-665. [Pg.126]

Pearce, J. 1996. Sources and settings of granitic rocks. Episodes, 24, 956-983. Schilling, J.-K. et al. 1983. Petrologic variations along the Mid-Atlantic Ridge from 29°N to 73°N. American Journal of Science, 283, 510-586. [Pg.146]

Villar Fabre, J. Quartino, B. 1966. Exomorphic and endomorphic effects from marble-contaminated granite contacts in the San Miguel quarry, Barker, Province of Buenos Aires, Argentina. American Journal of Science, 264, 310-320. [Pg.284]

American Journal of Science, Kline Geological Laboratory, New Haven, CT, USA A figure from D. Langmuir (1971), Am. J. Science, 271, 147-156 was reprinted by permission of American Journal of Science. [Pg.659]

Fritts CE (1883) On a New Form of Selenium Photocell. Proc American Association for the Advancement of Science. 33 97 and American Journal of Science 26 465... [Pg.511]

The American Journal of Science for 1840 described an amazing phenomenon caused by this kind of gas. At West Town, Chester County, Pennsylvania, the students of the boarding school used to bathe in a mill-pond supplied by Chester Creek. Rising from the creek were countless bubbles of gas from decaying leaves and wood (25). "I first visited the place in the year 1834, said Moses Lockwood. Taking as apparatus a bell-glass furnished with a stop-cock and a taper, and as companion an assistant teacher. . ., we proceeded to the pond, readily filled the... [Pg.80]

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