Internally Heated Pressure Vessels

  • John R. Holloway


Internally heated pressure vessels (IHPV) are finding increasing applications in the investigation of systems with a non-condensed phase. Although the concept of an IHPV is a general one, and several dissimilar types are in existence, this chapter will emphasize the description and use of relatively large volume, gas-media types capable of operation to pressures of 10 Kb. Also, while the examples described at the end of this chapter are primarily of studies in experimental geochemistry, the IHPV has obvious use in many types of chemical and physical problems.


Pressure Vessel Pressure Port Closure Head Alumina Cement Power Lead 
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  1. Anderson, G.M. and Burnham, C.W. (1965). The solubility of quartz in supercritical water. Amer. J. Sci., 263: 494–511.Google Scholar
  2. Anderson, G.M. and Burnham, C.W. (1967). Reactions of quartz and corundum with aqueous chloride and hydroxide solutions at high temperatures and pressures. Amer. J. Sci., 265: 12–27.Google Scholar
  3. Bell, P.M. and England, J.L. (1967). High pressure experimental techniques,in Researches in geochemistry, Vol. 2, P.H. Abelson, editor. New York: John Wiley and Sons.Google Scholar
  4. Birch, F., Robertson, E.C., and Clark, S.P. (1957). Apparatus for pressures of 27,000 bars and temperatures of 1400°C. Ind. and Eng. Chem., 49: 1965.Google Scholar
  5. Bradley, R.S. and Munro, D.C. (1965). High pressure chemistry. Oxford: Pergamon Press.Google Scholar
  6. Bridgman, P.W. (1949). The physics of high pressure. London: G. Bell and Sons.Google Scholar
  7. Burnham, C.W. (1962). Large volume apparatus for hydrothermal investigations to 10,000 bars and 1500°C (abs). Amer. Ceram. Soc. Program, Seattle, Washington.Google Scholar
  8. Burnham, C.W. (1963). Viscosity of a water-rich pegmatite melt at high pressures (abs). Geol. Soc. Amer. Program 1963 Ann. Mtg.: 26A.Google Scholar
  9. Burnham, C.W. and Davis, N.F. (1969). The partial molar volume of water in albite melts (abs). Trans Amer. Geophys. Union, 50: 338.Google Scholar
  10. Burnham, C.W., Holloway, J.R., and Davis, N.F. (1969). The specific volume of water in the range 1000 to 8900 bars, 20° to 900°C. Amer. J. Sci., ( Schairer Vol. ) 267A: 70–95.Google Scholar
  11. Burnham, C.W. and Jahns, R.H. (1962). A method for determining solubility of water in silicate melts. Amer. J. Sci., 260: 721–745.Google Scholar
  12. Comings, E.W. (1956). High pressure technology. New York: McGraw-Hill.Google Scholar
  13. Downs, H.A., Hastings, J.R., and Waxman, M. (1969). An improved tool for refinishing the conical ends of high pressure tubing. Rev. Sci. Instr., 40: 1238.Google Scholar
  14. Downs, J.L. and Payne, R.T. (1969). A review of electrical feed-through techniques for high pressure gas systems. Rev. Sci. Instr., 40: 1278–1280.Google Scholar
  15. Eugster, H.P. and Skippen, G.B. (1967). Igneous and metamorphic reactions involving gas equilibria, in Researches in geochemistry, Vol. 2, P.H. Abelson, editor. New York: John Wiley and Sons.Google Scholar
  16. Goldsmith, J.R. and Heard, H.C. (1961). Subsolidus relations in the system CaCO3-MgCO3. J. Geol., 69: 45–74.CrossRefGoogle Scholar
  17. Graham, E.K. and Barsch, G.R. (1969). Elastic constants of single-crystal forsterite as a function of temperature and pressure. J. Geophys. Res., 74: 5949–5960.CrossRefGoogle Scholar
  18. Hamilton, D.L., Burnham, C.W., and Osborn, E.F. (1964). The solubility of water and effects of oxygen fugacity and water content on crystallization in mafic magmas. J. Petrol., 5: 21–39.Google Scholar
  19. Holloway, J.R., Burnham, C.W., and Millhollen, G.L. (1968). Generation of H20–0O2 mixtures for use in hydrothermal experimentation. J. Geophys. Res., 73: 6598–6600.Google Scholar
  20. Kennedy, G.C., Wasserburg, G.J., Heard, H.C., and Newton, R.C. (1962). The upper three-phase region in the system Si02H20. Amer. J. Sci., 260: 501–521.Google Scholar
  21. Khitarov, N.I., Lebedev, E.B., Rengarten, E.B., and Arseneva, R.V. (1959). The solubility of water in basaltic and granitic melts. Geochemistry, 5: 479–492.Google Scholar
  22. Kushiro, I. and Yoder, H.S. (1969). Melting of forsterite and enstatite at high pressures under anhydrous conditions. Carnegie Inst. Washington Year Book, 67: 153–158.Google Scholar
  23. Lebedev, E.B.andKhitarov, N.I. ( 1964. ). Dependence of the beginning of melting of granite and the electrical conductivity of its melt on high water vapor pressure. Geochem. International, 2: 193–197.Google Scholar
  24. Newhall, D.H. (1957). Hydraulically driven pumps. Ind. and Eng. Chem., 49: 1949–1954.Google Scholar
  25. Newhall, D.H. and Abbot, L.H. (1968). A contemporary version of the Bridgman-Birch 30 Kb apparatus and certain ancillary devices. Proc. Instn. Mech. Engrs., Part 3C, 182: 288–294.Google Scholar
  26. Piwinskii, A., Weidner, J.R., and Carman, J.H. (1968). Hydrogen osmosis experiments at elevated temperatures and pressures (abs). Geol. Soc. Amer. Program, 1968 Ann. Mtg: 239.Google Scholar
  27. Shaw, H.R. (1967). Hydrogen osmosis in hydrothermal experiments, in Researches in geochemistry, Vol. 2, P.H. Ableson, editor. New York: John Wiley and Sons.Google Scholar
  28. Spetzler, H., Schreiber, E., and Newbigging, D. (1969). Leak detection in high pressure gas system. Rev. Sci. Instr., 40: 179.Google Scholar
  29. Tsiklis, D.S. (1965). Handbook of techniques in high-pressure research and engineering, translated by A. Bobrosky ( 1968 ). New York: Plénum Press.Google Scholar
  30. Vodar, B. and Saurel, J. (1963). The properties of compressed gases, in High pressure physics and chemistry, Vol. 1, R.S. Bradley, editor, London: Academic Press.Google Scholar
  31. Neale, K.E. (1967). Chemical reactions at high pressures. London: E. F.N. Spon.Google Scholar
  32. Williams, D.W. (1966). Externally heated cold-seal pressure vessels for use to 1200°C at 1000 bars. Mineral. Mag., 35: 1003–1012.Google Scholar
  33. Wolf, R.C. and Bowen, J.C. (1957). Compressing of gases in the pure state to high pressures. Ind. and Eng. Chem., 49: 19621964.Google Scholar
  34. Yoder, H.S. (1950). High-low quartz inversion up to 10,000 bars. Trans. Amer. Geophys. Union, 31: 827–835.Google Scholar
  35. Yoder, H.S. (1952). Change of melting point of diopside with pressure. J. Geol., 60: 364–374.CrossRefGoogle Scholar
  36. Yoder, H.S. (1968). Akermanite and related mullite-bearing assemblages. Carnegie Inst. Washington Year Book, 66: 471–477.Google Scholar

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© Springer-Verlag New York Inc. 1971

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  • John R. Holloway

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