Dissolution of strontianite at high P-T conditions: An in-situ synchrotron X-ray fluorescence study

American Mineralogist

Volumn 88, Issue 7, 2003, Pages 978-985

  Sanchez Valle, Carmen ^a   Martinez, Isabelle ^b   Daniel, Isabelle ^a   Philippot, Pascal ^c   Bohic, Sylvain ^d   Simionovici, Alexandre ^d  

^a UNIVERSITÉ LYON 1   (France)

^b INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

^c CNRS   (France)

^d EUROPEAN SYNCHROTRON RADIATION FACILITY   (France)

Author keywords

[No Author keywords available]

Indexed keywords

DISSOLUTION; FLUORESCENCE; STRONTIUM COMPOUNDS;

DIAMOND-ANVIL CELL; FUNCTION OF TIME; HIGH PRESSURE AND HIGH TEMPERATURE; IN-SITU MEASUREMENT; IN-SITU SYNCHROTRONS; SOLUTION COMPOSITION; SYNCHROTRON X-RAY FLUORESCENCES; TRANSMISSION GEOMETRIES;

X RAYS;

CARBONATE; DISSOLUTION; IN SITU MEASUREMENT; P-T CONDITIONS; STRONTIANITE; X-RAY FLUORESCENCE;

EID: 0042128406     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-2003-0705     Document Type: Article

References (45)

1. 2O activity-composition relations at 600-1000 °C and 6-14 kbar by reversed decarbonation and dehydration reactions. American Mineralogist. 84, 1319-1332.
2. 2O-NaCl fluids at 1.5 and 2.0 GPa pressure: implications for mantle metasomatism. Geochimica et Cosmochimica Acta, 59, 4237-4246.
3. 2O at 2.0-3.0 GPa and 900-1100 °C. and application to models of subduction zone process. Earth and Planetary Science Letters, 150, 381-389.
4. Brenan, J.M., Shaw, H.F., Ryerson, F.J., and Phynney, D.L., (1995). Mineral-aqueous fluid partitioning of trace elements at 900 °C and 2.0 GPa: constraints on the trace elements chemistry of mantle and deep crustal fluids. Geochimica et Cosmochimica Acta, 59, 3331-3350.
5. 3(er) at 25 °C and 1 atm total pressure. Geochimica et Cosmochimica Acta, 48, 2021-2035.
6. Chervin, J.C., Canny, B., Besson, J.M., and Pruzan, P. (1995) A diamond anvil cell for IR microspectroscopy. Review of Scientific Instruments, 66, 2595-2598.
7. 2O fluids. Geochimica et Cosmochimica Acta, 51, 1665-1673.
8. Frantz, J.D., Mao, H.K., Zhang, Y.G., Wu, Y., Thompson, A.C., Underwood, J.H., Giauque, R.D., Jones, K.W., and Rivers, M.L. (1988) Analysis of fluid inclusions by X-ray fluorescence using synchrotron radiation. Chemical Geology, 69, 235-244.
9. Hachnel, O. (1924) Solubilities and properties of the carbonates of Strontium, Barium and heavy metals in water containing carbon dioxide. Journal für Praktische Chemie, 108, 187-193.
10. Hawkesworth, C.J., Gallagher, K., Hergt, J.M., and McDemott, F. (1993) Mantle and slab contributions in arc magmas. Annual Review of Earth and Planetary Sciences, 21, 175-204.
11. Helz, G.R. and Holland, H.D. (1965) The solubility and geologic occurrence of Strontianite. Geochimica et Cosmochimica Acta, 29, 1303-1315.
12. Henke, B.L., Gullikson, E.M., and Davis, J.C. (1993) Atomic Data and Nuclear Data Tables, 54, no. 2, 181-342.
13. Jaklevic, J.M. and Giauque, R.D. (1993) Semiconductor detectors for X-ray spectrometry. In R.E. van Grieken and A.A. Markowicz, Ed., Handbook of X-ray Spectrometry, vol. 14, p. 152-168. Practical Spectroscopy Series. Marcel Dekker. Inc., New York.
14. Keppler, H. (1996) Constraints from partitioning experiments on the composition of subduction-zone fluids. Nature, 380, 237-240.
15. Krause, M.O., Nestor Jr. C.W., Sparks Jr., C.J., and Ricci, E. (1978) ORNL Report Nr. 5399.
16. Lengeler, B., Schroer, C., Tümmler, J., Benner, B., Richwin, M., Snigirev, A., and Snigireva, I. (1999) Imaging by parabolic refractive lenses in the hard x-ray range. Journal of Synchrotron Radiation, 6, 1153-1167.
17. 2O in the lower crust and upper mantle. Geochimica et Cosmochimica Acta, 58, 4381-4839.
18. Manning, C.E. and Boettcher, S.L. (1994) Rapid-quench hydrothermal experiments at mantle pressures and temperatures. American Mineralogist, 79, 1153-1158.
19. Mao, H.K., Bell, P.M., Shaner, J.W., and Steinber, D.J. (1978) Specific volume measurements of Cu, Mo, Pd and Ag and calibration of the ruby R, fluorescence gauge from 0.06 to 1 Mbar. Journal of Applied Physics, 49, 3276-3283.
20. Mavrogenes, J.A., Bodnar, R.J., Anderson, A.J., Bajt, S., Sutton, S.R., and Rivers, M.L. (1995) Assessment of the uncertainities and limitations of quantitative elemental analysis of individual fluid inclusions using synchrotron X-ray fluorescence (SXRF). Geochimica et Cosmochimica Acta, 59, 3987-3995.
21. McCoy, H.N. and Smith, H.J. (1911) Equilibrium between alkali-earth carbonates. Carbon dioxide and water. Journal of the American Chemical Society, 33, 468-473.
22. McCulloch, M.T. and Gamble, J.A. (1991) Geochemical and geodynamical constraints on subduction zone magmatism. Earth and Planetary Science Letters, 102, 358-374.
23. Melzer, S. and Wunder, B. (2001) K-Rb-Cs partitioning between phlogopite and fluid: experiments and consequences for the LILE signatures of island arc basalts. Lithos, 59, 69-90.
24. Ménez, B., Simionovici, A., Philippot, P., Bohic, S., Gibert, F., and Chukalina, M. (2001) X-ray fluorescence micro-tomography of an individual fluid inclusion using a third generation synchrotron light source. Nuclear Instruments and Methods in Physics Research B, 181, 749-754.
25. Ménez, B., Philippot, P., Bonnin-Mosbah, M., Simionovici, A., and Gibert, F. (2002) Analysis of individual fluid inclusions using Synchrotron X-Ray Fluorescence microprobe: progress toward calibration for trace elements. Geochimica et Cosmochimica Acta, 66, 561-576.
26. Millero, F.J., Milne, P.J., and Thurmond, V. (1984) The solubility of calcite, strontianite and witherite in NaCl solutions at 25 °C. Geochimica et Cosmochimica Acta, 48, 1141-1143.
27. Newton, R.C. and Manning, C.E. (2000a) Quartz solubility in concentrated aqueous NaCl solutions at deep crustal-upper mantle pressures and temperatures: 2-15 kbar and 500-900 °C. Geochimica et Cosmochimica Acta, 64, 2993-3005.
28. 2O-NaCl at high pressures and temperatures. International Geology Review, 42, 152-162.
29. Peacock, S.M. (1990) Fluid processes in subduction zones. Science, 248, 329-337.
30. Philippot, P., Ménez, B., Chevallier, P., Gibert, F., Legrand, F., and Populus, P. (1998) Absorption correction procedures for quantitative analysis of fluid inclusions using synchrotron radiation X-ray fluorescence. Chemical Geology, 144, 121-136.
31. 2O. Geochimica et Cosmochimica Acta, 46, 1011-1040.
32. Plummer, L.N. (1987) Thermodynamics of aragonite-strontianite solid solutions: Results from stoichiometric solubility at 25 and 76 °C. Geochimica et Cosmochimica Acta, 54, 1393-1411.
33. 2 fluorescence shift as a function of temperature from 0 to 600 K. Journal of Applied Physics, 72, 5539-5544.
34. Roedder, E. (1984) Fluid inclusions, vol. 12. Reviews in Mineralogy, Mineralogical Society of America, Washington, D.C.
35. Sanchez del Rio, M. and Dejus, R.J. (1997) Proceedings SPIE, 3152, 148.
36. Scambelluri, M. and Philippot, P. (2001) Deep fluids in subduction zones. Lithos. 55, 213-227.
37. Schmidt, C. and Rickers, K. (2002) In situ determination of mineral solubilities at high pressures and temperatures using synchrotron radiation XRF. Hydrothermal fluid geochemistry. EMPG IX, Abstracts, p. 96.
38. 2O in the two phases region calcite and aqueous solution. Journal of Geology, 73, 391-403.
39. Snigirev, A., Kohn, V.G., Snigireva, I., and Lengeler, B. (1996) A compound refractive lens for focusing high energy X-rays. Nature, 384, 49-51.
40. Sonderegger, J.L., Brower, K.R., and LeFebre, V.G.A. (1976) A preliminary investigation of strontianite dissolution kinetics. American Journal of Science, 276, 997-1022.
41. Sparks, C.J. (1980) X-ray Fluorescence Microprobe for Chemical Analysis. In H. Winick and S. Doniach, Ed., Synchrotron Radiation Research, p. 459-512. Plenum, New York.
42. Stalder, R., Foley, S.F., Brey, G.P., and Horn, I. (1998) Mineral-aqueous fluid partitioning of trace elements at 900-1200 °C and 3.0-5.7 GPa: New experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism. Geochimica et Cosmochimica Acta, 62, 1781-1801.
43. Vekemans, B., Janssens, K., Vincze, L., Adams, F., and Van Espen, P. (1994) Analysis of X-ray spectra by iterative least squares (AXIL): New developments. X-Ray Spectrometry, 23, 278-285.
44. Walther, J.V. and Orville, P.M. (1983) The extraction-quench technique for determination of the thermodynamic properties of solute complex: application to quartz solubility in fluid mixtures. American Mineralogist, 68, 731-741.
45. Zotov, N. and Keppler, H. (2002) Silica speciation in aqueous fluids at high pressures and high temperatures. Chemical Geology, 184, 71-82.