Characterization of geothermal scale deposits by Fe-57 mössbauer spectroscopy and complementary x-ray diffraction and infra-red studies
- 1 January 1991
- journal article
- Published by Elsevier BV in Geothermics
- Vol. 20 (4), 207-224
- https://doi.org/10.1016/0375-6505(91)90033-r
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- Influence of Structural and Adsorbed Si on the Transformation of Synthetic FerrihydriteClays and Clay Minerals, 1989
- Characterization of clay scales forming in Philippine geothermal wellsGeothermics, 1989
- Advances in the study of solids deposition in geothermal systemsGeothermics, 1989
- Nuclear waste glass, and the Fe2+/Fe3+ ratioJournal of Chemical Education, 1988
- Tetrahedral Fe3+ in Ferrihydrite: 57Fe Möossbauer Spectroscopic EvidenceClays and Clay Minerals, 1988
- Effect of silicon on the crystallization and adsorption properties of ferric oxidesEnvironmental Science & Technology, 1985
- Thermal and Mossbauer studies of iron-containing hydrous silicates. II. HisingeriteThermochimica Acta, 1980
- The Influence of [Fe(II)], [Si], and pH on the formation of lepidocrocite and ferrihydrite during oxidation of aqueous FeCl2 solutionsClay Minerals, 1976
- Hisingerite Occurring as a Weathering Product of Iron-Rich SaponiteClays and Clay Minerals, 1975
- Mössbauer Studies of Tektites, Pyroxenes, and OlivinesPublished by American Chemical Society (ACS) ,1967