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Characterization of geothermal scale deposits by Fe-57 Moessbauer spectroscopy and complementary x-ray diffraction and infra-red studies

Journal Article · · Geothermics (International Journal of Geothermal Research and its Applications); (United States)
 [1];  [2]
  1. Unocal Corp., Science and Technology Div., Brea, CA (US)
  2. Dept. of Chemistry, Northeastern Univ., Boston, MA (US)

Scales deposited form Salton Sea, California and Tiwi, Philippines geothermal brines have been analyzed by Fe-57 Mossbauer spectroscopy. Supporting analyses employing X-ray diffraction and infra-red spectroscopy have also been obtained. Mossbauer analyses of the scales detect the presence of six-coordinate, high spin ferric and ferrous iron believed to be present as hydrous silicates resembling the mineral hisingerite. Highly-ordered oxide backgrounds, attributable to corrosion products, as also detected in the scale samples employing this spectral technique. Ferric-rich silicates and corrosion products are commonly observed in scales deposited from acidified brines at high temperature. Ferrous-rich silicates are predominant in scales deposited at low temperature. Mossbauer spectroscopy has proven useful in distinguishing between and quantifying true scale precipitates and poorly crystalline corrosion products. In this paper, Mossbauer analyses are reported for twenty iron mineral phases common to geothermal scale deposits.

OSTI ID:
7117309
Journal Information:
Geothermics (International Journal of Geothermal Research and its Applications); (United States), Journal Name: Geothermics (International Journal of Geothermal Research and its Applications); (United States) Vol. 20:5; ISSN GTMCA; ISSN 0375-6505
Country of Publication:
United States
Language:
English