RAMAN INVESTIGATION OF H2O MOLECULE AND HYDROXYL GROUPS IN THE CHANNELS OF HEMIMORPHITE

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dc.contributor.author Kolesov B.
dc.date.accessioned 2024-07-20T12:13:53Z
dc.date.available 2024-07-20T12:13:53Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=13519463
dc.identifier.citation American Mineralogist, 2006, 91, 8-9, 1355-1362
dc.identifier.issn 0003-004X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44459
dc.description.abstract Single-crystal polarized Raman spectra (40 to 4000 cm-1 at 4 ≤ T ≤ 860 K) were measured for hemimorphite, Zn4Si2O7(OH)2.H2O, to determine the behavior of H2O molecules and OH groups in the channels. All observed stretching modes of the O-H vibrations could be assigned. Low-temperature Raman spectra show the presence of two different spatially divided regions in the crystal where the H2O molecules and hydroxyl groups have slightly different positions in the channel. Two structural phase transitions were observed at 20-30 and 80-100 K, respectively, which reflect temperature replacement and reorientation of the H2O molecules in the cavity. At T > 100 K, H2O molecules are rotationally disordered around the c axis. An analysis of combined modes consisting of external and internal H2O vibrations permits the frequency of translational T(H2O) modes at 30, 53, 71, 90, 118, and 148 cm-1 to be determined. The T(H2O) modes also can be observed directly at low frequencies in the Raman spectra. The dehydration process of hemimorphite was investigated by Raman measurements at elevated temperatures of the crystal. One of two hydroxyl groups in the dehydrated crystal is hydrogen-bonded to neighbor oxygen and disordered statistically.
dc.subject H2O MOLECULES
dc.subject HEMIMORPHITE
dc.subject MICROPOROUS MINERALS
dc.subject RAMAN SPECTROSCOPY
dc.title RAMAN INVESTIGATION OF H2O MOLECULE AND HYDROXYL GROUPS IN THE CHANNELS OF HEMIMORPHITE
dc.type Статья
dc.identifier.doi 10.2138/am.2006.2179


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