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Goethite, hematite and intermediate products of goetite thermal decomposition were studied by IR and Raman spectroscopy to identify these products used as catalysts of some chemical reactions. The presence of a small number of OH-groups in the products of the decomposition up to 900–1000° C was supposed to hinder the formation of perfect hematite structure. The hypothesis concerning C 3v 6 space group of protohematite indistinguishable from D 3d 6 space group of hematite by X-Ray diffraction was suggested. This hypothesis explains both the additional lines in IR and Raman spectra compared to hematite spectra and the same position of peaks in X-Ray diffraction picture.  相似文献   
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Melnichenko  N. A.  Tyuveev  A. V.  Lazaryuk  A. Yu.  Kustova  E. V.  Kharlamov  P. O. 《Oceanology》2022,62(4):464-470
Oceanology - The article presents the results of a study on the microstructure of fast sea ice in Amur Bay for 2013–2018 based on hydrological observations and magnetic resonance imaging...  相似文献   
3.
Oceanology - Spatial distribution of the liquid and solid phases in the pores of first-year sea ice in Amursky Bay was studied using the method of nuclear magnetic resonance and magnetic resonance...  相似文献   
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