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- W2381731317 abstract "In the structure of valleriite, iron ions may occupy two sites: tetrahedral site in sulfide layer and octahedral site in hydroxide layer. Based on the mossbauer data at room temperature, it is suggested that the high spin Fe 2+ presents in tetrahedral site with isomer shift of 0.42￣ 0.48 mm·s -1 and quadrupole splitting of 0.81￣1.28 mm·s -1 ; while the low spin Fe 3+ in octahedral site with isomer shift of 0.32￣0.36 mm·s -1 and quadrupole splitting of 0.44￣0.59 mm·s -1 ." @default.
- W2381731317 created "2016-06-24" @default.
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- W2381731317 date "1997-01-01" @default.
- W2381731317 modified "2023-09-25" @default.
- W2381731317 title "Mossbauer Spectra of Valleriite from China" @default.
- W2381731317 hasPublicationYear "1997" @default.
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