Abstract:Applied‐field Mössbauer spectra are reported for selected synthetic samples of α‐Fe1‐xAlxOOH, γ‐Fe1‐xAlxOOH, δ‐FeOOH, α‐(Fe1‐xAlx)2O3 and γ‐Fe2O3. Field strengths of up to 90 kOe were used at temperatures of mostly 4.2 K. The effects of the Al substitution and/or the crystallinity are discussed. Specific characteristics of the spectra are enlightened which might serve as complimentary sources of information for the characterization of soil oxides and oxyhydroxides. It is pointed out that several questions rema… Show more
“…Specifically, this technique showed its potentials in the investigations of Al 3+ [20][21][22][23], Ga 3+ [24] and Sn 4+ [25] substitutions for Fe in ␣-FeOOH.…”
“…Specifically, this technique showed its potentials in the investigations of Al 3+ [20][21][22][23], Ga 3+ [24] and Sn 4+ [25] substitutions for Fe in ␣-FeOOH.…”
“…These measurements showed that the c-dimension was a linear function of Al substitution in the range 0-33 mol% Al, the a-dimension was variable over the same concentration range, whereas the b-dimension slightly deviated from linearity in the range 20-33 mol% Al. Mössbauer spectroscopy found important application in the investigation of Al-doped ␣-FeOOH [15][16][17][18][19].…”
“…Schulze [16] showed that in synthetic Al-substituted ␣-FeOOH crystallites the c-dimension was a linear function of Al-substitution between 0 and 33 mol% Al, the a-dimension varied over the same range, whereas the b-dimension was a linear function up to 20 mol% Al. Mössbauer spectroscopy found important application in the investigation of Al-doped ␣-FeOOH [17][18][19][20][21].…”
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