Characterization of Solid Materials and Heterogeneous Catalysts 2012
DOI: 10.1002/9783527645329.ch10
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Mössbauer Spectroscopy

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Cited by 13 publications
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“…But the two fitted Mössbauer parameters, i.e., the isomer shift (δ) and the quadrupole splitting energy (Δ E QS ) of the ZVI particles (S-N­(C)-mZVI bm , N­(C)-mZVI bm , and mZVI bm ) were different from each other (Figure S9). Since these two parameters originate from hyperfine interactions between the Fe nucleus and its surrounding electronic environment, they should vary with the iron oxidation state, spin state, and chemical surroundings. The differences in the δ and Δ E QS parameters of S-N­(C)-mZVI bm , N­(C)-mZVI bm , and mZVI bm indicate that S and N have influenced the coordination properties of Fe species on S-mZVI bm and S-N­(C)-mZVI bm . Since the XANES spectra of S-N­(C)-mZVI bm at the S K-edge showed the formation of FeS and Mössbauer spectra of N­(C)-mZVI bm proved the presence of Fe-N X (C), it can be inferred that Fe-N X (C) might have been formed on/in S-N­(C)-mZVI bm .…”
Section: Resultsmentioning
confidence: 99%
“…But the two fitted Mössbauer parameters, i.e., the isomer shift (δ) and the quadrupole splitting energy (Δ E QS ) of the ZVI particles (S-N­(C)-mZVI bm , N­(C)-mZVI bm , and mZVI bm ) were different from each other (Figure S9). Since these two parameters originate from hyperfine interactions between the Fe nucleus and its surrounding electronic environment, they should vary with the iron oxidation state, spin state, and chemical surroundings. The differences in the δ and Δ E QS parameters of S-N­(C)-mZVI bm , N­(C)-mZVI bm , and mZVI bm indicate that S and N have influenced the coordination properties of Fe species on S-mZVI bm and S-N­(C)-mZVI bm . Since the XANES spectra of S-N­(C)-mZVI bm at the S K-edge showed the formation of FeS and Mössbauer spectra of N­(C)-mZVI bm proved the presence of Fe-N X (C), it can be inferred that Fe-N X (C) might have been formed on/in S-N­(C)-mZVI bm .…”
Section: Resultsmentioning
confidence: 99%
“…Namely, for spectra recorded in the absence of a strong external magnetic field, metallic iron and iron carbides result in sextets (except for the paramagnetic γ-Fe structure, leading to a singlet), whereas the fingerprint of FeN x C y moieties is a quadrupole doublet. Its two Mössbauer parameters are the isomer shift (δ) and the quadrupole splitting energy (Δ E QS ). These two parameters originate from hyperfine interactions between the iron nucleus and the surrounding electronic environment and vary, therefore, with the iron oxidation state, spin state, and its chemical surrounding …”
Section: Introductionmentioning
confidence: 99%
“…3 ) to Fe 2+ located at M1 and M2 sites, respectively, confirming that also in this case, there is no cationic site preference for the iron ions. The third doublet (green line), less intense than the other two, is characteristic of octahedral Fe 2+ in pyroxene [(Mg,Fe)Si 2 O 6 ] [ 29 ]. Such results agree with the composition determined by XRD analysis, which detected the presence of forsterite, enstatite ferroan and clinochlore [ 20 ].…”
Section: Resultsmentioning
confidence: 99%
“…Moreover, the observed formation of Fe 3+ agrees well with the observations of Raman spectroscopy. The sample measured after 150 min of milling is characterized by the four doublets described previously attributed to Fe 2+ in the two sites of olivine, pyroxene site and superparamagnetic Fe 3+ oxides [ 28 , 29 ]. As the relative area of Fe 3+ doublet increases, those of Fe 2+ sites related to pristine olivine decrease, while the relative area of Fe 2+ related to the pyroxene site remains almost unchanged up to 180 min.…”
Section: Resultsmentioning
confidence: 99%