2016
DOI: 10.1007/s10812-016-0380-4
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Spectroscopic Study of Sediments from Chapala Lake in Western Mexico

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Cited by 3 publications
(1 citation statement)
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“…We further performed X‐band electron paramagnetic resonance spectroscopy (EPR) to show the difference in electronic structures of the NiFeCr‐6:2:1, NiFe‐3:1, and NiCr‐2:1 LDH samples and confirm the stability before and after OER measurement ( Figure 4 ). The intense and broad g = 2.0 signal in NiFe‐3:1 sample was indicative of the high‐spin Fe 3+ sites in the octahedral symmetry (3d 5 electronic configuration, S = 5/2 electronic spin) . The weak g = 2.2 signal in NiCr‐2:1 sample was indicative of the Cr 3+ sites in the octahedral symmetry (3d 3 electronic configuration, S = 3/2 electronic spin) .…”
Section: Resultsmentioning
confidence: 98%
“…We further performed X‐band electron paramagnetic resonance spectroscopy (EPR) to show the difference in electronic structures of the NiFeCr‐6:2:1, NiFe‐3:1, and NiCr‐2:1 LDH samples and confirm the stability before and after OER measurement ( Figure 4 ). The intense and broad g = 2.0 signal in NiFe‐3:1 sample was indicative of the high‐spin Fe 3+ sites in the octahedral symmetry (3d 5 electronic configuration, S = 5/2 electronic spin) . The weak g = 2.2 signal in NiCr‐2:1 sample was indicative of the Cr 3+ sites in the octahedral symmetry (3d 3 electronic configuration, S = 3/2 electronic spin) .…”
Section: Resultsmentioning
confidence: 98%