2021
DOI: 10.1007/s42247-021-00323-1
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Green synthesis of cobalt ferrite using grape extract: the impact of cation distribution and inversion degree on the catalytic activity in the decomposition of hydrogen peroxide

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Cited by 24 publications
(6 citation statements)
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“…The Fe-O-Co interface and their bridge formations were attained from the phenolic compounds of the plant extract. The tetrahedral sites of Fe and Co [ 31 , 32 ] were confirmed by the peaks of 912 cm −1 , 545 cm −1 , and 445 cm −1 . The plant compounds induced spinel ferrite formation and motivated enhanced degradation and bio-activities.…”
Section: Resultsmentioning
confidence: 99%
“…The Fe-O-Co interface and their bridge formations were attained from the phenolic compounds of the plant extract. The tetrahedral sites of Fe and Co [ 31 , 32 ] were confirmed by the peaks of 912 cm −1 , 545 cm −1 , and 445 cm −1 . The plant compounds induced spinel ferrite formation and motivated enhanced degradation and bio-activities.…”
Section: Resultsmentioning
confidence: 99%
“…A decrease in  has a relatively weak effect on the number of subspectra corresponding to the A-coordinated Fe 3+ , therefore, all magnetically non-equivalent coordination can be described by only one broad magnetic sextet. At the same time, a decrease in the inverse degree leads to significant changes in the probability of the ion configuration for Bcoordinated Fe 3+ , therefore, in this case, the multiple subspectra should be used [14] The values of isomeric shifts for tetrahedrally coordinated Fe 3+ are relatively smaller due to stronger covalent FeA-O bonds, which makes it possible to identify subspectra. The calculated ratio of the integral intensities of the subspectra corresponding to tetrahedrally and octahedrally coordinated Fe 3+ (SA and SB, respectively) allows calculating the inversion degree parameter as…”
Section: Resultsmentioning
confidence: 99%
“…These spectra have a complex composition; it was optimally fitted with 4 sextet and 2 doublet components, which correspond to differences in the Fe 3+ surrounding that cause changes in the effective magnetic fields at the nuclei and quadrupole splitting values. The association of Fe 3+ ions with tetrahedral and octahedral sites of the crystal structure was made using the values of the isomeric shift () of each sextet component, since  for tetrahedrally coordinated iron ions is lower due to the correspondingly greater strength of Fe-O covalent bonds [8]. An analysis of the integral intensities of the sextet components makes it possible to calculate the distribution of Fe 3+ ions between the tetra (A)-and octa(B)-sublattices: (Ni0.07Fe0.95)A[Ni0.93Fe1.05]BO4.…”
Section: Resultsmentioning
confidence: 99%