1975
DOI: 10.1007/bf00526167
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The ESR and paramagnetic relaxation of Fe3+ in sulfonic acid ion-exchange resins

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Cited by 2 publications
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“…The width of a large line is about 800 Oe for samples heated at ≤140°C and decreases to 400 Oe for samples heated at >140°C. The signals at g = 4.3 and 2.003 (wide line) are attributed to the Fe(III) ions in rhombic and octahedral surroundings, respectively 16. As is known, jarosite‐type compounds consist of octahedrons.…”
Section: Resultsmentioning
confidence: 94%
“…The width of a large line is about 800 Oe for samples heated at ≤140°C and decreases to 400 Oe for samples heated at >140°C. The signals at g = 4.3 and 2.003 (wide line) are attributed to the Fe(III) ions in rhombic and octahedral surroundings, respectively 16. As is known, jarosite‐type compounds consist of octahedrons.…”
Section: Resultsmentioning
confidence: 94%
“…Typically no Fe 3+ spectral line is observed downfield in either plant sample material. According to [8,17], this first of all may be associated with these ions predominantly existing in the form of hexaaqua complexes [Fe(H 2 O)6] 3+ with pseudo-octahedral symmetry of the environment, observed in the g ~ 2 region, compared with rhombically distorted complexes appearing at g ~ 4. Secondly, the signal from lowsymmetry centers in the g ~ 4 region may undergo considerable broadening due to the short relaxation times.…”
mentioning
confidence: 99%