ESR SPECTRA OF Fe+3 IN SINGLE CRYSTALS OF ANDALUSITE
Keyword(s):
ESR spectra of Fe+3 in andalusite have been investigated at X- and K-band frequencies at room temperature. They have been interpreted on the assumption that Fe+3 occupies the two inequivalent Al+3 sites in andalusite. The spectra show large zero-field splitting. The constants of the conventional orthorhombic spin Hamiltonian which fit the spectra are as follows: for site I: b20 = 15.0 ± 0.1 kG, b22 = 5.0 ± 0.1 kG, and isotropic g = 2.001 ± 0.002; for site II: b20 = 20.1 ± 0.1 kG, b22 = 0.075 ± 0.010 kG, and isotropic g = 2.004 ± 0.0005. A study of the intensities of ESR signals due to site I follow a pattern predicted by theory. The implications of these results are considered briefly.
Keyword(s):
2006 ◽
Vol 61
(5-6)
◽
pp. 289-292
◽
2010 ◽
Vol 645-648
◽
pp. 403-406
◽
Keyword(s):
2008 ◽
Vol 10
(10)
◽
pp. 1387-1394
◽
2011 ◽
Vol 25
(8)
◽
pp. 2697-2700
2008 ◽
Vol 71
(4)
◽
pp. 1623-1626
◽
Keyword(s):