1970
DOI: 10.1016/0022-4596(70)90061-7
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New garnet compounds with trivalent rare-earth ions on both dodecahedral and octahedral sites

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Cited by 44 publications
(8 citation statements)
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“…The comparison of these values with those reported in ref is not completely fair, as those were not standardized and therefore not absolute. Moreover, as shown in ref , at low dopant content nonideality of the lattice constant variation versus dopant content is often encountered in these materials.…”
Section: Resultsmentioning
confidence: 85%
See 1 more Smart Citation
“…The comparison of these values with those reported in ref is not completely fair, as those were not standardized and therefore not absolute. Moreover, as shown in ref , at low dopant content nonideality of the lattice constant variation versus dopant content is often encountered in these materials.…”
Section: Resultsmentioning
confidence: 85%
“…In ref it is reported that upon expanding the lattice of YIG by the addition of 25% of the larger Bi 3+ (i.e., (Y 9/4 Bi 3/4 )Fe 5 O 12 ) the site preference of Lu 3+ for the (c) site decreases considerably. The possibility of synthesizing garnets with the general formula Nd 3 (Ga 2 - x RE x )Ga 3 O 12 was systematically investigated by Suchow et al In ref , Nd garnets were considered because of the large radius of Nd 3+ that guarantees that it will only enter the dodecahedral sites. Small rare earths such as Lu 3+ , Yb 3+ , Tm 3+ , Er 3+ , Ho 3+ , and Dy 3+ were investigated.…”
Section: Resultsmentioning
confidence: 99%
“…Mixed fluorides (ZVEREV, KOLODNY) and scheelites (VORONKO et al 1966) have been thoroughly studied. Recently, papers are concerned with mixed garnets their growing and investigation have been reported (BRANDLY, BARNS;VORONKO et al 1972;SUCHOV et al 1970SUCHOV et al , 1972. Generation has been obtained from yttriumlutecium-alluminiuin garnet of the composition Yz,l~Lu~.~~~Nd~.oosAl,O,, (VORONKO et al 1972).…”
Section: Discussion Of Resultsmentioning
confidence: 97%
“…The Ln 3+ distribution over 24c and 16a garnet sites is a topic which has been addressed with several purposes and under different approaches. [15][16][17][18][19][20][21][22][23] The main factor governing the site preference of Ln 3+ in the garnet structure is the ionic size, in such a way that garnets with any Ln 3+ cation occupying the dodecahedral 24c site are known, 15 and only the smallest size Ln 3+ cations, typically Dy 3+ to Lu 3+ and also Y 3+ or Sc 3+ , are able to enter into the octahedral 16a site, even up to its complete filling, but in this case a 24c cation with a considerably large size, for example Ca 2+ in the germanate series Ca 3 Ln 2 Ge 3 O 12 , 18 including Ca 3 Y 2 Ge 3 O 12 , 20 is required, thus the relative sizes of 24c and 16a cations also play a role. The presence of Yb 3+ in both garnet sites would offer the possibility of having the MD probe and ED reference ions in the same tested volume minimizing uncertainties related to excitation and detection processes, but so far the properties of Yb coexisting in both garnet sites have not been properly documented.…”
Section: Introductionmentioning
confidence: 99%
“…The presence of Yb 3+ in both garnet sites would offer the possibility of having the MD probe and ED reference ions in the same tested volume minimizing uncertainties related to excitation and detection processes, but so far the properties of Yb coexisting in both garnet sites have not been properly documented. Either the studies are limited to crystallographic aspects, 16,17,20 or the spectroscopicbased proposals 21,23 are not soundly supported by crystallographic data and/or crystal field (CF) interaction calculations.…”
Section: Introductionmentioning
confidence: 99%