2002
DOI: 10.1016/s0304-8853(01)00625-4
|View full text |Cite
|
Sign up to set email alerts
|

Mössbauer studies of Y3Fe4.75Al0.25O12

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
2
0

Year Published

2003
2003
2023
2023

Publication Types

Select...
4
1

Relationship

0
5

Authors

Journals

citations
Cited by 6 publications
(3 citation statements)
references
References 8 publications
0
2
0
Order By: Relevance
“…The measured hyperfine fields are typical for ferric iron (Fe 3+ ) in a high-spin configuration. The isomer shift δ at room temperature is δ = 0.35(1) mm/s relative to α-Fe metal, which is consistent with the ferric state (Fe 3+ ) in oxide materials [38,39]. This isomer shift differs from that of Fe 4+ (δ = 0.089 mm/s), which suggests that our BBFO compound has no Fe 4+ ions.…”
Section: Discussionsupporting
confidence: 68%
“…The measured hyperfine fields are typical for ferric iron (Fe 3+ ) in a high-spin configuration. The isomer shift δ at room temperature is δ = 0.35(1) mm/s relative to α-Fe metal, which is consistent with the ferric state (Fe 3+ ) in oxide materials [38,39]. This isomer shift differs from that of Fe 4+ (δ = 0.089 mm/s), which suggests that our BBFO compound has no Fe 4+ ions.…”
Section: Discussionsupporting
confidence: 68%
“…Based on the previous studies, aluminum-substituted iron in YIG were synthesized by different methods such as sol-gel method 14,17,18 , co-precipitation method 19 , and ball milling 16 . Mössbauer spectra for synthesized garnets were fitted with different numbers of components corresponding to Fe 3+ in octahedral and tetrahedral sites.…”
Section: The Magnetic Properties Of Yig With Chemical Compositionmentioning
confidence: 99%
“…Different synthesis routes and heat treatments were adopted for the preparation of iron garnets, including sol-gel method [12,16,17], co-precipitation method [18], and ball milling [13,14,[19][20][21]. Even though YIG garnets with different scenarios of substitution for Fe 3+ , and/ or Y 3+ ions by other rare earth ions were synthesized and carefully characterized, to our best knowledge, no reports were provided on the synthesis and characterization of erbium iron garnet with partial substitution of Fe 3+ ions by Al 3+ ions.…”
Section: Introductionmentioning
confidence: 99%