28 2. TUNABLE MATERIALS–CHARACTERISTICS AND CONSTITUTIVE PARAMETERS
2.3.2 HEXAGONAL FERRITES OR HEXAFERRITES–PERMANENT
MAGNETIC FERRITES
Self-Biased Ferrites e distinguishing feature of hexagonal ferrites is their high residual
magnetization, which enables the development of “self biased” microwave devices in the mw
frequency range (e.g., above 30 GHz). It is expected that hexagonal ferrites can be used for
non-reciprocal functions at frequencies up to or higher than 100 GHz. For this purpose, their
large built-in anisotropy field is exploited. However, most of them have a uniaxial permeability
tensor [18, 19]; that is, hexagonal ferrites are mostly used in the mw range in order to eliminate
the need for a very high external DC bias magnetic field.
ChemicalComposition Hexagonal ferrites are, in general, complex crystalline structures with
complicated chemical formulas, which have been given code letters. One large family based on
barium (Ba
+2
) is (Ba
+2
O)
X
(Me
+2
O)
Y
(Fe
2
O
3
)
Z
. Me
+2
is a divalent metallic ion from the first
series of transition elements or a combination of elements with valence equal to two [12]. e
most widely known representatives are BaFe
12
O
19
, with the code letter M (also known as BaM)
and Me
2
BaFe
16
O
27
, with the code letter W. Another widely used hexagonal ferrite is based on
strontium: this is SrFe
12
O
19
, known as SrM.
Saturation Magnetization e saturation magnetization and the anisotropy field of BaM and
SrM can be reduced by partial substitution of cations. In addition, for the W type Ni
2
BaFe
16
O
27
,
a partial substitution of nickel (Ni) by cobalt (Co) lowers its saturation magnetization, while
aluminum’s (Al
+3
) substitution for iron (Fe
+3
) increases both its saturation magnetization and
its anisotropy.
It is important to note that in order to achieve low microwave losses, the ferrite should be
produced with all iron ions in trivalent state so that losses related to electron transfer between
divalent and trivalent iron ions can be prevented.
2.3.3 MAGNETIC GARNETS
It was as early as 1956 that Bertaut and his coworkers [20] synthesized the first magnetic rare-
earth iron garnet in Grenoble. An avalanche of works followed and by the end of the decade,
magnetic garnets, including YIG as the most important along with spinel ferrites, had become
available to microwave engineers [19].
Crystal Structure e garnet crystal structure is very complicated. Each unit cell is composed
of formula units as A
3
B
2
C
3
O
12
, where A, B, and C are trivalent metallic cations [12]. Within
this crystal structure, metal cations are surrounded by oxygen anions in tetrahedron, octahedron,
and dodecahedron coordination, occupied correspondingly by C , B, and A ions. e YIG for-
mula is Y
3
Fe
5
O
12
or Y
+3
! A and Fe
+3
! B plus C. us, Yttrium occupies the dodecahedron
and iron occupies both the tetrahedron and octahedron sites in the crystal structure. An example
of the crystal structure of the garnet is shown in Figure 2.7.