Magnetic properties of isotropic SrFe12O19 fine particles prepared by mechanical alloying
被引:52
作者:
Jin, ZQ
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机构:
Nanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R ChinaNanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R China
Jin, ZQ
[1
]
Tang, W
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机构:Nanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R China
Tang, W
Zhang, JR
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机构:Nanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R China
Zhang, JR
Lin, H
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机构:Nanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R China
Lin, H
Du, YW
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机构:Nanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R China
Du, YW
机构:
[1] Nanjing Univ, Natl Lab Solid State Microstruct, Nanjing 210093, Peoples R China
[2] Nanjing Univ, Dept Phys, Inst Solid State Phys, Nanjing 210093, Peoples R China
mechanical alloying;
ferrite;
magnetic properties;
D O I:
10.1016/S0304-8853(97)00679-3
中图分类号:
T [工业技术];
学科分类号:
08 ;
摘要:
M-type Sr-hexaferrites fine particles have been prepared by mechanical alloying. The influences of milling conditions on magnetic properties of SrFe12O19 compounds have been systematically investigated. It can be found that annealing treatment at low temperature can play similar role in structural transformation as compared with long time milling process. For those samples annealed at about 750-800 degrees C, it is clear that saturation magnetization sigma(s), values are more sensitive to milling conditions than coercivity values H-c. The maximum sigma(s) of 74.8 emu/g and H-c of 5.6 kOe have been obtained in the isotropic powders annealed at 1000 degrees C after milling for 30 h by using high energy mill. With prolonged annealing time, little changes of magnetic saturation and coercivity in powders can be observed and short annealing time results in low properties. The coercive field H-c, as determined from demagnetization curve, corresponds to the pinning or nucleation field. (C) 1998 Elsevier Science B.V. All rights reserved.
机构:
PENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USAPENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USA
HODGE, MH
;
BITLER, WR
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机构:
PENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USAPENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USA
BITLER, WR
;
BRADT, RC
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机构:
PENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USAPENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USA
机构:
PENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USAPENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USA
HODGE, MH
;
BITLER, WR
论文数: 0引用数: 0
h-index: 0
机构:
PENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USAPENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USA
BITLER, WR
;
BRADT, RC
论文数: 0引用数: 0
h-index: 0
机构:
PENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USAPENN STATE UNIV, COLL EARTH & MINERAL SCI, MAT SCI DEPT, UNIVERSITY PK, PA 16802 USA