Magnetic anisotropy in Hg1201 and Hg1223 superconducting single crystals

1996 ◽  
Vol 46 (S3) ◽  
pp. 1769-1770 ◽  
Author(s):  
G. Le Bras ◽  
J. Hammann ◽  
A. Bertinotti ◽  
D. Colson ◽  
A. Forget ◽  
...  
Keyword(s):  
Magnetic Anisotropy ◽  
Single Crystals

scholarly journals Reduction of Nd moments and local magnetic anisotropy in Nd2Fe14B single crystals

AIP Advances ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 025224
Author(s):  
H. Sato ◽  
Y. Kubo ◽  
T. Yoshioka ◽  
H. Tsuchiura ◽  
Y. Mizuno ◽  
...  
Keyword(s):  
Magnetic Anisotropy ◽  
Single Crystals

Spin-Lattice Coupling and Peculiarities of Magnetic Behavior of Ferrimagnetic Ludwigites Mn0.52+M1.52+Mn3+BO5(M=Cu, Ni)

2015 ◽  
Vol 233-234 ◽  
pp. 133-136 ◽  
Author(s):  
Leonard Bezmaternykh ◽  
Evgeniya Moshkina ◽  
Evgeniy Eremin ◽  
Maxim Molokeev ◽  
Nikita Volkov ◽  
...  
Keyword(s):  
Temperature Field ◽  
Low Temperature ◽  
Magnetic Anisotropy ◽  
Single Crystals ◽  
Magnetic Behavior ◽  
Temperature Hysteresis ◽  
Spin Lattice ◽  
Field Magnetization ◽  
Lattice Coupling

Temperature-field and orientational magnetization dependences of single crystals were measured. Both samples demonstrate significant field-depending temperature hysteresis and low-temperature counter field magnetization. The correlation of orientational dependences of these effects and magnetic anisotropy is analyzed; the role of spin-lattice interactions is discussed.

Magnetic Anisotropy in Co and Co-Ni Single Crystals Deformed by Cold Rolling

1975 ◽  
Vol 38 (2) ◽  
pp. 391-399 ◽  
Author(s):  
Migaku Takahashi ◽  
Tokuo Wakiyama ◽  
Takeshi Anayama ◽  
Minoru Takahashi ◽  
Takao Suzuki
Keyword(s):  
Cold Rolling ◽  
Magnetic Anisotropy ◽  
Single Crystals

Magnetic Anisotropy in Single Crystals of Zn–Mn and Zn–Cr

1974 ◽  
Vol 52 (18) ◽  
pp. 1759-1764 ◽  
Author(s):  
F. T. Hedgcock ◽  
S. Lenis ◽  
P. L. Li ◽  
J. O. Ström-Olsen ◽  
E. F. Wassermann
Keyword(s):  
Low Temperature ◽  
Magnetic Fields ◽  
Magnetic Anisotropy ◽  
Single Crystals ◽  
Crystal Field ◽  
Interaction Effects ◽  
Crystal Field Splitting ◽  
High Magnetic Fields ◽  
Field Splitting ◽  
Chromium Ion

We have extended the low temperature magnetic anisotropy measurements on single crystals of zinc containing up to 600 p.p.m. manganese from magnetic fields of 9 to 56 kG. The crystal field splitting parameters determined at low magnetic fields also characterizes the magnetic anisotropy at high magnetic fields. Manganese–manganese interaction effects are observed in the magnetic anisotropy at manganese concentrations greater than 300 p.p.m. Low temperature magnetic anisotropy measurements on single crystals of zinc containing up to 164 p.p.m. chromium are reported and indicate a crystal field splitting of 0.16 K for the chromium ion.

Magnetic anisotropy of layered superconducting oxide Bi2Sr2CaCu2O8+δ single crystals

1991 ◽  
Vol 185-189 ◽  
pp. 1857-1858 ◽  
Author(s):  
Kiichi Okuda ◽  
Shuichi Kawamata ◽  
Satoru Noguchi ◽  
Nobutaka Itoh ◽  
Kazuo Kadowaki
Keyword(s):  
Magnetic Anisotropy ◽  
Single Crystals

Pulling single crystals of iron-yttrium garnet with a samarium impurity and a study of the resulting magnetic anisotropy

1976 ◽  
Vol 19 (1) ◽  
pp. 100-103 ◽  
Author(s):  
M. A. Stel'mashenko ◽  
R. F. Uchaikina ◽  
A. V. Kochetkova ◽  
A. D. Barbakov ◽  
V. E. Ginsar ◽  
...  
Keyword(s):  
Magnetic Anisotropy ◽  
Single Crystals ◽  
Iron Yttrium Garnet

scholarly journals Preferred orientation of ferromagnetic phases in rock-forming minerals: insights from magnetic anisotropy of single crystals

2019 ◽  
Vol 56 (9) ◽  
pp. 994-1001 ◽  
Author(s):  
Ann M. Hirt ◽  
Andrea R. Biedermann
Keyword(s):  
Magnetic Field ◽  
Magnetic Anisotropy ◽  
Single Crystals ◽  
Remanent Magnetization ◽  
Igneous Rocks ◽  
Flow Structures ◽  
Silicate Minerals ◽  
Fine Grained ◽  
Crystallographic Axes ◽  
Paleomagnetic Direction

In the early days of paleomagnetism, David Strangway was interested in understanding why igneous rocks are faithful recorders of the Earth’s magnetic field. He recognized that ferromagnetic (s.l.) grains that could be discerned by optical microscopy were too large to carry a stable remanent magnetization, and speculated whether fine-grained, ferromagnetic (s.l.) inclusions or exsolutions in silicate minerals are responsible. When these inclusions or exsolutions are randomly oriented, or the silicate hosts are randomly oriented in a rock, they can be a good recorder of the field. If these minerals, however, show an alignment within the silicate host, and the host is preferentially aligned due to flow structures or deformation, then the paleomagnetic direction and paleointensity could be biased. We examine the magnetic anisotropy arising from the ferromagnetic (s.l.) phases in silicate-host minerals. Single crystals of phyllosilicate, clinopyroxene, and calcite show most consistent ferrimagnetic fabric with relation to the minerals’ crystallographic axes, whereas olivine and feldspar display only a weak relationship. No discernable relationship is found between the ferrimagnetic anisotropy and crystallographic axes for amphibole minerals. Our results have implications when single crystals are being used for either studies of field direction or paleointensity or in cases where silicate minerals have a preferential orientation. Phyllosilicate minerals and pyroxene should be screened for significant magnetic anisotropy.

Magnetic anisotropy in AnTGa5 single crystals

2006 ◽  
Vol 378-380 ◽  
pp. 1015-1017 ◽  
Author(s):  
Eric Colineau ◽  
Franck Wastin ◽  
Pavel Javorský ◽  
Jean Rebizant
Keyword(s):  
Magnetic Anisotropy ◽  
Single Crystals
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