Ion Beam Mixing in Epitaxial Ag/Fe/Ag-(001)-Layers Investigated with Ferromagnetic Resonance and X-Ray-Diffraction

1997 ◽  
Vol 248-249 ◽  
pp. 177-180 ◽  
Author(s):  
D. Kurowski ◽  
J. Pelzl ◽  
K. Brand ◽  
P. Sonntag ◽  
P. Grünberg
ICAME 2007 ◽  
2008 ◽  
pp. 1203-1210
Author(s):  
P. U. Sharma ◽  
M. K. Roy ◽  
Ravi Kumar ◽  
H. C. Verma ◽  
H. H. Joshi ◽  
...  

1983 ◽  
Vol 27 ◽  
Author(s):  
G. Battaglin ◽  
A. Carnera ◽  
G. Celotti ◽  
G. Della Mea ◽  
V.N. Kulkarni ◽  
...  

ABSTRACTMixing effects induced by Kr++ bombardment in the Au-Fe and Pt-Fe metallic systems have been studied by Rutherford backscattering and X-ray diffraction techniques. The mixed amount of Fe atoms shows a linear dependence on the square root of the Kr do se for both systems. The induced mixing appears more efficient for the Pt-Fe with respect to the Au-Fe system. In the case of Pt-Fe mixing is much more efficient when the initial bilayer structure has Pt on the top. The X-ray diffraction analysis reveals the formation of an extended solid solution of Fe in Pt, having the Fe40 Pt60 composition.


2008 ◽  
Vol 187 (1-3) ◽  
pp. 117-124 ◽  
Author(s):  
P. U. Sharma ◽  
M. K. Roy ◽  
Ravi Kumar ◽  
H. C. Verma ◽  
H. H. Joshi ◽  
...  

1990 ◽  
Vol 67 (2) ◽  
pp. 710-714 ◽  
Author(s):  
S. N. Yedave ◽  
S. M. Chaudhari ◽  
S. M. Kanetkar ◽  
S. B. Ogale ◽  
S. V. Ghaisas

1998 ◽  
Vol 540 ◽  
Author(s):  
L. C. Wei ◽  
R. S. Averback

AbstractIon beam mixing of Cu/Mo multilayer samples and demixing of Cu-Mo alloy samples were examined as functions of temperature and ion mass. Even at liquid nitrogen temperature, the mixing of one component in other was very small under 1.0 MeV Kr irradiation. The maximum solubility was about 10%. Irradiation of homogeneous Cu-Mo alloys under the same conditions, moreover, led to phase separation. These conclusions were deduced from bulk X-ray diffraction measurements and corroborated by EXAFS examination. The maximum solubility obtained by irradiating multilayer samples occurred at about 600 K. At lower or higher temperature, the solubility of Cu in Mo-rich phase was lower. A model based on the ballistic difflusion explains these results.


1989 ◽  
Vol 213 (2-3) ◽  
pp. A230
Author(s):  
M. StróŻak ◽  
P. MikoŁajczak ◽  
M. Subotowicz
Keyword(s):  
Ion Beam ◽  

1995 ◽  
Vol 396 ◽  
Author(s):  
J.K.N. Lindner ◽  
B. Götz ◽  
A. Frohnwieser ◽  
B. Stritzker

AbstractWell-defined, homogenous, deep-buried 3C-SiC layers have been formed in silicon by ion beam synthesis using MeV C+ ions. Layers are characterized by RBS/channeling, X-ray diffraction, x-sectional TEM and electron diffraction. The redistribution of implanted carbon atoms into a rectangular carbon depth distribution associated with a well-defined layer during the post-implantation anneal is shown to depend strongly on the existence of crystalline carbide precipitates in the as-implanted state.


1997 ◽  
Vol 07 (03n04) ◽  
pp. 265-275
Author(s):  
R. Q. Zhang ◽  
S. Yamamoto ◽  
Z. N. Dai ◽  
K. Narumi ◽  
A. Miyashita ◽  
...  

Natural FeTiO 3 (illuminate) and synthesized FeTiO 3, single crystals were characterized by Rutherford backscattering spectroscopy combined with channeling technique and particle-induced x-ray emission (RBS-C and PIXE). The results obtained by the ion beam analysis were supplemented by the x-ray diffraction analysis to identify the crystallographic phase. Oriented single crystals of synthesized FeTiO 3 were grown under the pressure control of CO 2 and H 2 mixture gas using a single-crystal floating zone technique. The crystal quality of synthesized FeTiO 3 single crystals could be improved by the thermal treatment but the exact pressure control is needed to avoid the precipitation of Fe 2 O 3 even during the annealing procedure. Natural FeTiO 3 contains several kinds of impurities such as Mn , Mg , Na and Si . The synthesized samples contain Al , Si and Na which are around 100 ppm level as impurities. The PBS-C results of the natural sample imply that Mn impurities occupy the Fe sublattice in FeTiO 3 or in mixed phase between ilmenite and hematite.


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