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Featured researches published by Ray K. Eby.


Journal of Materials Research | 1992

The amorphization of complex silicates by ion-beam irradiation

Ray K. Eby; Rodney C. Ewing; R.C. Birtcher

Twenty-five silicates were irradiated at ambient temperature conditions with 1.5 MeV Kr[sup +]. Critical doses of amorphization were monitored [ital in] [ital situ] with transmission electron microscopy. The doses required for amorphization are compared with the structures, bond-types, compositions, and physical properties of the silicates using simple correlation methods and more complex multivariate statistical analysis. These analyses were made in order to determine which properties most affect the critical amorphization dose. Simple two-variable correlations indicate that melting point, efficiency of atomic packing, the dimensionality of SiO[sub 4] polymerization (DOSP), and bond ionicity have a relationship with critical amorphization dose. However, these relationships are evident only in selected portions of the data set; that is, for silicate phases with a common structure type.


MRS Proceedings | 1990

Ion-Irradiation Study of the “Exotic” Mineral Neptunite: LiNa 2 K(Fe,Mg,Mn) 2 Ti 2 Si 8 O 24

Ray K. Eby; L.M. Wang; G. W. Arnold; Rodney C. Ewing

Single crystals of the silicate neptunite were irradiated with 600 keV Ar 2+ and 1.5 MeV Kr + and analysed by transmission electron microscopy. Amorphization was observed in a surface layer several hundred angstroms thick following Ar 2+ irradiations up to 5.0×l0 13 Ar/cm 2 , yet the Ar 2+ ions travelled an average of 1/2 μm in depth. The microstructure of the amorphous surface layer depends on the ion fluence, but the amorphous layer thickness remained constant. At the highest fluence, a narrow region below the amorphous layer shows a brittle-to-ductile strain transition, due to tensional volume-expansion of the adjacent ductile amorphous layer. With 1.5 MeV Kr1 + , amorphization of the electron transparent region was completed after a fluence of 1.7×l0 14 Kr + /cm 2 , and no further damage was observed up to 5.1×10 15 Kr + /cm 2 . However, following a low fluence of 2.0×10 11 Kr + /cm 2 , a single crystal of neptunite became a polycrystalline aggregate (grain size 10 nm) within 7 days of room temperature aging.


Journal of Materials Research | 1991

Alpha-recoil damage in titanite (CaTiSiO 5 ): Direct observation and annealing study using high resolution transmission electron microscopy

G.R. Lumpkin; Ray K. Eby; Rodney C. Ewing


Journal of Materials Research | 1991

Accumulation of structural defects in ion-irradiated Ca2Nd8(SiO4)6O2

William J. Weber; Ray K. Eby; Rodney C. Ewing


Acta Crystallographica Section C-crystal Structure Communications | 1990

Clinoclase and the geometry of [5]-coordinate Cu2+ in minerals

Ray K. Eby; Frank C. Hawthorne


Canadian Mineralogist | 1993

METAMICT AND CHEMICALLY ALTERED VESUVIANITE

Ray K. Eby; J. Janeczek; Rodney C. Ewing; T. S. Ercit; L. A. Groat; Bryan C. Chakoumakos; Frank C. Hawthorne; George R. Rossman


Acta Crystallographica Section C-crystal Structure Communications | 1989

Euchroite, a heteropolyhedral framework structure

Ray K. Eby; Frank C. Hawthorne


Beam Solid Interactions: Fundamentals and Applications | 1992

Temperature and ion-mass dependence of amorphization dose for ion beam irradiated zircon (ZrSiO[sub 4])

L.M. Wang; Rodney C. Ewing; William J. Weber; Ray K. Eby


MRS Proceedings | 1990

Annealing of Alpha-Recoil Damage in Natural Titanite, CaTiSiO 5 .

Ray K. Eby; Rodney C. Ewing


MRS Proceedings | 2005

Patterning PETN and HMX using Dip Pen Nanolithography

Omkar A. Nafday; Brandon L. Weeks; Jason R. Haaheim; Ray K. Eby

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L.M. Wang

University of New Mexico

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Bryan C. Chakoumakos

Oak Ridge National Laboratory

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G. W. Arnold

Sandia National Laboratories

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G.R. Lumpkin

University of New Mexico

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George R. Rossman

California Institute of Technology

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J. Janeczek

University of New Mexico

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