THE AMORPHIZATION OF COMPLEX SILICATES BY ION-BEAM IRRADIATION

被引:94
作者
EBY, RK
EWING, RC
BIRTCHER, RC
机构
[1] UNIV NEW MEXICO,DEPT GEOL,ALBUQUERQUE,NM 87131
[2] ARGONNE NATL LAB,ARGONNE,IL 60439
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.1557/JMR.1992.3080
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Twenty-five silicates were irradiated at ambient temperature conditions with 1.5 MeV Kr+. Critical doses of amorphization were monitored in 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 SiO4 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. A clearer relationship between the silicate properties and critical amorphization dose was determined for the entire data set with multiple linear regression. Several regression models are proposed which describe the variation in amorphization dose. All regression models contain the following properties: (i) melting point; (ii) a structural variable (DOSP, elastic modulus, and/or atomic packing); and (iii) the proportion of Si-O bonding (instead of bond ionicity). The regression models are equivalent, because they represent combinations of similar properties. Notably, density and atomic mass are not controlling properties for the critical amorphization dose. Melting and amorphization by ion irradiation are apparently related processes. Neither melting point nor critical amorphization dose can be predicted by considering only the structure, composition, or bonding of a particular phase. The Si-O bond is the most covalent bond in silicates, and is the "weak link" in the structure with respect to amorphization. Thus, DOSP is also an important property, as the topology of these "weak links" influences a structure's ability to accumulate amorphous regions. The efficiency of atomic packing is related to the process of defect self-recombination during amorphization. The bulk modulus and shear modulus are important variables within the regression models because of their direct relationship to atomic packing.
引用
收藏
页码:3080 / 3102
页数:23
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