SURFACE-MORPHOLOGY AND LATTICE DISTORTION OF HETEROEPITAXIAL GAINP ON INP

被引:14
作者
BENSAADA, A
COCHRANE, RW
MASUT, RA
LEONELLI, R
KAJRYS, G
机构
[1] ECOLE POLYTECH,RECH PHYS & TECHNOL COUCHES MINCES,MONTREAL H3C 3A7,QUEBEC,CANADA
[2] ECOLE POLYTECH,DEPT GENIE PHYS,MONTREAL H3C 3A7,QUEBEC,CANADA
[3] UNIV MONTREAL,DEPT PHYS,MONTREAL H3C 3J7,QUEBEC,CANADA
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.1016/0022-0248(93)90530-A
中图分类号
O7 [晶体学];
学科分类号
0702 ; 070205 ; 0703 ; 080501 ;
摘要
We examine the relation between surface morphology and lattice distortions of a number of GaxIn1-xP epilayers (x approximately 0.04) grown On InP (001) substrates using atomic force microscopy (AFM) and high resolution X-ray diffractometry (HRXRD), The heteroepitaxial layers (thickness approximately 1 mum) were grown by low pressure metalorganic vapour phase epitaxy (MOVPE) at temperatures from 600 to 660-degrees-C. AFM images over a scale of 75 mum by 75 mum show no surface corrugations for samples grown at 640-degrees-C. For other growth temperatures between 600 and 660-degrees-C, unidirectional corrugations aligned along the [110] direction or a cross-hatched pattern can be seen on the sample surfaces with a typical interline separation of 10 mum. Another feature revealed by AFM is the presence, for some samples, of weak parallel corrugations along the direction making a 54-degrees angle with the [110BAR] direction. HRXRD spectra recorded first with the [110] and then with the [110BAR] direction in the plane of incidence reveal an asymmetric relaxation in the sample plane accompanied by a broadening of the epilayer X-ray peak for diffraction with the [110] direction in the plane of incidence. The lattice distortion changes from tetragonal to orthorhombic as the surface corrugations appear along the [110BAR] direction. Proton microprobe scans indicate that these samples are compositionally uniform so that the asymmetry is not the result of lateral variations of the alloy composition. Finally, low temperature photoluminescence from these samples shows good agreement between observed and calculated peak positions on the basis of the strains obtained from HRXRD measurements.
引用
收藏
页码:433 / 443
页数:11
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