SI CONTAMINATION IN OPEN FLOW QUARTZ SYSTEMS FOR GROWTH OF GAAS AND GAP

被引:61
作者
WEINER, ME
机构
关键词
CRYSTALS; -; Growing; QUARTZ;
D O I
10.1149/1.2404238
中图分类号
O646 [电化学、电解、磁化学];
学科分类号
081704 ;
摘要
In this paper, calculations are presented for the rates of contamination of liquid gallium with silicon and of flowing H//2 - HCl mixtures with volatile silicon compounds. Ideal gas behavior and local thermodynamic equilibrium are assumed. It is shown that the contact of Ga or HCl with quartz at normal growth temperatures can lead to significant silicon contamination in very dry systems. Models are presented for the formation of high concentrations of Si at the substrate-epitaxial interface and for the formation of SiO//2 precipitates in vapor growth systems. The former has previously been associated with the formation of ″I″ or insulating layers.
引用
收藏
页码:496 / &
相关论文
共 27 条
[1]  
BASS SJ, 1966, GALLIUM ARSENIDE P I, P41
[2]  
CASEY HC, PRIVATE COMMUNICATIO
[3]   REACTIONS OF GALLIUM WITH QUARTZ AND WITH WATER VAPOR, WITH IMPLICATIONS IN THE SYNTHESIS OF GALLIUM ARSENIDE [J].
COCHRAN, CN ;
FOSTER, LM .
JOURNAL OF THE ELECTROCHEMICAL SOCIETY, 1962, 109 (02) :149-154
[4]   OBSERVATION OF OPTICAL PHONONS BOUND TO NEUTRAL DONORS [J].
DEAN, PJ ;
MANCHON, DD ;
HOPFIELD, JJ .
PHYSICAL REVIEW LETTERS, 1970, 25 (15) :1027-&
[5]   OPTICAL PROPERTIES OF GROUP 4 ELEMENTS CARBON AND SILICON IN GALLIUM PHOSPHIDE [J].
DEAN, PJ ;
FROSCH, CJ ;
HENRY, CH .
JOURNAL OF APPLIED PHYSICS, 1968, 39 (12) :5631-&
[6]   ANALYSIS OF IMPURITY DISTRIBUTION IN HOMOEPITAXIAL N ON N+ FILMS OF GAAS WHICH CONTAIN HIGH-RESISTIVITY REGIONS [J].
DILORENZO, JV ;
MARCUS, RB ;
LEWIS, R .
JOURNAL OF APPLIED PHYSICS, 1971, 42 (02) :729-+
[7]  
DILORENZO JV, 1970, MAY EL SOC M LOS ANG
[8]   THE TRANSPORT OF GALLIUM ARSENIDE IN THE VAPOR PHASE BY CHEMICAL REACTION [J].
FERGUSSON, RR ;
GABOR, T .
JOURNAL OF THE ELECTROCHEMICAL SOCIETY, 1964, 111 (05) :585-592
[9]  
FROSCH CJ, 1967, T METALL SOC AIME, V239, P365
[10]  
Hansen M., 1958, J ELECTROCHEM SOC, DOI DOI 10.1149/1.2428700