The Influence of Constitutional Supercooling on the Distribution of Te-Particles in Melt-Grown CZT
A section of a vertical gradient freeze Cd 0.9 Zn 0.1 Te boule approximately 2100 mm 3 with a planar area of 300 mm 2 was prepared and examined using transmitted infrared microscopy at various magnifications to determine the three-dimensional spatial and size distributions of Te-particles over large...
Saved in:
Published in | Journal of electronic materials Vol. 44; no. 11; pp. 4604 - 4621 |
---|---|
Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
New York
Springer US
01.11.2015
Springer Nature B.V Springer |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Summary: | A section of a vertical gradient freeze Cd
0.9
Zn
0.1
Te boule approximately 2100 mm
3
with a planar area of 300 mm
2
was prepared and examined using transmitted infrared microscopy at various magnifications to determine the three-dimensional spatial and size distributions of Te-particles over large longitudinal and radial length scales. Te-particle density distributions were determined as a function of longitudinal and radial positions in these strips and exhibited a multi-modal log-normal size density distribution that indicated a slight preference for increasing size with longitudinal growth time, while showing a pronounced cellular network structure. Higher magnification images revealed a typical Rayleigh-instability pearl string morphology with large and small satellite droplets. This study includes solidification experiments in small crucibles of 30:70 mixtures of Cd:Te performed over a wide range of cooling rates which clearly demonstrated a growth instability with Te-particle capture that is suggested to be responsible for one of the peaks in the size distribution using size discrimination visualization. The results are discussed with regard to a manifold Te-particle genesis history as Te-particle direct capture from melt–solid growth instabilities due to constitutional supercooling and as Te-particle formation from the breakup of Te-ribbons via a Rayleigh–Plateau instability. |
---|---|
Bibliography: | USDOE AC05-76RL01830 PNNL-SA-107729 |
ISSN: | 0361-5235 1543-186X |
DOI: | 10.1007/s11664-015-3995-y |