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...

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Bibliographic Details
Published inJournal of electronic materials Vol. 44; no. 11; pp. 4604 - 4621
Main Authors Henager, CHARLES H., Alvine, Kyle J., Bliss, Mary, Riley, Brian J., Stave, Jean A.
Format Journal Article
LanguageEnglish
Published New York Springer US 01.11.2015
Springer Nature B.V
Springer
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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