Date of Award
10-1991
Document Type
Dissertation - Restricted
Degree Name
Doctor of Philosophy (PhD)
Department
Mechanical Engineering
First Advisor
Robert F. Brebrick
Second Advisor
Robert N. Blumenthal
Third Advisor
Louis Cartz
Fourth Advisor
Raymond A. Fournelle
Fifth Advisor
Martin A. Seitz
Abstract
Mercury zinc telluride, (Hg1-xZnx)1-yTey, has been considered as an alternative material to (Hg1-xCdx)1-yTey for infrared opto-electronic devices due to its superior structural properties. Considerable research effort has been expended on the HgTe-ZnTe solid solutions. However, the experimental thermodynamic and phase diagram data for this ternary system are limited. The experimental technique consisted of measuring the optical density of the vapor phase coexisting with a sample of the solid solution in a sealed optical cell of known volume and temperature. In high temperature measurements between 500 and 800°C with a high pressure Xenon lamp, the partial pressures of mercury PHg and of diatomic tellurium P2 have been determined for x = 0.10, 0.20, 0.30, 0.50, and 0.70. The optical density was measured between 250 and 750 nm. It was possible to place narrow limits on the solidus temperature for some of the x values and to derive the chemical potential of HgTe in the solid solutions. In low temperature measurements between 100 and 230°C with a Hg hollow-cathode lamp, the partial pressures of mercury PHg has been determined for the Te- saturated solid solutions for x = 0.0, 0.10, 0.20, 0.30, 0.50, and 0.70. The optical density was measured at 253.7 nm. For Te-saturated HgTe(c), the data below the 686 K eutectic temperature with Te(c) were used to calculate the standard Gibbs energy of formation and to obtain ΔH°f,298 and ΔS°f,298. Results agree with previous single beam measurements and high temperature optical density measurements within the 95% confident level uncertainties. The standard enthalpy of formation at 298 K differs significantly from the value published by others. For the Te-saturated solid solutions, the partial pressures indicate a miscibility gap between x = 0.10 and 0.50 for the entire 100-230°C range. X-ray diffraction patterns do not show the two sets of lines required for a miscibility gap. However, the diffraction lines are significantly broader than the instrumental half-width. It appears that the attainment of equilibrium, and the formation of a miscibility gap was restricted to a surface layer thin relative to the X-ray penetration depth of about 12 μm.