Simulation of radial dopant segregation in vertical Bridgman growth of GaSe, a semiconductor with anisotropic solid-phase thermal conductivity

2001 ◽  
Vol 231 (1-2) ◽  
pp. 148-170 ◽  
Author(s):  
Hanjie Lee ◽  
Arne J. Pearlstein
2001 ◽  
Vol 123 (4) ◽  
pp. 729-740 ◽  
Author(s):  
Hanjie Lee ◽  
Arne J. Pearlstein

For vertical Bridgman growth of thermally anisotropic semiconductors, we present a detailed model accounting for heat transfer, flow driven by thermal buoyancy and solidification shrinkage, and interface deformation. The model allows for anisotropic solid-phase thermal conductivity, characteristic of nonlinear optical materials, as well as conduction in the ampoule wall, and conduction and convection in the liquid. The interface shape is determined as part of the solution of a moving boundary problem. For the nonlinear optical material gallium selenide and a range of growth conditions of practical interest, we present steady axisymmetric computations of the isotherms, flow, and interface shape. For ampoule-wall temperature profiles typical of three-zone Bridgman furnaces, the strength of the flow and deflection of the interface increase considerably with increasing growth rate, while the temperature distribution is relatively insensitive, except near the interface. Interface deflection decreases as the maximum ampoule-wall temperature gradient increases. The flow depends significantly on whether the melting temperature is “centered” between the high and low temperatures. The 23°C uncertainty in the melting temperature of GaSe is shown to have little effect on the flow and interface shape over the entire range of growth conditions. We show that properly accounting for thermal anisotropy is critical to predicting the flow and interface shape, both of which are relatively insensitive to the temperature dependence of the viscosity and thermal conductivities. We also show that localized heating along the ampoule wall can both reverse the direction of flow along the interface, which is expected to significantly influence distribution of dopants or impurities in the solid phase, as well as reduce interfacial curvature. When GaSe is grown under zero gravity conditions, the only flow is due to solidification shrinkage, and is essentially normal to the interface, whose shape is similar to those computed at normal gravity. Comparison of results for GaSe to previous work for benzene, a surrogate for organic nonlinear optical materials, shows that the qualitatively different results are associated with differences in the anisotropy of the thermal conductivity.


2002 ◽  
Author(s):  
Julaporn Kaenton ◽  
Victoria Timchenko ◽  
Mohammed El Ganaoui ◽  
Graham de Vahl Davis ◽  
Eddie Leonardi ◽  
...  

2018 ◽  
Vol 25 (6) ◽  
pp. 1157-1165
Author(s):  
Taoufik Mnasri ◽  
Adel Abbessi ◽  
Rached Ben Younes ◽  
Atef Mazioud

AbstractThis work focuses on identifying the thermal conductivity of composites loaded with phase-change materials (PCMs). Three configurations are studied: (1) the PCMs are divided into identical spherical inclusions arranged in one plane, (2) the PCMs are inserted into the matrix as a plate on the level of the same plane of arrangement, and (3) the PCMs are divided into identical spherical inclusions arranged periodically in the whole matrix. The percentage PCM/matrix is fixed for all cases. A comparison among the various situations is made for the first time, thus providing a new idea on how to insert PCMs into composite matrices. The results show that the composite conductivity is the most important consideration in the first case, precisely when the arrangement plane is parallel with the flux and diagonal to the entry face. In the present work, we are interested in exploring the solid-solid PCMs. The PCM polyurethane and a wood matrix are particularly studied.


2000 ◽  
Vol 17 (10) ◽  
pp. 775-777 ◽  
Author(s):  
Liu Yong-Cai ◽  
Chen Wan-Chun ◽  
Ge Pei-Wen ◽  
Huo Chong-Ru

2013 ◽  
Vol 2013 ◽  
pp. 1-7 ◽  
Author(s):  
Kan Ankang ◽  
Han Houde

Based on the fractal theory, the geometric structure inside an open cell polyurethane foam, which is widely used as adiabatic material, is illustrated. A simplified cell fractal model is created. In the model, the method of calculating the equivalent thermal conductivity of the porous foam is described and the fractal dimension is calculated. The mathematical formulas for the fractal equivalent thermal conductivity combined with gas and solid phase, for heat radiation equivalent thermal conductivity and for the total thermal conductivity, are deduced. However, the total effective heat flux is the summation of the heat conduction by the solid phase and the gas in pores, the radiation, and the convection between gas and solid phase. Fractal mathematical equation of effective thermal conductivity is derived with fractal dimension and vacancy porosity in the cell body. The calculated results have good agreement with the experimental data, and the difference is less than 5%. The main influencing factors are summarized. The research work is useful for the enhancement of adiabatic performance of foam materials and development of new materials.


2010 ◽  
Vol 14 (1) ◽  
pp. 91-98 ◽  
Author(s):  
D. Jougnot ◽  
A. Revil

Abstract. The parameters used to describe the electrical conductivity of a porous material can be used to describe also its thermal conductivity. A new relationship is developed to connect the thermal conductivity of an unsaturated porous material to the thermal conductivity of the different phases of the composite, and two electrical parameters called the first and second Archie's exponents. A good agreement is obtained between the new model and thermal conductivity measurements performed using packs of glass beads and core samples of the Callovo-Oxfordian clay-rocks at different saturations of the water phase. We showed that the three model parameters optimised to fit the new model against experimental data (namely the thermal conductivity of the solid phase and the two Archie's exponents) are consistent with independent estimates. We also observed that the anisotropy of the effective thermal conductivity of the Callovo-Oxfordian clay-rock was mainly due to the anisotropy of the thermal conductivity of the solid phase.


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