کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
1790991 1524457 2013 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Non-isothermal model experiments and numerical simulations for directional solidification of multicrystalline silicon in a traveling magnetic field
موضوعات مرتبط
مهندسی و علوم پایه فیزیک و نجوم فیزیک ماده چگال
پیش نمایش صفحه اول مقاله
Non-isothermal model experiments and numerical simulations for directional solidification of multicrystalline silicon in a traveling magnetic field
چکیده انگلیسی

A new experimental setup containing a GaInSn melt with a square horizontal cross section of 10×10 cm2 and a variable melt height up to 10 cm has been developed. The melt is positioned in the center of a coil system generating a traveling magnetic field (TMF). Using a cooling system at the bottom and a heating system at the top of the melt, a vertical temperature difference up to approximately 50 K can be applied to the melt, imitating the thermal conditions during the directional solidification of multicrystalline silicon. Direct measurements of the time-dependent velocity and the temperature profiles were performed using ultrasonic Doppler velocimetry and thermocouples, respectively. Complementary three-dimensional (3D) numerical simulations of the model experiments were used to validate the numerical tools and to gain a deeper insight into the characteristics of TMF flows in square melts. The classical toroidal flow structure known from isothermal cylindrical melts is shown to obtain a large horizontal central vortex at a small height of the square melt, whereas a distinct 3D asymmetry appears at a large height. A vertical temperature gradient tends to suppress the vertical melt motion and leads to new complex horizontal flow structures.


► We study flows in a square GaInSn model melt numerically and experimentally.
► The 3D flow structure in a traveling magnetic field changes significantly with the melt height.
► An asymmetric 3D torus is observed if the melt's height-to-width ratio exceeds unity.
► A vertical temperature gradient causes a critical transition to several horizontal vortices.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Crystal Growth - Volume 372, 1 June 2013, Pages 145–156
نویسندگان
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