Facetting during directional growth of oxides from the melt: coupling between thermal fields, kinetics and melt/crystal interface shapes
Introduction
It is well recognized that large-scale numerical analysis of transport-limited crystal growth is a useful tool for the understanding and improvement of melt growth techniques (see e.g. Refs. [1], [2], [3] and references within). Such analyses have been successfully used to complement and guide experimental studies of directional crystal growth. In particular, they can provide detail which is very difficult or even impossible to obtain from experiments. This approach has been successful in the investigation of a variety of phenomena occurring during growth, such as melt convection (e.g. Refs. [4], [5]), radiative heat transport (e.g. Refs. [6], [7], [8], [9]), solute segregation (e.g. Refs. [10], [11], [12], [13]), and more. However, facetting of the melt/crystal interface, often observed in experimental investigations of oxides (e.g. Refs. [14], [15], [16]) as well as other materials (e.g. semiconductors [17], [18], [19]), cannot be explained using models based on transport phenomena alone.
Facets appearing along the melt/crystal interface are associated with a local reduction of the interfacial temperature (undercooling) to values below the equilibrium melting point of the material grown. This local undercooling along the facets can theoretically be attributed to anisotropy in interfacial energy2 and/or anisotropy in the interfacial attachment kinetics. Experimental studies of directional melt growth of certain oxides [15], [16], [21] provide evidence that the evolution of facets along the melt/crystal interface during the directional growth of these materials is often a kinetic phenomenon. For example, in Ref. [15] the size of facets was shown to vary with crystal growth rate in a manner suggesting that the growth rate is proportional to the interfacial undercooling raised to the second power. This behavior is most probably a direct manifestation of interfacial growth kinetics. An alternative explanation, relating local changes in thermal fields (due to the dependence of latent heat release on growth rate) to variations in facet size, is compatible with interfacial energy driven facetting. However, this explanation is unlikely since detailed calculations [9] have shown latent heat effects to be negligible in small-diameter systems operated under conditions similar to those reported in Ref. [15]. Additional evidence supporting this line of reasoning is given in Section 4.4.
Theoretical studies of the relation between interfacial undercooling and growth velocity for both rough and flat faces are well documented in the literature (see e.g. Ref. [22] and references within). It has been recognized that rough surfaces grow at a rate proportional to the undercooling (i.e. yielding a kinetic coefficient independent of undercooling). Facetted interfaces, on the other hand, often grow at a rate dependent in a nonlinear manner on the local undercooling. Two classical mechanisms in this case are growth by screw dislocations, which is characterized by a dependence of growth rate on undercooling raised to the second power (Vn∝ΔT2),3 and two-dimensional nucleation-limited growth which requires relatively large undercoolings and is associated with an exponential growth rate dependence on undercooling (Vn∝exp(−A/ΔT)).
Studying coupled anisotropic kinetics and transport in a crystal growth system often requires the application of computational methods. There has been extensive work in this area with respect to the growth of small particles from a supersaturated solution/vapor or from a supercooled melt (see e.g. Refs. [23], [24], [25], [26]). Of special relevance to this work is a study by Yokoyama and Kuroda [23] who reproduced morphologies of snow crystals using a model for the anisotropic kinetics occurring during supersaturation-driven vapor growth. These authors used a nontrivial kinetic coefficient in their analysis, taking into account nonlinear kinetics on singular (facetted) surfaces while accounting for linear kinetics on nonfacetted surfaces. It is also worth noting the contribution of Yokoyama and Sekerka [25] who studied the anisotropic evolution of two-dimensional particles growing from their melt. They demonstrated how isotropic surface energy prevents the appearance of sharp corners along the melt/crystal interface.
Although the effect of kinetics on the growth of particles from supercooled melts has been addressed using computational analysis techniques, the application of these methods to the study of such effects in large-scale directional growth systems has been largely overlooked. Elementary geometric ideas relating facetting phenomena to kinetic undercooling, during the directional growth of single crystals from the melt, have been put forward in Refs. [27], [28]. Such ideas were later quantified into simple algebraic relations in Refs. [29], [30], [31]. These relations are, however, limited by the simplified assumptions on which they are based.
In this study we apply the Galerkin finite element method (GFEM) in an investigation of the effects of interface kinetics on the directional melt growth of oxide single crystals. As indicated above, existing computational studies of the growth of oxides via confined and meniscus-defined techniques (e.g. Refs. [7], [8], [9], [32], [33], [34]) put an emphasis on the better understanding of internal radiative heat transfer and melt convection. These analyses, however, include the assumption that the melt/crystal interface is at the material's melting point therefore ignoring facet formation during growth. In general, the existence of facets during growth may significantly modify temperature fields, melt flow, and solute segregation. In particular, the formation of facets in these materials may adversely affect crystalline quality. For example, in the case of garnets, nonequilibrium solute segregation along the facetted interface may lead to (unwanted) localized strained areas within the crystal [35], [36]. Note that the phenomenon of nonequilibrium segregation on facets, often termed “the facet effect”, has also been observed in nonoxide materials (see e.g. Ref. [37] and references within). It is also worth noting that facet formation along the melt/crystal interface during the growth of certain semiconductors is known to lead to unwanted twinning phenomenon (see e.g. Refs. [38], [39], [40], [41]).
This paper is organized as follows. In Section 2 the model is formulated, giving details of the transient analysis, quasi-steady state equations and model of interfacial kinetics. The numerical scheme is briefly presented in the next section (Section 3), followed by Section 4 which includes a summary of results and their discussion. Conclusions are given in Section 5.
Section snippets
Model formulation
We consider an idealized system for the growth of oxide slabs via the vertical gradient freeze (VGF) method. Using this technique, a slab-shaped molybdenum crucible, filled with starting material is placed in a vertical furnace whose temperature varies linearly between time-dependent hot-zone Tho(t) and cold-zone Tco(t) values; directional solidification is induced by slowly lowering Tho and Tco with time.
The mathematical representation of the physical domain and coordinate system we use is
Numerical technique
In this study we employ a numerical technique based on a standard Galerkin finite element method (GFEM) together, in the case of the transient calculations, with a backward Euler variable time-stepping technique; these methods are described in previous studies (e.g. Refs. [9], [46] and references within). For the sake of brevity we will briefly mention our approach, emphasizing the differences between our method and those we have previously employed. For a more detailed description of the
Results and discussion
New algorithms of the type developed here should always be tested by observing their ability to reproduce results available from the literature. In our case, we applied our technique to the anisotropic solidification problem presented in Ref. [25] as well as to the transient melting analysis discussed in Ref. [52]. Following the success of these tests (for details see Ref. [47]), the algorithm was applied to a realistic problem in which kinetics-driven facetting is expected.
We have investigated
Conclusions
The appearance of facets along the melt/crystal interface during the directional growth of single crystals from the melt is a scientifically and technologically important phenomenon. Unfortunately, until now this effect has been overlooked by researchers applying large-scale computational analyses to relevant systems. In this manuscript a method for the computational analysis of facetting is proposed, tested, and applied. The vertical gradient freeze growth of oxide slabs is chosen as a model
Acknowledgements
This Research was supported by The Technion V.P.R. Fund–Henri Gutwirth promotion of research fund and by The Israel Science Foundation administered by The Israel Academy of Sciences and Humanities. A.V. acknowledges partial support by the Israel Absorption Ministry. The authors would like to thank A.A. Chernov, J.J. Derby, R. Ghez and V.V. Voronkov for their very useful remarks.
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Current address: Department of Chemical Engineering, Tianjin University, Tianjin 300072, People's Republic of China.