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The three-dimensional starting solution for a melting slab
Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences, 1971Abstract A short-time closed-form solution is developed for the melting or solidification of a halfspace under a general surface heat input, such that change of phase starts at a point of the surface, and then spreads simultaneously both towards the interior of the body and along its surface. The solution is obtained by the embedding
B. A. Boley, H. P. Yagoda
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Heat Conduction in a Melting Slab
Journal of the Aerospace Sciences, 1960The behavior, after the initiation of melting, of a slab insulated on one side and subjected to a heat input varying arbitrarily with time on the other is studied. A method of successive approximations is developed which requires the solution of an ordinary nonlinear differential equation; this equation is readily solved numerically on a desk ...
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The low-melting phosphate glass was prepared for production of glass binders for protective coating of steel slab. Effects of different O/P ratios on glass structures and properties were analyzed.
Xiaomeng Zhang +2 more
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TTGs and adakites: are they both slab melts?
Lithos, 2005Abstract Although both high-Al TTG (tonalite–trondhjemite–granodiorite) and adakite show strongly fractionated REE and incompatible element patterns, TTGs have lower Sr, Mg, Ni, Cr, and Nb/Ta than most adakites. These compositional differences cannot be easily related by shallow fractional crystallization. While adakites are probably slab melts, TTGs
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Formation and melting of a vertical ice slab in an enclosure
International Communications in Heat and Mass Transfer, 1987Abstract An experimental study was conducted on the formation and melting of a vertical ice slab subjected to uniform heat flux boundary conditions. The rectangular testing section was heated from one side by an electric heater and cooled from the opposing one by a refrigerant system.
M.M. Sorour +3 more
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Total Melting Time in the Ablating Slab Problem
Journal of Applied Physics, 1971An exact melt-through time is derived for the one-dimensional heated slab problem when the melted material is immediately removed. The result is derived via two different approaches and is shown to be independent of the transport properties of the material.
J. E. Rogerson, G. A. Chayt
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, 2014
As an important part of the Central Asian Orogenic Belt (CAOB), the Altay Range contains large-scale Paleozoic magmatic rocks. However, owing to the lack of precise age constraints, the tectonic setting and petrogenesis of the magmatic rocks in this area
Xiaoming Shen +4 more
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As an important part of the Central Asian Orogenic Belt (CAOB), the Altay Range contains large-scale Paleozoic magmatic rocks. However, owing to the lack of precise age constraints, the tectonic setting and petrogenesis of the magmatic rocks in this area
Xiaoming Shen +4 more
semanticscholar +1 more source
ON THE CONDUCTION OF HEAT IN A MELTING SLAB
1961Abstract : A new method for the solution of the problem of heat conduction in a melting slab, where the molten material is immediately removed upon formation, is presented. No restrictions are placed on the boundary conditions which may be imposed on the slab and the material properties are allowed to be temperature dependent.
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UPPER AND LOWER BOUNDS IN PROBLEMS OF MELTING OR SOLIDIFYING SLABS
The Quarterly Journal of Mechanics and Applied Mathematics, 1964Abstract : The problem studied is that of a slab, heated in an arbitrary manner on one face and insulated on the other, which melts (or solidifies), the material being allowed to remain stationary after change of phase. Variable material properties are taken into account.
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