The propagation of a molten blob of aluminium at melting point were then simulated using both codes.
In practice, after a set time the voltage is disconnected, the heating ceases and the molten zone solidifies.
The molten aluminium cools to its melting temperature as the simulation progresses and solidification is more rapid.
The sensible heat in the molten drop is essential if a significant proportion of the liquid can escape from the drilled hole.
Sequential additions (b, c) to the shallow magma chamber lead to a larger and increasingly molten body of magma.
The molten zone acts as an electrical conductor with normal conductivity and heat is generated throughout its volume.
The polymerization reaction occurred by taking advantage of the high polarity of molten urea as well as its dehydrating ability.
We discuss the conditions for a physically meaningful solution to exist, a solution with a nonempty molten zone.
