Directional solidification: watch the freezing front pass four sensors
A quartz cuvette of liquid DMSO translates from a hot zone to a cold zone at 5 µm/s. The solid–liquid interface (SLI, the 18.5 °C isotherm) sweeps the bore and crosses the four centerline sheathed thermocouples in succession — each sensor traces the classic S-curve as the gradient zone passes over it. A fifth trace follows a bare, uninstrumented melt node so you can see the natural DMSO response undistorted by sensor hardware. Every frame is output of the refined, breadboard-matched NovaThermal solve (0.1 mm quartz-wall mesh), not an illustration.
Edit the geometry
These fields map 1:1 to the solver template. Changing them redraws the drawing so you can stage your own case; the animation above stays the solved reference case. Run your edited case in the console →
What the model showed
A thermocouple is a thermal short
A 0.25 mm sheathed probe (effective axial k ≈ 14.9 W/m·K vs DMSO’s 0.25) shifts the front about 0.5–0.7 mm. The sign depends on which zone the sheath bridges.
Symmetry governs front shape
Equal-length probes (center or corners) keep the front flat. A rake of differing lengths tilts it — warp peaks near 0.9 mm as the SLI sweeps the tip span.
Steady == transient to ~1%
At 5 µm/s the Péclet number is tiny: the conduction field is quasi-static and the isotherm lands mid gradient-gap at the measured 1.5–2.1 K/mm.
Explore next: see the microstructure this front leaves behind in the 3D lamellar-growth viewer (sweep the transverse and axial cross-sections), or read how the number is proven — mesh-independence gating, the mushy-zone enthalpy method, and result provenance.