Vertical geometry is simple: stack thousands of horizontal rings and fuse them into one solid. Each layer follows the same six-beat cycle:
- Degrain and feed. Sieved regolith (75-150 µm) flows to the sintering head.
- Deposit the bead. The head traces the wall contour, laying down a thin bead 20-40 mm wide.
- Laser sinter. The laser melts the bead - and the top of the layer beneath it.
- Fuse and cool. The melt pool penetrates 1-3 mm into the previous layer, fusing the interface. Cooling in vacuum is mainly radiative.
- Index up. The head rises 5-15 mm to the next layer height.
- Repeat. Thousands of layers become a monolithic wall - not stacked bricks, but one continuous fused structure.
That interlayer remelt in step 4 is the entire ballgame. A wall is only as strong as its weakest interface, and controlled remelt depth is what makes a stack of layers behave as a single solid.
Closed-loop control runs the whole cycle. Sensors read the melt pool in real time and continuously adjust laser power, traverse speed, and remelt depth to the material actually in front of the beam - because regolith varies by region, by depth, by scoop, and open-loop systems fail when the feedstock changes. The system sinters the regolith it has, not the regolith a model assumed. In-process sensing doubles as quality assurance: dimensional accuracy is verified as the wall grows, not inspected after the fact.
Why vertical is easy - and overhangs are harder. A vertical wall is self-supporting: every layer sits fully on the one below. Overhangs and domes require corbeling - stepping each layer inward - and in lunar conditions the self-support angle is roughly
50-60°. This is why our structures favor vertical shells, buttressed footings, and sintered caps: geometry chosen to work with the physics, not against it.