Behavior of Ice During Pulsed NIR Laser Cutting

Institutions
University of Minnesota
Climate Change Institute - University of Maine
Related Projects

Ice
RELIC

Hello, and thanks for viewing our poster from WAIS Workshop 2022 (but it’s also all good if you didn’t!) This page holds videos, extra images, and other good stuff that we couldn’t put on a poster.

Poster

Click here for your very own copy of the poster! (In screen-resolution PDF form. Sorry, we sold out of the T-shirts already.)

The basics: CW cuts

When we first got our 1 kW laser source last year, pulsed operation took a little bit of setup—it requires a proprietary piece of software with no API, so we eventually had to reverse-engineere its communication protocol to integrate it into our experiments—so our early cutting experiments were done with continuous-wave beams.

We use cheap webcams with laser-reflecting filters for monitoring experiments, and also for trying to get interesting—if risky—angles. Bonus: this sensor sees the near-infrared laser as a purplish light. Here, a rectangular rod of tap-water ice, about 1 inch on each side, is moved downward at 2.5 mm/sec through a 550 W beam of 1.07 μm CW laser light. The ice starts out somewhere north of -20 °C and is experimented on in room temperature, which doesn’t help limit the rate of meltwater production.
A webcam shot from the other side of the sample, looking (almost) back into the laser.
One more webcam shot, this time looking downward from the top of the vertical motion stage that moves the ice sample downward to cross the cutting beam.

Pulsed drilling

Moving the laser beam around on an ice sample (or vice versa) makes it a little challenging to closely examine how the two are interacting: cameras have to follow a moving target, features like bubbles in the ice can affect the interactions, analysis gets confused by all the moving things… better to just hold everything steady.

A series of 3 ms, 500 W laser pulses impingent (from the upper left of the image) at a static point on a sidelit clear ice stick, as viewed from above.
Two flavors of analysis on the video above. The first displays the cumulative difference between each frame and the very first, highlighting the trajectory of the hole; the second plots the progress of the laser-ice interaction front.

Pulsed cutting

Drilling holes is great for measuring laser mechanics—but it does have some vital differences from cutting slots, such as greatly increased capillary forces preventing meltwater from escaping the hole. Some behaviors therefore require a moving beam to read.

CW cutting can quickly carve through a large amount of ice, but it does so by dumping in energy, resulting in quite a lot of heating to the ice (and once that disappears, to the beam stop behind it.)
One positive: it does slice through two inches of ice cube in one go.
Coming down to 5 ms pulses, applied at 10 ms, greatly reduces the heating of the ice cube…
…even if we cut less far per pass. However, most scientists would probably prefer this neat slot about 1 mm wide to the CW cut’s inverted-V-shaped groove over 1 cm across, even if excising the sample does take a bit longer!

Sampling wedges

We’ve found that some people find the wedge cutting a little hard to picture, so we took a few days for a fun diversion from our actual experiments. Bolting a rotation stage and linear stage together gives us a motion system that can carve a wedge out of a short 3" diameter tap-water ice core with a wide CW beam. Video is 15x actual speed, because the built-in-a-day rig is a bit wobbly.
All work and no play makes Jack a dull motion rig, so here’s the same setup carving a UMN logo. Video is 10x actual speed.

Other things going on: LN2, ice, and acoustic sensors

We strongly suspect that vibration-free laser cutting will have a massive advantage over mechanical saws in treating brittle ice samples, but testing this in the lab is a challenge since ice from the brittle zones has, by definition, a tendency to fracture or shatter during retrieval, and thus intact samples are fairly rare. An obvious alternative: make some tap-water ice brittle. While we are also investigating more complex options to emulate the internal forces in natural brittle ice, applying an extreme temperature gradient by chilling the center of an artificial core with liquid nitrogen seems to very effectively create fractures.

The laser!

Lots of people wonder what a 1 kW laser looks like. While ours has a disappointing lack of very mad-science flair, its standard 4U computer server form factor is encouragingly portable. The optical delivery fiber emerges from the rear, and the bigger thing at the bottom of the rack is a water-cooling unit.

3D printed parts

Some of our rapidly-proliferating lab mechanisms, designed and 3D-printed in-house at UMN.

You might have noticed a number of plastic parts holding our samples, mounting our cameras, getting frozen into our tap-water cores… You get the drift. We design and produce these parts in-house with the facilities and staff of UMN’s Anderson Innovation Labs, and if any of them look like they might meet your needs, then our parts are your parts! We’re uploading any designs we think might be useful to YouMagine, a site for open-source 3D print designs; however, we’re more often than not pretty behind on uploads, so please don’t hesitate to ask!


Other Research

Laser Damage

Optical Materials and Laser Damage

Infrared

Spectrally-Selective Uncooled Infrared Bolometers

Ice

Optical Characterization of Glacial Ice

Thermoluminescence

Thermoluminescent Extreme-Environment Temperature Sensors

Quantum Tuning

Tuning the Semiconductor Bandgap: Nanomechanical Control of Electron States

About (TL;DR)

We are the ECE research group of Professor Joey Talghader at the University of Minnesota.

Keep In Touch

About This Site

Designed by Merlin Mah, with a little help.
Runs on Jekyll.