The electronics workshop at the USGS Hawaiian Volcano Observatory buzzes with creative activity. It’s like Santa Claus’ workshop — for volcano science. Workbenches line the walls of the room, cluttered with things in the making: pliers, wires, and bottles of glue; voltmeters, calipers and microchips, too.
At one bench, a worker is hunkered, soldering a rainbow splay of wires into a cable harness. Nearby, another fine-tunes a glowing waveform on an oscilloscope. Across the room, another hurriedly puts the finishing touches on a volcano-proof camera — one of the latest models.
The electronics shop is well-lit, ventilated, and fully networked. There’s constant motion — people and equipment flow through doors on each end. A small radio plays ‘Jingle Bells,’ while someone runs a shop vacuum.
Here, technical problems are wrestled, new ideas are developed, and informal education is shared.
When the workday is done, the staff closes up, and the room grows quiet — almost. At one end of the darkened shop, there is a restless stirring: a 3D printer zigzags rhythmically on its midnight program. It’s building carbon fiber drone parts, destined to fly over Kilauea to measure volcanic gas emissions that cause volcanic air pollution (vog) downwind.
Over the past five years, HVO’s use of 3D printing has grown. It has evolved into a technique that enables custom production and high-performance innovation.
This technique has allowed HVO to realize several advantages of digital fabrication: shortened supply chains, nimble design iterations, and on-demand production.
A new idea moves forward in the design process using computer aided drafting software. A 3D CAD model is created using engineering, drafting, and design proficiencies. The 3D model is readily tweaked, shared, and documented as part of the digital workflow.
Slicing software is used to convert a 3D model into a sequence of thin, stacked layers for 3D printing. Algorithms are used to tweak many 3D printing parameters — to optimize infill density, strength to weight, cost, and printing time.
Parts are constructed in 3D printing by depositing layer after layer of material. This type of additive manufacturing opens many design possibilities, such as low-density infill, embedded hardware, and composite reinforcement.
HVO uses two 3D printing techniques depending on the part being constructed, what it will be made of, and how it will be used.
The fused filament fabrication process is used to 3D print parts from starch-based bioplastic. Applications have included terrain models, petrology sample holders, templates, and mounting brackets.
With the FFF technique, the 3D printer uses an extrusion nozzle on a travelling print head. Plastic filament is melted and deposited in a small bead as the print head traverses a flat plane. As the extruded material cools and solidifies, the print head rises and deposits the next layer.
To make functional parts that meet higher performance demands, HVO uses a more advanced 3D printing process: continuous fiber fabrication. Advanced composite materials — carbon fiber, Kevlar, fiberglass, and nylon — are used to achieve higher strength, durability, and dimensional tolerances.
With the CFF technique, a second printhead nozzle weaves long strands of carbon fiber into layers of extruded nylon. The reinforced composite parts can achieve strength comparable to solid aluminum, at a fraction of the weight.
Many new designs have been enabled by CFF: from airborne drone payloads, where strength-to-weight ratio is a primary consideration; to submerged crater lake instruments, where heat- and chemical-resistance are crucial.
These techniques have been used to make more than 430 unique designs at HVO over the past 5 years! Multiple versions, customization, and testing are enabled by this design/production cycle. Small quantities of each design — from one to ten parts — are efficiently printed in-house. Larger quantities are scaled-up using commercial services.
Recently, HVO has explored 3D printed metal parts. Metal powder is used as the raw material in selective laser melting. HVO has tested aluminum alloy printed parts as an alternative to traditional machining.
Like elves in Santa’s workshop, HVO technicians practice their art; they fuse software and filament to print a new part. An invention is born of necessity. At HVO, the mother of all necessity is monitoring Hawaii’s six active volcanoes.
Volcano
activity updates
Kilauea volcano is erupting. Its USGS Volcano Alert level is at WATCH (https://www.usgs.gov/natural-hazards/volcano-hazards/about-alert-levels). Kilauea updates are issued daily.
Lava continues to erupt from a single vent in the western wall of Halema‘uma‘u crater. All lava activity is confined within Halema‘uma‘u crater in Hawaii Volcanoes National Park. Sulfur dioxide emission rates remain elevated and were measured at approximately 1,200 tonnes per day on Nov. 29. Seismicity is elevated but stable, with few earthquakes and ongoing volcanic tremor. Summit tiltmeter data has shown brief inflationary and deflationary signals over the past week. For more information on the current eruption of Kilauea, see Recent Eruption (usgs.gov).
Mauna Loa is not erupting and remains at Volcano Alert Level ADVISORY. This alert level does not mean that an eruption is imminent or that progression to an eruption from the current level of unrest is certain. Mauna Loa updates are issued weekly.
This past week, about 42 small-magnitude earthquakes were recorded below the summit and upper elevation flanks of Mauna Loa — the majority of these occurred at shallow depths less than 10 kilometers (6 miles). Global Positioning System measurements show no major deformation over the past week. Gas concentrations and fumarole temperatures at both the summit and at Sulphur Cone on the Southwest Rift Zone remain stable. Webcams show no changes to the landscape. For more information on current monitoring of Mauna Loa, see: https://www.usgs.gov/volcanoes/mauna-loa/monitoring.
There were 3 events with 3 or more felt reports in the Hawaiian Islands during the past week: a M3.5 earthquake 4 km (2 mi) S of Pahala at 32 km (20 mi) depth on Dec. 8 at 8:38 a.m. HST, a M3.5 earthquake 3 km (1 mi) S of Pahala at 36 km (22 mi) depth on Dec. 4 at 8:43 p.m. HST, and a M3.1 earthquake 7 km (4 mi) E of Pahala at 33 km (21 mi) depth on Dec. 3 at 5:02 p.m. HST.
HVO continues to closely monitor Kilauea’s ongoing eruption and Mauna Loa for any signs of increased activity.
Please visit HVO’s website for past Volcano Watch articles, Kilauea and Mauna Loa updates, volcano photos, maps, recent earthquake info, and more. Email questions to askHVO@usgs.gov.
Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.
