SANDIA GEOPHYSICISTS Danny Bowman and Sarah Albert, display an infrasound sensor and the Styrofoam box used to protect the sensors from the extreme temperatures experienced by their balloons. Sarah has found testing balloon-borne infrasound sensor arrays really exciting. “It’s one of those projects that you imagine scientists do when you’re a child.”
New Sandia balloon-borne infrasound sensor array detects explosions
Sheets of plastic similar to that used for garbage bags, packing tape, some string, a little charcoal dust, and a white shoebox-sized box are more than odds and ends. These are the supplies Danny Bowman, a Sandia National Laboratories geophysicist, needs to build a solar-powered hot air balloon for detecting infrasound.
Infrasound is sound of very low frequencies, below 20 hertz, which is lower than humans can hear. African elephants produce infrasound for long-distance communication at around 15 hertz. For comparison, a bumblebee’s buzz is typically 150 hertz and humans hear in the range of 20 to 20,000 hertz.
Last July, a fleet of five solar-powered balloons reached a height of 13 to 15 miles, twice as high as commercial jets, and detected the infrasound from a test explosion. This experiment was funded by Sandia’s Laboratory Directed Research and Development program. Danny presented the results at the American Geophysical Union conference in December. The results will be published soon.
Infrasound is important because it’s one of the verification technologies that the US and the international community use to monitor explosions, including those caused by nuclear tests. Traditionally, infrasound is detected by ground-based sensor arrays, which don’t cover the open ocean and can be muddled by other noises, such as the wind. Danny says air conditioners are also a common source of infrasound noise.
“The stratosphere is much less noisy so you can detect events of interest to science and national security from greater distances,” Danny says. The stratosphere is the atmospheric layer from about 5 miles to 31 miles above the ground.
Inexpensive hot air balloons fly all day
The solar-powered hot air balloons take three hours for Danny and fellow geophysicist Sarah Albert to make and use about $50 worth of materials, not including the reusable infrasound sensor or GPS tracker. The charcoal dust helps heat up the air inside the balloon, providing lift without requiring helium gas, a nonrenewable resource.
The balloons can even be launched on partly cloudy days, Sarah says. They stay up in the stratosphere all day and come down after the sun sets. This “guaranteed termination mechanism” is both a pro and con, Danny says.
It’s a fool-proof way to bring down the balloons, the sensors, and the data they have collected. On the other hand, longer flights would be useful. During the Arctic summer, the balloons could fly for weeks, but the team is also working on balloons that can keep flying at night.
For future experiments, Danny is interested in a balloon design with an insulator on the top surface of the balloon and absorber on the bottom, so it absorbs heat from the Earth to allow it to keep flying at night.
Multiple sensors determine location
The most important aspect of this experiment is that the five balloons formed a 3-D array of sensors, Sarah says. One sensor can hear a sound, but cannot provide any location information. Sarah says, “My mom is deaf in one ear so it’s hard for her to tell where a sound is coming from.” Having two ears allows animals to determine the source of a sound.
Five microphones in an array, as in this experiment or ground-based sensor arrays, provide the same information — the direction the sound wave is coming from. Researchers coordinate the information from multiple arrays to triangulate the source of the sound.
Calculating where the sound wave is coming from can be a challenge when each sensor in the array is moving relative to each other and the source, admits Danny. A lot of computational algorithms assume stationary sensors, so the team needed to adapt them to include GPS information.
Future use in treaty monitoring and solar system exploration
Danny has proposed flying balloon-borne infrasound sensors as a part of the next series of the NNSA’s Source Physics Experiment project. This project develops new and improved, physics-based approaches for monitoring underground nuclear explosions.
In addition to potential treaty monitoring and national security uses, Danny and Sarah hope to fly hot air balloons in non-terrestrial experiments.
Danny is assisting a NASA Jet Propulsion Laboratory project to explore the possibility of using balloon-borne infrasound sensors on Venus to listen for Venus-quakes. Venus is similar to Earth in mass, but is geologically very different with no apparent plate tectonics.
Another possibility the team is exploring is flying infrasound sensors on Jupiter. Jupiter is a gas giant with open scientific questions about its internal structure and geology that infrasound could help answer. “We’re still decades out from an actual mission,” Danny says, “but I’m excited to see how far it will go.”
The results from his prior research test flying individual infrasound sensors on balloons was published in Geophysical Research Letters, and more recently in Journal of Geophysical Research: Atmospheres.
Danny says, “This is a really exciting new area of research. Balloon-borne infrasound sensors will never replace ground-based acoustic arrays, but I think it can augment them. And the most exciting thing is flying in the atmospheres of other planets and what we can learning from them."