Research
NASA’s space mission to the asteroid Psyche—located in the asteroid belt between Mars and Jupiter—will help us better understand our own Earth. DTU supplies instruments that can measure and map the asteroid’s magnetic field.
The magnetometer is astonishingly small compared to its performance and capacity. The size of a tennis ball, the sensor is placed in a cylinder and with a pineapple-like surface. The grooves on the surface hold coils that generate a magnetic field similar to what you want to measure. The spacecraft itself is taller than a human and weighs just under two tonnes without fuel and just under three with fuel, so the weight of the magnetometer, which is about 2 kg, is not much in comparison. But it is efficient and reliable, developed and built manually at DTU with a focus on every little detail.
We know absolutely nothing about Psyche's magnetic field—whether it is large or small; whether it is a single large field or a scattering of smaller fields. The magnetometer must be prepared for all eventualities.
DTU’s magnetometer is unique in being able to measure the size and direction of magnetic fields with extreme precision. The strength of magnetic fields is usually measured in tesla. For very weak magnetic fields, measurements are stated in nanotesla (nano = 10-9). The Earth’s magnetic field measured in Denmark is approximately 54,000 nanotesla.
The magnetometer from DTU is capable of detecting extremely weak magnetic fields measuring down to just 0.025 nanotesla as well as extremely strong fields measuring up to 80,000 nanotesla. This means that the weakest magnetic field measurable by the instrument is six million times less powerful than the strongest field it can measure. In other words: The instrument can detect magnetic fields ranging from the weak fields of solar wind to the stronger magnetic fields of large planets.
The spacecraft will be carrying two magnetometers to secure data if something should happen to one of them. But there is also another reason:
“The spaceship itself can generate a magnetic field, and we don’t want that to be included in our data. Therefore, the instruments will be installed on a boom some distance from the spacecraft, and with two sensors we will be able to detect signals from the spacecraft, which can then be deducted. If the two sensors produce the same measurements, we can safely assume that what they are measuring is the natural magnetic field. If they produce different measurements, we can assume that this is down to the spaceship,” explains José Merayo.
José Merayo’s research group at DTU Space has built magnetometers for several missions that have measured the Earth’s magnetic field. Initially for the Ørsted satellite, then for the German CHAMP mission, and finally for the European Space Agency’s SWARM mission.
“All in all, our magnetometer has been in operation in space for a combined more than 155 years and has provided measurements for the geomagnetic field maps used for navigation and in the event of GPS crashing,” says José Merayo.
The magnetometers on the Psyche mission will be powered by the solar panels installed on the sides of the spacecraft and will start measuring immediately after launch. Of course, the instrument has undergone all manner of pre-launch testing, but we will need to check that everything works as expected, or whether something needs adjusting once it is actually in space.
Psyche is located in the asteroid belt between Mars and Jupiter, and on the 500 million km journey it may also be possible to obtain data about Mars’ surroundings as the spacecraft will be flying close to the planet; also, it will probably be possible to gain new knowledge about solar storms and their impact on the solar system. For this reason, the instrument will be operating throughout the voyage even though it could be turned on and off.
In six years’ time, the mission will hopefully reach the metal-rich asteroid, and the plan is then for the spacecraft to orbit the asteroid at altitudes of approximately 700, 500, 300 and 100 km for a combined period of more than two years.
This will generate lots of new data and hopefully increase our understanding of the creation of our solar system and of planetary magnetic fields.
“Why do some planets, such as Venus, have no magnetic field, while the magnetic fields of other planets, such as Jupiter, are stronger even that the magnetic field on Earth? In Psyche, we have a stripped-bare core that we can measure directly. We believe that will tell us a lot. By learning more about Psyche’s magnetic field, we can also learn more about the workings of Earth’s magnetic field. The solar system is huge, and any data we can gather will help us understand it better—for example, how the weather in space helps protect our Earth,” says José Merayo.
There are no plans to bring the spacecraft back to Earth at the end of the mission. “Maybe it will land on Psyche, who knows? Or it will carry on orbiting the asteroid as a small artificial moon, says José Merayo.
Facts
Asteroids are celestial bodies that are too small to be classified as planets. Most asteroids orbit the Sun in the asteroid belt between Mars and Jupiter. Although there are millions of asteroids in this belt, their combined volume is smaller than that of the Moon.
Source: vildmedrummet.dk (website in Danish only)
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Find more information about the Psyche mission at psyche.asu.edu.
José M. G. Merayo Professor Phone: +45 45253452 jmgm@dtu.dk