Making High Fidelity Fluxgate Cores for Space Science and Space Weather Missions

A NASA-sponsored team at the University of Iowa (UI) is restoring and advancing the nation’s capability to make high-fidelity magnetic field measurements needed to investigate space weather that can impact our communication and power grids on Earth and our assets in space.

Fluxgate magnetometers are widely-used space science and space weather instruments, but they depend on a legacy component—a ferromagnetic core—that was developed and manufactured for the U.S. Navy using technology that has been subsequently lost to the civilian community.

The UI team manufactures new fluxgate cores using a method that does not rely on legacy processes or materials and then integrates these cores into modern spaceflight magnetometers. The ferromagnetic cores are produced starting from base metal powders that are melted into custom alloys, rolled into thin foils, formed into the desired geometry of the fluxgate core, and artificially aged using heat to optimize their magnetic properties. The resulting cores are integrated into a complete fluxgate sensor ready for spaceflight applications.

Designing, prototyping, and manufacturing the cores, sensors, and paired electronics in house allows the team to explore new sensor geometries that are compatible with different missions. Most recently, the UI team developed a new core to be used in the Space Weather Iowa Magnetometer (SWIM). While the SWIM core is based on a core previously developed for the MAGnetometers for Innovation and Capability (MAGIC) Tesseract sensor that recently launched on NASA’s TRACERS (Tandem Reconnection and Cusp Electrodynamics Reconnaissance Satellites) mission the SWIM core is miniaturized and retains the same level of performance. The first flight opportunity for the SWIM fluxgate is on the University of Oslo’s ICI-5bis sounding rocket mission that is scheduled to launch in winter 2025/2026 from the Andoya Space Sub-Orbital range in Norway.

Fluxgate magnetometers sense the magnetic field by detecting the electromagnetic force (EMF) induced by the changing magnetic flux. Current is driven into the drive winding (the interior winding on the fluxgate core) creating a magnetic field. When the ferromagnetic material in the cores experiences the magnetic field, its relative permeability (the intrinsic magnetic property of the metal within the core) changes. As the relative permeability changes, a voltage is induced in the sense winding (the outer winding on the core). By knowing the amount of current driven into the core and the voltage that was induced in the sense winding, we can understand the magnetic field that the sensor is experiencing. Most in-space magnetometers are not located onboard the main body of the spacecraft; instead, they are placed on booms to ensure that the magnetic fields produced by the electronics and magnetic materials onboard the spacecraft do not interfere with the sensor.

The manufacturing process for these new cores is now well documented and ~90% of the cores produced have a noise floor that is comparable or better than previous legacy cores. Consequently, UI can reliably mass-produce cores for the SWIM payload and potential future follow-on missions. 

The new SWIM magnetometer design reflects three significant changes compared to the previous MAGIC instrument. The sensor has been simplified and shrunk. Its power consumption has been reduced without sacrificing measurement performance. Both these changes aid its accommodation on a magnetometer boom. In addition, the topology of the paired electronics in each magnetometer channel has been redesigned, which allows use of lower-performance parts that tolerate a higher radiation exposure.

Reduced Sensor size: The compact SWIM design reduces the sensor size by ~30% compared to the MAGIC sensor, with further reduction to the sensor mass likely as the mechanical design is optimized. The MAGIC Tesseract design used six cores whereas the SWIM sensor utilizes three smaller cores of the same geometry. Mass is a major performance driver for deployable boom design and vehicle dynamics. The SWIM sensor can also be manufactured with a lightweight carbon-composite cover (or the cover can be omitted) to achieve a sensor mass of ~110 g, which would enable the sensor to be easily accommodated on small satellite booms.

Reduced Power consumption: Using three smaller cores with improved metallurgy instead of six large racetrack cores reduced the power consumption of the SWIM sensor by a factor of two compared to the MAGIC sensor. Although this power reduction is modest compared to the total consumption of the instrument, it positively impacts the capability for boom deployment. Significant reduction in heat dissipation at the sensor minimizes the spot-heating of the deployable boom and reduces thermal gradients that can drive boom deformation/rotation, which impacts the pointing knowledge at the sensor. These improvements to the sensor have been achieved without impacting the measurement fidelity. In fact, prototype miniaturized SWIM race-track cores are outperforming the previous MAGIC cores due to their improved metallurgy.

Updated Electronics Topology: The MAGIC electronics use a traditional analog demodulator fluxgate and magnetic feedback design. This design requires high-performance components to be able to resolve small variations in large ambient magnetic fields. There are radiation limitations to these high-performance components making it difficult for the MAGIC design to operate in a high-radiation environment. To mitigate these issues, the SWIM design employs digital demodulation instead of analog demodulation and provides magnetic feedback via temperature-compensated, digital, pulse-width-modulation. This update to the electronics enables SWIM to potentially be used in long-duration and/or high-reliability operational applications such as radiation belt missions or planetary missions with long cruise phases.

The SWIM fluxgate design allows for more future applications in a variety of environments without sacrificing the performance seen on the MAGIC sensors. The UI team is looking forward to multiple upcoming flight opportunities for SWIM, including on the Observing Cusp High-altitude Reconnection and Electrodynamics (OCHRE) and ICI5bis sounding rockets.

Project Lead(s): Dr. David Miles, University of Iowa

Sponsoring Organization(s): Heliophysics Strategic Technology Office (HESTO)

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Curiosity Blog, Sols 4668-4674: Winding Our Way Along

Written by Alex Innanen, Atmospheric Scientist at York University

Earth planning date: Friday, Sept. 26, 2025

We are continuing through the boxwork region, taking a twisty-turny path along the ridges (many of which are conveniently Curiosity-sized). One thing we’re keeping an eye out for is our next drill location in one of the hollows. Our most recent drive put us right in the middle of two such hollows, which we’ve named “Laguna Escondida,” and “Laguna Socompa.” As we’re keeping an eye out for a good spot to drill though, we’re still using our normal suite of instruments to continue our investigation of the boxwork structures. 

This week, we’ve had six contact science targets along the tops of the ridges, which have given MAHLI and APXS plenty to do. ChemCam and Mastcam have also been keeping busy, with several LIBS measurements from ChemCam and mosaics from both, of targets near and far. We’re not only interested in imaging the hollows to scope out our next drill site but also in continuing to investigate the structure of the ridges, and look further afield at the more distant boxwork structures and buttes around us.  

On Monday, I was on shift as the science theme lead for the environmental science theme group (ENV). We’re coming up to the end of the cloudy season in just over a week. As a result, we’ve been making the most of the clouds while they’re still here with our suite of cloud movies — the shorter suprahorizon and zenith movies, which we use to look at clouds’ properties directly overhead and just over the horizon; a survey to see how the brightness of the sky and clouds change with direction, which consists of nine cloud movies all around the rover; and the cloud altitude observation, which uses shadows cast by clouds to, as its name suggests, infer the height of the clouds. Once the cloudy season is over the number of water-ice clouds we see above Gale crater decreases dramatically, so we shelve the two longer observations for another year and just use the zenith and suprahorizon movies to monitor cloud activity. 

The end of the cloudy season does bring about the start of the dusty season though, where more dust gets lifted into the atmosphere and the lovely view of the crater rim that we’ve been enjoying gets a bit hazier. We monitor this with our regular line-of-sight and tau observations. We also tend to see more dust-lifting activity, like dust devils, which we keep an eye on with 360-degree surveys and dedicated movies. With the ever-changing atmosphere, there’s always something for ENV to do. 

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New File Download Process for PSI Large Requests

A recent update to the PSI database improves how large dataset downloads are handled, resulting in more efficient processing for users.

Download requests larger than 1GB are now delivered via email, rather than downloading directly from the website. This allows the system to prepare your files in the background so you can continue working without delays, accessing the files at your convenience once your request is processed.

Why The Change?

This update improves user experience by:

• Reducing system lag and download interruptions.
• Allowing you to stay productive while files are processed in the background.
• Increasing reliability of large downloads.
• Delivering files in manageable parts, making them easier to handle and extract.

How Does it Work?

To download files larger than 1GB:

1. Users select 2 or more desired files and click “Download Zip.”

2. In the Prepared Large Download section:

• Enter the email address where the download access links should be sent.

• Check the box to confirm: “I understand large downloads are delivered in multiple parts via email.”

• Click “Send me the links.”

3. Users will receive an email confirming the download request has been submitted.

4. Once the files are ready, users receive a second email with link(s) to access the download. NOTE: Download links are valid for 7 days from the time you receive the email. Be sure to save the requested files before the links expire.

Best Practices

To ensure a smooth and efficient download experience, especially when working with large datasets, follow these best practices to help reduce processing time, prevent errors, and simplify file handling.

• Download only what you need: Smaller requests are processed faster.
• Split very large requests: If possible, divide and submit large requests into smaller sets to speed up processing.
• Avoid simultaneous large requests: Submit one large download at a time for smoother performance.
• Before extracting, save all ZIP parts to the same folder: This ensures proper extraction of multi-part downloads.
• Download promptly: Remember, download links will expire. Save your files while the link is active.
• Use a reliable email address: Double-check for typos and check your spam/junk folder if you don’t receive the emails.

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Joe A. Adam Presents Ring Sheared Drop (RSD) Research at 2025 ISSRDC

At the virtual 2025 ISS Research and Development Conference (ISSDRC), Joe A. Adam of Rensselaer Polytechnic Institute, presented the topic titled “Surface Science in Microgravity – Fluid Geometry in the Ring-Sheared Drop,” presented to a broad audience from academia and the scientific community during the Physical Sciences and Materials Development session.

Dr. Adam provided a comprehensive overview of the Ring Sheared Drop (RSD) hardware, experiment campaigns and the evolving role of RSD in advancing biophysical science, particularly in the characterization of proteins. Leveraging the absence of gravity aboard the ISS, the RSD enables researchers to isolate shear-induced aggregation processes relevant to neurodegenerative diseases such as Alzheimer’s and Parkinson’s, offering insight into mechanisms that are difficult to observe with ground-based experiments.

The presentation traced the RSD development, beginning with the initial campaign in 2016 which was funded by Biological and Physical Sciences (BPS) for hardware development and the first science campaign, and culminating in the most recent 2025 flight campaign, which involved the study of three key proteins: Immunoglobulin G (IgG), Insulin, and Human Serum Albumin (HSA).

A highlight of the session was a discussion of the RSD’s custom camera configuration, which has enabled a novel fluid characterization technique known as Particle Tracking Velocimetry (PTV). This method allows researchers to visually track particle motion within the fluid drop, supporting the validation and refinement of theoretical and computational models describing protein behavior in microgravity.

Adam further explained how in-situ imaging and velocimetry techniques, enabled by the unique RSD camera setup, enhance the analysis of fluid flow and shear-driven aggregation at the molecular level.

The presentation showcased a series of comparative videos from past and current RSD campaigns, illustrating protein dynamics under varying sample compositions. He emphasized how flight data are being compared against Earth analog experiments to 1) validate predictive models and 2) inform the design of future microgravity research – the two-fold focus of the research from the beginning.

The session concluded with a summary of preliminary findings from the 2025 campaign, including multi-geometry rheometry results, which offer deeper insight into the viscoelastic behavior of proteins under shear. These findings may well contribute to the development of future pharmaceutical and therapeutic strategies.

To view the entire presentation, a recording is available for downloaded from the 2025 ISSRDC site.

Visit the Physical Sciences Informatics (PSI) database to access experiment data from two RSD campaigns, Interfacial Bioprocessing of Pharmaceuticals (IBP-I) and Amyloid Fibril Formation (AFF) with additional RSD data planned for release in 2026.

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Astronaut Candidates Get to Work at Johnson Space Center

NASA announced its newest class of astronaut candidates on Sept. 22, 2025, at the agency’s Johnson Space Center in Houston. After the welcome ceremony, the 10 highly qualified individuals rolled up their sleeves and prepared for the next step in their journey to the stars: nearly two years of training to become flight-eligible for missions to low Earth orbit, the Moon, and ultimately, Mars.

The training astronaut candidates complete is comprehensive and rigorous. They learn about NASA’s history and vision, and how astronauts advance the agency’s mission. They take classes on space health – gaining an understanding of radiation exposure, microgravity’s effects on the human body, space food and nutrition, and how to use the exercise equipment aboard the International Space Station. They also study first aid and practice providing medical care for crewmates. Each candidate will receive flight training, learning to pilot or improving their current piloting skills through the T-38 supersonic jet and other aviation platforms.

With NASA’s plans for the future of exploration, this class of astronauts may have opportunities to fly to low Earth orbit, or even beyond. Some may contribute to research and technology investigations taking place aboard the space station – which is about to celebrate 25 years of continuous human presence in space. Others may venture to the Moon to prepare for future Mars missions.   

To be ready for any destination, this class will complete both space station training and advanced preparation for deep space. These exercises allow astronaut candidates to work through problems and build relationships with their classmates while preparing them for space flights.

“Training was such an intense period that we got to know each other really well,” said NASA astronaut Anil Menon, who joined the agency as part of the 2021 class – astronaut group 23. “Now when we come together, there are these moments – like we might be handing off a capcom shift, or we might be flying a jet together – and in those moments, I feel like I know them so well that we know how to navigate all sorts of challenges together and just be our best selves as a team.”

Astronaut candidate training also teaches foundational skills that can be applied to any destination in space. The group will complete several dives in the Neutral Buoyancy Laboratory, simulating spacewalks in different environments and learning how to do maintenance tasks in microgravity with a full-scale underwater mockup of the International Space Station as their worksite. They will also train inside other mockups of space vehicles, learning emergency procedures, maintenance, and repair of spacecraft, along with how to contribute to future developmental programs.

Robotics training will prepare them to use the station’s Canadarm2 robotic arm. They will trek through the wilderness as part of their land and water survival training, and they will study geology in the classroom and in the field. The group will practice tasks in a variety of simulations, leveraging Johnson’s world-class facilities, virtual reality, and immersive technologies. Additionally, the class will work shifts in the Mission Control Center in Houston to experience a day in the life of the people who keep watch over the astronauts and vehicles.

Astronaut candidates who successfully complete the training program celebrate their achievement in a graduation ceremony, after which they are officially flight-eligible members of NASA’s astronaut corps. They will also receive office and ground support roles at Johnson while they await future flight assignments.

“I’ve been exposed to a lot of different parts of what we do at Johnson Space Center, working both with the current increment of supporting operations aboard the International Space Station, as well as supporting some development of the Orion spacecraft and Artemis II preparations,” said NASA astronaut Chris Birch, another member of astronaut group 23.

Many members of NASA’s active astronaut corps emphasize that the learning does not stop when astronaut candidate training ends. “You have the foundational training and you continue to build off of that,” said Deniz Burnham, adding that the hardest days can be the most educational. “You get to learn, you get to improve, and then you’re still getting the opportunity. It’s such a positively unique experience and environment, and you can’t help but be grateful.”

As NASA astronaut Frank Rubio, class mentor, told the group, “You’ll become part of a legacy of those who trained before you, continuing the adventure they started, and looking ahead to future human exploration.”

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Linda E. Grimm