Skip to main content

So This is How You Get Magnetars

Neutron stars are stellar remnants. Composed of dense nuclear material, they all have strong magnetic fields. But the magnetic fields of some neutron stars can be a thousand times stronger. They are known as magnetars, and we aren’t entirely sure how they generated such powerful magnetic fields. But a new study in Nature Astronomy reveals some clues.

The general thought has been that magnetars create their fields through some type of dynamo process. This is where a flow of magnetic material generates a magnetic field. Since the flow is driven by heat convection, it can power strong fields. Earth’s magnetic field is unusually strong for a planet of its size and is powered by the convection of iron in its core. However, the core of a neutron star is made of nucleons, not atoms, so it is difficult to determine a specific dynamo process for magnetars.

For this study, the team wanted to understand what are known as low-field magnetars. These are magnetars that have weaker magnetic fields than most magnetars, but still generate bursts of X-rays and gamma rays. Most magnetars are identified by their high-energy emissions, since it takes intense magnetic fields to create such powerful bursts. Low-field magnetars shouldn’t have a strong enough field to create such bursts, but they sometimes do. This would suggest that at times their magnetic fields become intense. The question is how.

To answer this question, the team ran computer simulations of several dynamo models, looking for one that best fit the observational data. They found that the best fit involved what’s known as the Tayler–Spruit dynamo. This dynamo is well known in stellar models and involves the differential rotation of a stellar core. Stars don’t rotate as a single rigid object. Instead, different latitudes of a star rotate at slightly different rates. This is likely caused by a fast-rotating core, which can produce the Tayler–Spruit dynamo.

The authors demonstrated that as a low-field magnetar forms, the supernova that created the magnetar transfers angular momentum to its core, thus creating a differential rotation. Through the Tayler–Spruit dynamo, this can create bursts of intense magnetic fields that power the X-rays and gamma rays we observe from these stars. This process is likely unique for low-field magnetars, as opposed to traditional magnetars that generate their magnetic fields in other ways.

Reference: Igoshev, Andrei, et al. “A connection between proto-neutron-star Tayler–Spruit dynamos and low-field magnetars.” Nature Astronomy (2025): 1-11.

The post So This is How You Get Magnetars appeared first on Universe Today.



from Universe Today https://ift.tt/gRyeIlA
via IFTTT

Comments

Popular posts from this blog

Researchers Match Up 12 Meteorites with the Near-Earth Asteroids They Came From

Every day meteoroids blast through our planet’s atmosphere to hit the ground as meteorites. A team of researchers in Italy traced twelve of them to progenitor asteroids that orbit in near-Earth space. Scientists treasure meteorites because they reveal information about their parent bodies. In an arXiv paper, two Italian researchers—Albino Carbognani and Marco Fenucci—analyze the characteristics of the parent bodies of 20 selected meteorites. They were able to track all but eight back to their parent asteroids. Based on their work, the pair says at least a quarter of meteorites come from collisions that happened in near-Earth space and not in the Main Belt. Meteorites from Near-Earth Asteroids: How They Got Here Many meteorites are chondritic, similar to asteroids in the Main Belt (or came from it). In their paper, the authors point out that progenitor meteoroids (including many that fall to Earth and become meteorites) formed millions of years ago following collisions between main-...

JWST Takes a Detailed Look at Jupiter’s Moon Ganymede

Nature doesn’t conform to our ideas of neatly-contained categories. Many things in nature blur the lines we try to draw around them. That’s true of Jupiter’s moon Ganymede, the largest moon in the Solar System. The JWST took a closer look at Ganymede, the moon that’s kind of like a planet, to understand its surface better. Ganymede is basically a planet, except it doesn’t orbit the Sun. If it did orbit the Sun instead of Jupiter, it would be indistinguishable from a planet. It has a differentiated internal structure with a molten core that produces a magnetic field. It has a silicon mantle much like Earth’s, and has a complex icy crust with a deep ocean submerged beneath it. It has an atmosphere, though it’s thin. It’s also larger than Mercury, and almost as large as Mars. According to the authors of a new study, it’s an archetype of a water world. But even with all this knowledge of the huge moon, there are details yet to be revealed. This is especially true of its complex surface...

The Ultraviolet Habitable Zone Sets a Time Limit on the Formation of Life

The field of extrasolar planet studies has grown exponentially in the past twenty years. Thanks to missions like Kepler, the Transiting Exoplanet Survey Satellite (TESS), and other dedicated observatories, astronomers have confirmed 5,690 exoplanets in 4,243 star systems . With so many planets and systems available for study, scientists have been forced to reconsider many previously-held notions about planet formation and evolution and what conditions are necessary for life. In the latter case, scientists have been rethinking the concept of the Circumsolar Habitable Zone (CHZ). By definition, a CHZ is the region around a star where an orbiting planet would be warm enough to maintain liquid water on its surface. As stars evolve with time, their radiance and heat will increase or decrease depending on their mass , altering the boundaries of the CHZ. In a recent study , a team of astronomers from the Italian National Institute of Astrophysics (INAF) considered how the evolution of star...