Stunning Plasma Experiment: Modeling Earth’s Magnetosphere in the Laboratory

Modeling Earth’s Magnetosphere

Experimental platform combines Giant Plasma System with lasers, magnetic dipoles; reveals insights about Earth’s protect towards photo voltaic wind.

A magnetosphere types round any magnetized object, corresponding to a planet, that's immersed inside a stream of ionized fuel, referred to as plasma. As a result of Earth possesses an intrinsic magnetic area, the planet is surrounded by a big magnetosphere that extends out into area, blocks deadly cosmic rays and particles from the solar and stars, and permits life itself to exist.

In Physics of Plasmas, by AIP Publishing, scientists from Princeton, UCLA, and the Instituto Superior Técnico, Portugal, report a technique to check smaller magnetospheres, typically simply millimeters thick, within the laboratory.

These mini-magnetospheres have been noticed round comets and close to sure areas of the moon and have been advised to propel spacecraft. They're good testbeds for finding out bigger planet-sized magnetospheres.

Laser-Driven Plasma Expanding Into Dipole Magnetic Field

Picture of the laser-driven plasma increasing into the dipole magnetic area. Magnetic area measurements exhibiting the placement of the magnetopause are overlaid. Credit score: Derek Schaeffer

Earlier laboratory experiments have been carried out using plasma wind tunnels or high-energy lasers to create mini-magnetospheres. Nonetheless, these earlier experiments have been restricted to 1D measurements of magnetic fields that don't seize the complete 3D conduct scientists want to know.

“To beat these limitations, we have now developed a brand new experimental platform to check mini-magnetospheres on the Giant Plasma System (LAPD) at UCLA,” stated creator Derek Schaeffer.

This platform combines the magnetic area of the LAPD with a quick laser-driven plasma and a current-driven dipole magnet.

The LAPD magnetic area offers a mannequin of the photo voltaic system’s interplanetary magnetic area, whereas the laser-driven plasma fashions the photo voltaic wind and the dipole magnet offers a mannequin for the Earth’s inherent magnetic area. Motorized probes permit system scans in three dimensions by combining knowledge from tens of hundreds of laser photographs.


Simulation of a laser-driven plasma increasing right into a dipole magnetic area. Credit score: Filipe Cruz

One benefit to utilizing this setup is that the magnetic area and different parameters might be rigorously diversified and managed.

If the dipole magnet is switched off, all indicators of a magnetosphere disappear. When the magnetic area of the dipole is switched on, a magnetopause might be detected, which is essential proof of the formation of a magnetosphere.

A magnetopause is the place within the magnetosphere the place stress from the planetary magnetic area is precisely balanced by the photo voltaic wind. The experiments revealed that because the dipole magnetic area is elevated, the magnetopause will get bigger and stronger.

The impact on the magnetopause was predicted by pc simulations, which have been carried out by the investigators to know and validate their experimental outcomes extra absolutely. These simulations can even information future experiments, together with research using a cathode not too long ago put in on the LAPD.

“The brand new cathode will allow sooner plasma flows, which in flip will permit us to check the bow shocks noticed round many planets,” Schaeffer stated.

Different experiments will research magnetic reconnection, an necessary course of in Earth’s magnetosphere wherein magnetic fields annihilate to launch large power.

Reference: “Laser-driven, ion-scale magnetospheres in laboratory plasmas. I. Experimental platform and first outcomes” by Derek B. Schaeffer, Filipe D. Cruz, Robert S. Dorst, Fabio Cruz, Peter V. Heuer, Carmen G. Constantin, Patrick Pribyl, Christoph Niemann, Luis O. Silva and Amitava Bhattacharjee, 12 April 2022, Physics of Plasmas.

DOI: 10.1063/5.0084353

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