Physicists have taken a significant step toward unraveling one of the most profound enigmas in geophysics: the origin of the Earth’s magnetic field.
A team of researchers from the University of Texas at Austin, in collaboration with scientists from Sichuan and Nanjing Universities in China, believes they have unearthed a fundamental physical mechanism that can help elucidate the surprisingly “soft” characteristics of the Earth’s dense inner core.
Deep within the Earth, approximately 1,800 miles beneath the crust, resides a spherical core primarily composed of iron and nickel. This core, with temperatures ranging from about 8,000 to 10,800 degrees Fahrenheit, consists of two layers: the liquid outer core and the dense, solid inner core. The movement of iron atoms within this core is understood to power the Earth’s magnetic field, a vital element in rendering the planet habitable. This magnetic field not only establishes compass directions but also acts as a protective shield, deflecting potent radiation from solar storms.
Continue reading… “Unlocking Earth’s Magnetic Mystery: The Role of Collective Motion in the Core”
