Earth’s ‘solid’ inner core may contain both mushy and hard iron

Locations of earthquakes (red) and corresponding seismic stations (yellow pins). Credit: Butler and Tsuboi (2021).
Locations of earthquakes (red) and corresponding seismic stations (yellow pins). Credit: Butler and Tsuboi (2021).

3,200 miles beneath Earth’s surface lies the inner core, a ball-shaped mass of mostly iron that is responsible for Earth’s magnetic field. In the 1950’s, researchers suggested the inner core was solid, in contrast to the liquid metal region surrounding it.

New research led by Rhett Butler, a geophysicist at the University of Hawai’i at Manoa School of Ocean and Earth Science and Technology (SOEST), suggests that Earth’s “solid” inner core is, in fact, endowed with a range of liquid, soft, and hard structures which vary across the top 150 miles of the inner core.

No human, nor machine has been to this region. The depth, pressure and temperature make inner Earth inaccessible. So Butler, a researcher at SOEST’s Hawai’i Institute of Geophysics and Planetology, and co-author Seiji Tsuboi, research scientist at the Japan Agency for Marine-Earth Science and Technology, relied on the only means available to probe the innermost Earth — earthquake waves.

“Illuminated by earthquakes in the crust and upper mantle, and observed by seismic observatories at Earth’s surface, seismology offers the only direct way to investigate the inner core and its processes,” said Butler.

As seismic waves move through various layers of Earth, their speed changes and they may reflect or refract depending on the minerals, temperature and density of that layer.

In order to infer features of the inner core, Butler and Tsuboi utilized data from seismometers directly opposite of the location where an earthquake was generated. Using Japan’s Earth Simulator supercomputer, they assessed five pairings to broadly cover the inner core region: Tonga-Algeria, Indonesia-Brazil, and three between Chile-China.

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“In stark contrast to the homogeneous, soft iron alloys considered in all Earth models of the inner core since the 1970’s, our models suggest there are adjacent regions of hard, soft, and liquid or mushy iron alloys in the top 150 miles of the inner core,” said Butler. “This puts new constraints upon the composition, thermal history, and evolution of Earth.

The study of the inner core and discovery of its heterogeneous structure provide important new information about dynamics at the boundary between the inner and outer core, which impact the generation Earth’s magnetic field.

“Knowledge of this boundary condition from seismology may enable better, predictive models of the geomagnetic field which shields and protects life on our planet,” said Butler.

The researchers plan to model the inner core structure in finer detail using the Earth Simulator and compare how that structure compares with various characteristics of Earth’s geomagnetic field.

Reference:
Rhett Butler, Seiji Tsuboi. Antipodal seismic reflections upon shear wave velocity structures within Earth’s inner core. Physics of the Earth and Planetary Interiors, Volume 321, December 2021, 106802 DOI: 10.1016/j.pepi.2021.106802

Note: The above post is reprinted from materials provided by University of Hawaii at Manoa. Original written by Marcie Grabowski.