National Science Foundation (NSF)-funded researchers at Amherst College in Massachusetts and the University of Texas at Austin have described a new technique based in particle physics that might one day reveal, in more detail than ever before, the composition and characteristics of the deep Earth.
There’s just one catch: The technique relies on a fifth force of nature that has not yet been detected, but some particle physicists think it might exist. The fifth force would be in addition to gravity, the weak and strong nuclear forces and electromagnetism.
Physicists call this fifth force a long-range spin-spin interaction. As theorized, the fifth force would rely on the building blocks of atoms (electrons, protons, and neutrons), separated over vast distances, to “feel” each other’s presence.
If it does exist, this exotic new force would connect matter at Earth’s surface with matter hundreds or even thousands of miles deep within Earth’s mantle and could potentially provide new information about the composition and characteristics of deep Earth, which is poorly understood because of its inaccessibility.
“The most rewarding and surprising thing about this project was realizing that particle physics could actually be used to study the deep Earth,” says Jung-Fu “Afu” Lin, associate professor at the University of Texas at Austin’s Jackson School of Geosciences and co-author of the study appearing in Science.
The research was supported by NSF’s Geoscience and Mathematical and Physical Science Directorates, the U.S. Department of Energy (DOE), and the Carnegie/DOE Alliance Center.
This new force could help settle a scientific quandary. When earth scientists previously have tried to model how factors such as iron concentration and physical and chemical properties of matter vary with depth—for example, using the way earthquake rumbles travel through the Earth or through laboratory experiments designed to mimic the intense temperatures and pressures of the deep Earth—they get different answers. The fifth force, assuming it exists, might help reconcile these conflicting lines of evidence.
Earth’s mantle is a thick geological layer sandwiched between the thin outer crust and central core, made up mostly of iron-bearing minerals. The atoms in these minerals and the subatomic particles making up the atoms have a property called spin.
Spin can be thought of as an arrow that points in a particular direction. It is thought that Earth’s magnetic field causes some of the electrons in these mantle minerals to become slightly spin-polarized, meaning the directions in which they spin are no longer completely random, but have some preferred orientation. These electrons have been dubbed “geoelectrons.”
The goal of this project was to see whether the scientists could use the proposed long-range spin-spin interaction to detect the presence of these distant geoelectrons.
The researchers, led by Larry Hunter, professor of physics at Amherst College, first created a computer model of Earth’s interior to map the expected densities and spin directions of geoelectrons. The model was based in part on insights gained from Lin’s laboratory experiments, which measure electron spins in minerals at the high temperatures and pressures of Earth’s interior. This map gave the researchers clues about the strength and orientations of interactions they might expect to detect in their laboratory in Amherst, Mass.
Second, the researchers used a specially designed apparatus to search for interactions between geoelectrons deep in the mantle and subatomic particles at Earth’s surface. The team’s experiments essentially explored whether the spins of electrons, neutrons, or protons in various laboratories might have a different energy, depending on the direction with respect to the Earth that they were pointing.
“We know, for example, that a magnet has a lower energy when it is oriented parallel to the geomagnetic field and it lines up with this particular direction–that is how a compass works,” Hunter says. “Our experiments removed this magnetic interaction and looked to see if there might be some other interaction with our experimental spins. One interpretation of this ‘other’ interaction is that it could be a long-range interaction between the spins in our apparatus and the electron spins within the Earth, that have been aligned by the geomagnetic field. This is the long-range spin-spin interaction we were looking for.”
Although the apparatus was not able to detect any such interactions, the researchers could at least infer that such interactions, if they exist, must be incredibly weak—no more than a millionth of the strength of the gravitational attraction between the particles. That’s useful information as scientists now look for ways to build ever more sensitive instruments to search for the elusive fifth force.
“No one had previously thought about the possible interactions that might occur between the Earth’s spin-polarized electrons and precision laboratory spin-measurements,” says Hunter.
If the long-range spin-spin interactions are discovered in future experiments, “geoscientists can eventually use such information to reliably understand the geochemistry and geophysics of the planet’s interior,” says Lin.
Source: National Science Foundation