4 April 2008—You probably haven’t noticed, but the length of a day is not what it used to be. Though only on the order of a few milliseconds’ difference and observable only over a period of decades, the time it takes the Earth to make one revolution varies. This anomaly has teased earth scientists for some time. They suspected that it is due to the exchange in angular momentum between the Earth’s fluid core and rocky mantle, but how that happens was still a question.
In today’s issue of Science , researchers at the Tokyo Institute of Technology provide evidence that a mineral phase in the Earth’s mantle is electrically conductive and could be doing the job by electromagnetically linking the core to the mantle. The Tokyo scientists say that the conductive mineral could point superconductor researchers in a new direction, too.
The conductive mineral, called post-perovskite, appears in the lowermost area of the Earth’s mantle, the rocky shell that surrounds the inner and outer cores of the Earth and is itself covered by the Earth’s crust. The most common component of the lower mantle is perovskite, which is rich in magnesium silicate (MgSiO 3 ).
Back in 2004, the Tokyo team reported that perovskite transitions into post-perovskite at depths below about 2600 kilometers because of the increasing pressure from the weight of the earth above. In making their discovery, the researchers had to recreate the temperatures and pressures at those depths in the lab. Other research groups in Japan and Switzerland independently made the same discovery at about the same time.
”Discovering the MgSiO 3 post-perovskite phase helped explain the differences in anomalous seismic-wave speeds propagating in the lowermost mantle,” says Kei Hirose, a professor of earth and planetary sciences at the Tokyo Institute of Technology and leader of the research group. ”And because the structure of the post-perovskite is very different from the structure of the perovskite, we expected their physical properties would also be different.”
To test this expectation, the group turned to the same lab techniques they employed to discover the mineral layer. They compressed samples of MgSiO 3 at room temperature using a diamond anvil and then heated the samples with a laser to synthesize both perovskite and post-perovskite. But this time, they also measured the materials’ conductivities.