8月 17, 2022

FUTSALNET

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Earth

地震による地震波によって明らかにされた地球の外核の変化

地震波のグループの移動時間の1秒の変動は、地球の奥深くで起こっていることへの重要で前例のない一瞥を私たちに与えます。

この理論は、地球の外核における対流と、惑星の磁場を制御する際のその機能についての私たちの理解を裏付けています。 科学者は、対流フラックスやそれらがどのように変化するかを直接観察していません。 バージニア工科大学の地質学者YingZhouが初めて証拠を提供します。

1997年5月に南太平洋のケルマデク諸島地域で大地震が発生しました。20年余り後の2018年9月に、同じ地域から地震エネルギーの波が発生し、2回目の大地震が同じ場所を襲いました。

バージニア工科大学の地球科学部の地質学者であるYingZhou氏は、20年間の地震活動によって地震が分離されましたが、同じ地域で発生したため、同じ速度で地球の層に地震波を送ることが期待されると述べています。 科学。

地球の核を貫く地震波

青い経路は、外核の領域を移動するコア貫通地震波を示しています。この領域への低強度フラックスの伝達により、地震波速度が増加しました。 クレジット:VirginiaTechのYingZhou

しかし、地震振動をリアルタイムで記録する150を超える世界の地震ネットワークステーションのうちの4つで記録されたデータで、周は2つのイベントの間に驚くべき異常を発見しました。 2018年の地震では、SKS波と呼ばれる地震波のグループが1997年の地震波よりも約1秒速く移動しました。

その結果が最近公開された周によると Seismic Rays Earth's Outer Core

Blue lines are seismic rays in the outer core, where core-penetrating seismic waves moved through that region faster in 2018 than in 1997. Credit: Image courtesy of Ying Zhou

Scientists also have only been able to speculate about the source of gradual changes in strength and direction of the magnetic field that have been observed, which likely involves changing flows in the outer core.

“If you look at the north geomagnetic pole, it’s currently moving at a speed of about 50 kilometers (31 miles) per year,” Zhou said. “It’s moving away from Canada and toward Siberia. The magnetic field is not the same every day. It’s changing. Since it’s changing, we also speculate that convection in the outer core is changing with time, but there’s no direct evidence. We’ve never seen it.”

Zhou set out to find that evidence. The changes happening in the outer core aren’t dramatic, she said, but they’re worth confirming and fundamentally understanding. In seismic waves and their changes in speed on a decade time scale, Zhou saw a means for “direct sampling” of the outer core. That’s because the SKS waves she studied pass right through it.

“SKS” represents three phases of the wave: First it goes through the mantle as an S wave, or shear wave; then into the outer core as a compressional wave; then back out through the mantle as an S wave. How fast these waves travel depend in part on the density of the outer core that’s in their path. If the density is lower in a region of the outer core as the wave penetrates it, the wave will travel faster, just as the anomalous SKS waves did in 2018.

“Something has changed along the path of that wave, so it can go faster now,” Zhou said.

Ying Zhou

Ying Zhou of the Virginia Tech Department of Geosciences. Credit: Photo courtesy of Ying Zhou

To Zhou, the difference in wave speed points to low-density regions forming in the outer core in the 20 years since the 1997 earthquake. That higher SKS wave speed during the 2018 earthquake can be attributed to the release of light elements such as hydrogen, carbon, and oxygen in the outer core during convection that takes place as the Earth cools, she said.

“The material that was there 20 years ago is no longer there,” Zhou said. “This is new material, and it’s lighter. These light elements will move upward and change the density in the region where they’re located.”

To Zhou, it’s evidence that movement really is happening in the core, and it’s changing over time, as scientists have theorized. “We’re able to see it now,” she said. “If we’re able to see it from seismic waves, in the future, we could set up seismic stations and monitor that flow.”

What’s next

That’s Zhou’s next effort. Using a method of wave measurement known as interferometry, her team plans to analyze continuous seismic recordings from two seismic stations, one of which will serve as a “virtual” earthquake source, she said.

“We can use earthquakes, but the limitation of relying on earthquake data is that we can’t really control the locations of the earthquakes,” Zhou said. “But we can control the locations of seismic stations. We can put the stations anywhere we want them to be, with the wave path from one station to the other station going through the outer core. If we monitor that over time, then we can see how core-penetrating seismic waves between those two stations change. With that, we will be better able to see the movement of fluid in the outer core with time.”

Reference: “Transient variation in seismic wave speed points to fast fluid movement in the Earth’s outer core” by Ying Zhou, 25 April 2022, Communications Earth & Environment.
DOI: 10.1038/s43247-022-00432-7

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