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(Japanese) AGUで廣瀬研究室から3名発表しました!

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(Japanese) 廣瀬研究室から4名が第63回高圧討論会に参加しました!

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(Japanese) 廣瀬先生と学生3人がIMA2022学会に参加しました

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(Japanese) 2022年 集合写真を撮りました

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ABOUT

We know that the interior of the earth is actually divided into many layers, just like an onion. When you peel away these layers one at a time from the outside in the same way you would peel an onion’s skin, you finally come to the core. The mantle above the core is also divided into four layers, and by 1974 we had identified what the first three layers were made of. When it comes to the lowest layer, the fourth layer, however, there were all kinds of hypotheses but they all remained in the realm of conjecture. This is why I wanted to elucidate the true nature of this material that formed the fourth layer.

My own determination as a scientist to take up for the first time in the world experiments that nobody had ever attempted.

The most important things are enthusiasm, effort and a little bit of luck. Moreover, in everything you do, it is important to first meet the challenge without making up your mind at the outset that it is impossible. This simple way of looking at things will change your life significantly. If some of you hold the view that you may not be able to pursue the scientific path just because your grades aren’t good, get rid of such a silly notion immediately and instead pursue every challenge that comes your way. When you do that, the path to the future will naturally open up before you.


Kei Hirose

RESEARCH

We investigate the Earth’s deep interior materials and dynamics with ultra-high pressure and temperature experiments.

We know that the interior of the earth is actually divided into many layers, just like an onion. When you peel away these layers one at a time from the outside in the same way you would peel an onion’s skin, you finally come to the core. The mantle above the core is also divided into four layers, and by 1974 we had identified what the first three layers were made of. When it comes to the lowest layer, the fourth layer, however, there were all kinds of hypotheses but they all remained in the realm of conjecture. This is why I wanted to elucidate the true nature of this material that formed the fourth layer.

PostPerovskite

PostPerovskite phase was discovered in the condition of lowermost lower mantle (the red zone) (Murakami et. al. Science 2004)

Member


2022 集合写真


2017 members

2018 members

2019 members

2021 members
PRINCIPAL RESEARCHER

廣瀬 敬(教授)

FACULTY


五味 斎(特任研究員)

奥田 善之(JSPS PD)

Fu Suyu(JSPS PD)

GRADUATE STUDENTS


小澤 佳祐(D3)
日本学術振興会特別研究員 DC1

岡 健太(D3)
日本学術振興会特別研究員 DC1

横尾 舜平(D2)
日本学術振興会特別研究員 DC1

彦坂 晃太郎(D2)
日本学術振興会特別研究員 DC1

堤 裕太郎(D1)

幾田 凪(M2)

坂井 郁哉(M2)

稲田 真子(M1)

栗田 直季(M1)

UNDERGRADUATE STUDENTS
特別研究での所属:
竹澤春樹
三田修平

OB/OG

日下部 真夕 M.S.
– 2019/03 修士課程修了
冨田 涼太 B.S.
– 2019/03 学部卒業
増田 滉己 B.S.
– 2019/03 修士より固体講座 井出研に進学
夏井 文凜 (研究生)
– 2020/03 修士より地震研に進学
長谷川 将弘 M.S.
– 2022/03 修士課程修了