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Member Since 2016
Suyu Fu
Post doc, The University of Tokyo, Japan
AGU Research
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Melting Behavior of B1 FeO Up To 186 GPa: Existence of FeO‐Rich Melts in the Lowermost Mantle
GEOPHYSICAL RESEARCH LETTERS
29 april 2024
Suyu Fu, Kei Hirose
FeO is an important component in both mantle silicates and core iron alloys. Understanding its melting behavior and physical properties is crucial ...
Eutectic Melting Curve for the Fe-FeH System
IRON, IRON ALLOYS, AND IRON-BEARING PHASES IN PLANETARY INTERIORS II POSTER
mineral and rock physics | 14 december 2023
Shuhei Mita, Suyu Fu, Kei Hirose
H, C, O, Si, and S are thought to be possible major light elements in the Earths core, but its composition is still unknown (Hirose et al., 2021). To ...
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The Fe-FeH Phase Diagram to Core Pressures by Experiments and Thermodynamic Modeling and the Possible Range of Earth’s Core Composition
IRON, IRON ALLOYS, AND IRON-BEARING PHASES IN PLANETARY INTERIORS I ORAL
mineral and rock physics | 14 december 2023
Kei Hirose, George R. Helffrich, Suyu Fu, Shoh Tag...
Hydrogen is likely to be a major light element in the core. The Fe-FeH phase diagram under high pressure, in particular the composition and temperatur...
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Liquid Density of Fe-H Alloys in Earth’s Outer Core
ADVANCED EXPERIMENTAL, COMPUTATIONAL, AND ANALYTICAL APPROACHES IN EXPLORING DEEP PLANETARY INTERIORS II POSTER
mineral and rock physics | 12 december 2023
Suyu Fu, Kei Hirose, Shunpei Yokoo, Fumiya Sakai
The composition of Earths core plays a key role in the structure, dynamics, and habitability of our planet. The liquid outer core is believed to consi...
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Hydrogen and Silicon Effects on Hexagonal Close Packed Fe Alloys at High Pressures: Implications for the Composition of Earth's Inner Core
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
25 april 2023
Suyu Fu, Stella Chariton, Vitali B. Prakapenka, Sa...
Hexagonal close‐packed (hcp) structured Fe‐Ni alloy is believed to be the dominant phase in the Earth's inner core. This phase is expec...
Understanding the E’ layer at the Topmost Core from Metal-Silicate Melting Experiments
INTERDISCIPLINARY INSIGHTS INTO EARTH AND PLANETARY CORES IV ORAL
study of earth's deep interior | 14 december 2022
Suyu Fu, Kei Hirose, Shunpei Yokoo, Yutaro Tsutsum...
Seismic studies have observed a low-velocity layer of 100-300 km thick at the topmost core, called as E layer (13), which is also expected to be light...
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Single‐Crystal Elasticity of Phase E at High Pressure and Temperature: Implications for the Low‐Velocity Layer Atop the 410‐km Depth
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
02 december 2022
Baoyun Wang, Yanyao Zhang, Suyu Fu, XING DING, Li...
Dense hydrous magnesium silicate (DHMS) phase E is a potential water carrier in subducting slabs that can transport water to the Earth's deep ...
Elasticity of Hydrated Al‐Bearing Stishovite and Post‐Stishovite: Implications for Understanding Regional Seismic VS Anomalies Along Subducting Slabs in the Lower Mantle
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
20 april 2022
Yanyao Zhang, Suyu Fu, Shun-ichiro Karato, Takuo O...
Seismic studies have found seismic scatterers with −2 to −12% shear velocity anomalies along some subducting slabs at 700–1900...