activity
20182021
most citedReconciliation of experiments and theory on transport properties of iron and the geodynamo

91 citations · 155 across the 4 of their papers we have counts for

collaborators

9 papers

cond-mat.mtrl-sci2021

Iron-rich Fe-O compounds with closest-packed layers at core pressures

Jin Liu, Yang Sun, Chaojia Lv +7

Oxygen solubility in solid iron is extremely low, even at high pressures and temperatures. Thus far, no Fe-O compounds between Fe and FeO endmembers have been reported experimental…

cond-mat.mtrl-sci2021

Strain-Modulated Interlayer Charge and Energy Transfers in MoS2/WS2 Heterobilayer

Joon-Seok Kim, Nikhilesh Maity, Myungsoo Kim +5

Excitonic properties in 2D heterobilayers are closely governed by charge transfer (CT) and excitonic energy transfer (ET) at van der Waals interfaces. Various means have been emplo…

cond-mat.mtrl-sci202064 cited

Low thermal conductivity of iron-silicon alloys at Earth core conditions with implications for the geodynamo

Wen-Pin Hsieh, Alexander F. Goncharov, Stéphane Labrosse +5

Earth core is composed of iron (Fe) alloyed with light elements, e.g., silicon (Si). Its thermal conductivity critically affects Earth thermal structure, evolution, and dynamics, a…

physics.geo-ph202091 cited

Reconciliation of experiments and theory on transport properties of iron and the geodynamo

Zhang Youjun, Hou Mingqiang, Liu Guangtao +6

The amount of heat transport from the core, which constrains the dynamics and thermal evolution of the region, depends on the transport properties of iron. Ohta et al.(2016) and Ko…

cond-mat.mtrl-sci2020

Stacking Order Driven Optical Properties and Carrier Dynamics in ReS2

Yongjian Zhou, Nikhilesh Maity, Amritesh Rai +8

Two distinct stacking orders in ReS2 are identified without ambiguity and their influence on vibrational, optical properties and carrier dynamics are investigated. With atomic reso…

physics.geo-ph2019

Blocked radiative heat transport in the hot pyrolitic lower mantle

Sergey S. Lobanov, Nicholas Holtgrewe, Gen Ito +8

The heat flux across the core-mantle boundary (QCMB) is the key parameter to understand the Earth/s thermal history and evolution. Mineralogical constraints of the QCMB require dec…