Constraints from material properties on the dynamics and evolution of Earth's core
The Earth's magnetic field is powered by energy supplied by the slow cooling and freezing
of the liquid iron core. Efforts to determine the thermal and chemical history of the core have …
of the liquid iron core. Efforts to determine the thermal and chemical history of the core have …
Longitudinal structure of Earth's magnetic field controlled by lower mantle heat flow
Thermal interactions between Earth's core and mantle provide the power that maintains the
geomagnetic field. However, the effect of these interactions and, in particular, the …
geomagnetic field. However, the effect of these interactions and, in particular, the …
Partitioning of sulfur between solid and liquid iron under Earth's core conditions: Constraints from atomistic simulations with machine learning potentials
Partition coefficients of light elements between the solid and liquid iron phases are crucial
for uncovering the state and dynamics of the Earth's core. As one of the major light element …
for uncovering the state and dynamics of the Earth's core. As one of the major light element …
Impurity resistivity of the Earth's inner core
H Gomi, K Hirose - Journal of Geophysical Research: Solid …, 2023 - Wiley Online Library
Seismic observations suggest that the Earth's inner core has a complex structure (eg, the
isotropic layer at the top, innermost inner core, and hemispherical dichotomy). These …
isotropic layer at the top, innermost inner core, and hemispherical dichotomy). These …
Double-diffusive translation of Earth's inner core
R Deguen, T Alboussière… - Geophysical Journal …, 2018 - academic.oup.com
The hemispherical asymmetry of the inner core has been interpreted as resulting from a high-
viscosity mode of inner core convection, consisting in a translation of the inner core. A …
viscosity mode of inner core convection, consisting in a translation of the inner core. A …
A Boussinesq slurry model of the F-layer at the base of Earth's outer core
Seismic observations suggest that a stably stratified layer, known as the F-layer, 150–300
km thick exists at the bottom of Earth's liquid outer core. These observations contrast with the …
km thick exists at the bottom of Earth's liquid outer core. These observations contrast with the …
Geomagnetic field effects on living systems
H Okano, S Ueno - Bioelectromagnetism, 2022 - taylorfrancis.com
The existence of the Earth's magnetic field (geomagnetic field, GMF) is indispensable for the
origin and evolution of life. In this chapter, the authors review the current understanding of …
origin and evolution of life. In this chapter, the authors review the current understanding of …
Elastic scattering of electron in neutral plasma: Interaction model and plasma environment effects
WL Quan, XW Sun, QF Chen - Physics of Plasmas, 2020 - pubs.aip.org
Elastic scattering of electrons in a plasma is studied for its pivotal role in relating transport
properties to plasma composition. A unified effective potential model is developed to …
properties to plasma composition. A unified effective potential model is developed to …
GrowYourIC: a step toward a coherent model of the Earth's inner core seismic structure
A complex inner core structure has been well established from seismic studies, showing
radial and lateral heterogeneities at various length scales. Yet no geodynamic model is able …
radial and lateral heterogeneities at various length scales. Yet no geodynamic model is able …
On observation of local strong heterogeneity in the Earth's inner core below southeastern Asia
DN Krasnoshchekov, PB Kaazik… - Physics of the Earth and …, 2016 - Elsevier
The dimensions and nature of multi-scale structural heterogeneities in the Earth's inner core
(IC) provide important constraints on its mineralogy and formation history. Teleseismic body …
(IC) provide important constraints on its mineralogy and formation history. Teleseismic body …