Results 61 to 70 of about 1,787 (204)
Sulfur‐Bearing hcp Iron for Earth's Inner Core
Abstract Earth's iron core is believed to contain light impurities which should have been included during core formation. In order to place constraints on core composition, here we report the effect of sulfur on density of hexagonal close‐packed (hcp) iron which was not previously examined, using laser‐heated diamond anvil cells with in situ ...
Emiko Sugimura‐Komabayashi +7 more
wiley +1 more source
Abstract Anisotropy of magnetic remanence (AMR) holds promise for quantifying relative paleointensity values from sedimentary rocks. A proof of concept was established for applied fields that exceeded the intensity of the geomagnetic field. Under Earth‐like fields, large uncertainties necessitate the development of a new approach to improve the ...
Felix K. Ostermeier +5 more
wiley +1 more source
Geodynamo Simulations with XSHELLS + SHTns
Details concerning the Spherical Harmonic Transform library SHTns and the geodynamo simulation code XSHELLS. Insights into a big simulation using XSHELLS and SHTns are given at the end.
Nathanael Schaeffer (474534)
core +1 more source
База данных параметров базисных мод и коэффициентов cпектральных моделей геодинамо
Спектральные модели геодинамо строятся на основании конечного набора базисных стационарных полей (мод). Поля скорости, температуры и магнитной индукции представляются в моделях в виде линейных комбинаций базисных мод с коэффициентами (амплитудами ...
Водинчар, Г.М. +2 more
doaj +1 more source
An Ensemble Algorithm Based Component for Geomagnetic Data Assimilation
Geomagnetic data assimilation is one of the most recent developments in geomagnetic studies. It combines geodynamo model outputs and surface geomagnetic observations to provide more accurate estimates of the core dynamic state and provide accurate ...
Zhibin Sun and Weijia Kuang
doaj +1 more source
Electronic correlations and transport in iron at Earth’s core conditions
The heat and electrical conductivity of Earth’s core matter represent key input quantities for geophysical models of the Earth’s core evolution and geodynamo.
L. V. Pourovskii +3 more
doaj +1 more source
Pressure Dependence of Liquid Iron Viscosity From Machine‐Learning Molecular Dynamics
Abstract We have developed a machine‐learning potential that accurately models the behavior of iron under the conditions of Earth's core. By performing numerous nanosecond scale equilibrium molecular dynamics simulations, the viscosities of liquid iron for the whole outer core conditions are obtained with much less uncertainty.
Kai Luo, Xuyang Long, R. E. Cohen
wiley +1 more source
Abstract The Ediacaran–Cambrian (∼635–539 Ma) geomagnetic field is characterized by unusually high reversal rates and markedly weakened field strength. Estimates of these reversal frequencies can reveal key aspects of deep Earth dynamics and their potential influence on surface environments and early complex life.
J. W. L. Afonso +12 more
wiley +1 more source
Current state of Computational Geodynamo
This project describes the physical and mathematical framework for simulating Earth's dynamo using Magneto-Hydrodynamics. Description of the technique can be found in review papers on geodynamo by Gltazmaier and Roberts and Kono.
arushi saxena (3371474)
core +1 more source
Testing the Accuracy of Paleointensity Estimates Using Experimental Pottery Assemblages
Abstract Paleointensity estimates from archaeological pottery represent a key source of information on Holocene variations in geomagnetic field intensity. Yet, pottery rarely exhibits ideal single‐domain behavior that fully satisfies the theoretical assumptions underlying absolute paleointensity methods.
Lior Bar‐Sovik +5 more
wiley +1 more source

