Directional dependence of magnetization and coercivity in hematite ore experimentally deformed in torsion

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F25%3A00637206" target="_blank" >RIV/67985530:_____/25:00637206 - isvavai.cz</a>

Výsledek na webu

<a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024JB031033" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024JB031033</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1029/2024JB031033" target="_blank" >10.1029/2024JB031033</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Directional dependence of magnetization and coercivity in hematite ore experimentally deformed in torsion

Popis výsledku v původním jazyce

Rock-magnetic properties are widely used to resolve the composition, concentration, size, shape, and alignment of iron oxides in rock samples. Although anisotropy of magnetic susceptibility is measured routinely, acquisition of remanent magnetization as well as hysteresis loops are usually measured in one direction only. This may lead to biased interpretation of the results. In our study, observation of strong directional dependence of remanence acquisition curves and hysteresis loops in experimentally deformed samples of hematite ore is reported. While the original undeformed hematite ore sample exhibited magnetic properties practically independent of the direction, the specimens which experienced deformation in torsion showed significant anisotropy. For example, the anisotropy of saturation magnetization reached several tens of percent. Our results suggest that experimental deformation resulted in neoformation of magnetite nanoparticles, as well as shift of the original hematite coercivity spectra toward lower values. These findings have significant impact on the remanent and induced magnetization measurement protocols and interpretation of the data. Anisotropy of these parameters should be checked at least in cases when hematite is assumed to be present in the samples, or the samples underwent creep deformation.

Název v anglickém jazyce

Directional dependence of magnetization and coercivity in hematite ore experimentally deformed in torsion

Popis výsledku anglicky

Rock-magnetic properties are widely used to resolve the composition, concentration, size, shape, and alignment of iron oxides in rock samples. Although anisotropy of magnetic susceptibility is measured routinely, acquisition of remanent magnetization as well as hysteresis loops are usually measured in one direction only. This may lead to biased interpretation of the results. In our study, observation of strong directional dependence of remanence acquisition curves and hysteresis loops in experimentally deformed samples of hematite ore is reported. While the original undeformed hematite ore sample exhibited magnetic properties practically independent of the direction, the specimens which experienced deformation in torsion showed significant anisotropy. For example, the anisotropy of saturation magnetization reached several tens of percent. Our results suggest that experimental deformation resulted in neoformation of magnetite nanoparticles, as well as shift of the original hematite coercivity spectra toward lower values. These findings have significant impact on the remanent and induced magnetization measurement protocols and interpretation of the data. Anisotropy of these parameters should be checked at least in cases when hematite is assumed to be present in the samples, or the samples underwent creep deformation.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/GA22-12828S" target="_blank" >GA22-12828S: Nový pohled na interpretaci magnetických staveb za pomoci 3D mikrostrukturní analýzy, numerického modelování a kvantově mechanického popisu</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Geophysical Research-Solid Earth

ISSN

2169-9313

e-ISSN

2169-9356

Svazek periodika

130

Číslo periodika v rámci svazku

7

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

15

Strana od-do

e2024JB031033

Kód UT WoS článku

001520852500001

EID výsledku v databázi Scopus

2-s2.0-105009824986