Fundamental relations of mineral specific magnetic carriers for paleointensity determination
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F17%3A10363669" target="_blank" >RIV/00216208:11310/17:10363669 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/17:00481730
Result on the web
<a href="http://dx.doi.org/10.1016/j.pepi.2017.09.008" target="_blank" >http://dx.doi.org/10.1016/j.pepi.2017.09.008</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.pepi.2017.09.008" target="_blank" >10.1016/j.pepi.2017.09.008</a>
Alternative languages
Result language
angličtina
Original language name
Fundamental relations of mineral specific magnetic carriers for paleointensity determination
Original language description
A fundamental linear relationship exists between the efficiency of thermoremanent magnetization measured at room temperature and the magnitude of the ambient field at the time of acquisition. The magnetic efficiency (the ratio of thermoremanent magnetization to saturation remanent magnetization) multiplied by the saturation mag-netization is proportional to the magnetizing field, where the proportionality constant is independent of magnetic mineralogy and domain state. The empirical constant for this equation was determined using existing experimen-tal data of single domain through pseudosingle domain to multidomain states of iron, meteoritic iron, magnetite, maghemite, pyrrhotite, and hematite. We show that the acquired magnetic efficiency is closely related to two types of demagnetizing fields that act as barriers against domain wall pinning during magnetic acquisition. The first relates to the saturation magnetization that is derived from the distribution of Bohr magnetons within the crystal lattice, and the second originates from grain shape. Theoretical considerations imply a factor of two dif-ference in the magnetic efficiency acquired during laboratory and geologic timescales. This equation reveals that troilite may be a potentially important magnetic carrier for extraterrestrial magnetism. Using magnetic scanning techniques, our relationship allows for estimating the paleointensity from samples that contain more than one magnetic species.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/GA17-05935S" target="_blank" >GA17-05935S: Role of changes in environemntal chemistry on lake ecosystems at the Younger Dryas onset</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2017
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Physics of the Earth and Planetary Interiors
ISSN
0031-9201
e-ISSN
—
Volume of the periodical
neuveden
Issue of the periodical within the volume
septembre
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
7
Pages from-to
—
UT code for WoS article
000415773900005
EID of the result in the Scopus database
—