Modified Jeffery model: Influence of particle concentration on mineral fabric in moderately concentrated suspensions
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10139636" target="_blank" >RIV/00216208:11310/13:10139636 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/13:00000029
Result on the web
<a href="http://dx.doi.org/10.1002/jgrb.50105" target="_blank" >http://dx.doi.org/10.1002/jgrb.50105</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/jgrb.50105" target="_blank" >10.1002/jgrb.50105</a>
Alternative languages
Result language
angličtina
Original language name
Modified Jeffery model: Influence of particle concentration on mineral fabric in moderately concentrated suspensions
Original language description
A modified Jeffery model involving particle interactions allows the simulation of preferred orientation of crystals and the anisotropy of magnetic susceptibility in magmatic flow with up to 40% of rigid particle fraction. Numerical simulations are compared to analogue and natural fabrics. A study of the role of particle concentration shows that the increasing percentage of crystal fraction in dilute suspensions leads to progressive attenuation of the fabric intensity and cyclicity. At high strains in simple shear flow, the lineation converges to a constant value close to the shear plane. With increasing particle concentration, the fabric diverges from the shear direction reflecting the effect of increased crystal tiling. The model can be applied to quantify mineral preferred orientations of crystal mushes in magmatic fabric studies.
Czech name
—
Czech description
—
Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
—
Result continuities
Project
<a href="/en/project/LK11202" target="_blank" >LK11202: The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust</a><br>
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach
Others
Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Geophysical Research
ISSN
0148-0227
e-ISSN
—
Volume of the periodical
118
Issue of the periodical within the volume
3
Country of publishing house
US - UNITED STATES
Number of pages
10
Pages from-to
852-861
UT code for WoS article
000318273300005
EID of the result in the Scopus database
—