Using image-based size analysis for determining the size distribution and flux of eolian particles sampled in coastal northern Chile (23° S)
Author
dc.contributor.author
Flores Aqueveque, Valentina Alejandra
Author
dc.contributor.author
Caquineau, Sandrine
es_CL
Author
dc.contributor.author
Alfaro, Stephane
es_CL
Author
dc.contributor.author
Valdés, Jorge
es_CL
Author
dc.contributor.author
Vargas Easton, Víctor
es_CL
Admission date
dc.date.accessioned
2015-01-08T14:54:05Z
Available date
dc.date.available
2015-01-08T14:54:05Z
Publication date
dc.date.issued
2014
Cita de ítem
dc.identifier.citation
Journal of Sedimentary Research, 2014, v. 84, 238–244
en_US
Identifier
dc.identifier.other
DOI: http://dx.doi.org/10.2110/jsr.2014.23
Identifier
dc.identifier.uri
https://repositorio.uchile.cl/handle/2250/127004
General note
dc.description
Artículo de publicación ISI
en_US
Abstract
dc.description.abstract
The aim of this study was to determine the size distribution and flux of the mineral fraction collected in marine
sediment traps in Mejillones Bay (23u S) using image-based size analysis. In this bay the material settling in the water column is
a mixture of biogenic particles and lithic grains. The sediments analyzed correspond to four samples collected in the austral
spring of 2008. We used image-based size analysis because it presents several advantages, which makes it an ideal method to
study fine marine sediments. This analysis also yielded important information about the aspect and the morphology of the
particles. In order to analyze the lithic fraction only, different pretreatments were applied and size—analyses were carried out
with and without image information. Besides the main lithic components (quartz, feldspar, amphiboles, and micas), some
nonlithic particles corresponding mainly to organic-matter remains were observed in the images, showing that the pretreatment
was not fully effective. Biogenic silica and unexpected dark particles of probable anthropogenic origin were also detected. To
avoid the influence of nonlithic grains in the analysis, the images were filtered based on the aspect of the particles using various
discrimination tools. Before and after this removal, the size distributions of the samples were estimated and used to calculate the
total flux. As compared to the flux of lithic particles, this total flux displays a systematic overestimation of up to 12%. As a
consequence, using image-based size analysis allows not only enhancing the determination of the size distribution and flux but
also controlling and improving the pretreatments protocols.
en_US
Patrocinador
dc.description.sponsorship
This investigation was carried out within the framework of an international
scientific collaboration between the University of Chile (Department of
Geology and Department of Geophysics), the University of Antofagasta
(Faremar), the University of Paris XII and Paris-Diderot (LISA), and IRD
(PALEOTROPIQUE), favored by the ECOS-CONICYT #C05U03 cooperation
project. Field experiments and data acquisition were funded by project
Fondecyt 11060484. Additional funds were provided by project Fondecyt
11121543 and project JEAI LASPAL, from the IRD–University of
Antofagasta–University of Chile cooperation program