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spelling paper:paper_09218181_v110_n_p321_Ludwig2023-06-08T15:50:49Z Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques Orgeira, María Julia Citrate-bicarbonate-dithionite extraction First-order reversal curve Magnetotactic bacteria and magnetofossils Pelagic carbonates Primary and secondary magnetic minerals Supernova explosion signatures First-order reversal curves Magnetic minerals Magnetotactic Bacteria Pelagic carbonates Supernova explosion Chemical detection Extraction Iron oxides Magnetic hysteresis Magnetic variables measurement Magnetism Minerals Numerical methods Submarine geology Sediments bacterium bicarbonate carbonate dilution explosion iron oxide magnetite measurement method mineral optimization quantitative analysis sediment analysis sediment chemistry Bacteria (microorganisms) We present a novel technique for quantitative unmixing of primary and secondary ferrimagnetic minerals in sediments. Hysteresis and high-resolution first-order reversal curve (FORC) measurements are performed on sediment samples before and after digestion in a citrate-bicarbonate-dithionite (CBD) solution optimized for maximum selective extraction of secondary fine-grained iron oxides. The difference between magnetic measurements of untreated and CBD-treated sample materials is used to calculate the original magnetic signature of CBD-extractable minerals. A combination of selective chemical extraction and magnetic measurements suited for the detection of single-domain particles provides a cross-check between chemical and magnetic unmixing of primary and secondary iron oxides and resolves the non-uniqueness problem of numerical unmixing methods. A quantitative magnetic characterization of secondary ferrimagnetic minerals in a magnetofossil-rich pelagic carbonate is presented for the first time. It can be used for calibration of recently developed fast magnetic unmixing techniques. CBD-based Fe extraction from sediments with minimal clastic and/or aeolian inputs, such as pelagic carbonates, is particularly suited for the search for cosmogenic 60Fe signatures from supernova explosions, because 60Fe dilution by dissolved primary Fe-bearing minerals is minimized. © 2013 Elsevier B.V. Fil:Orgeira, M.J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2013 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09218181_v110_n_p321_Ludwig http://hdl.handle.net/20.500.12110/paper_09218181_v110_n_p321_Ludwig
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Citrate-bicarbonate-dithionite extraction
First-order reversal curve
Magnetotactic bacteria and magnetofossils
Pelagic carbonates
Primary and secondary magnetic minerals
Supernova explosion signatures
First-order reversal curves
Magnetic minerals
Magnetotactic Bacteria
Pelagic carbonates
Supernova explosion
Chemical detection
Extraction
Iron oxides
Magnetic hysteresis
Magnetic variables measurement
Magnetism
Minerals
Numerical methods
Submarine geology
Sediments
bacterium
bicarbonate
carbonate
dilution
explosion
iron oxide
magnetite
measurement method
mineral
optimization
quantitative analysis
sediment analysis
sediment chemistry
Bacteria (microorganisms)
spellingShingle Citrate-bicarbonate-dithionite extraction
First-order reversal curve
Magnetotactic bacteria and magnetofossils
Pelagic carbonates
Primary and secondary magnetic minerals
Supernova explosion signatures
First-order reversal curves
Magnetic minerals
Magnetotactic Bacteria
Pelagic carbonates
Supernova explosion
Chemical detection
Extraction
Iron oxides
Magnetic hysteresis
Magnetic variables measurement
Magnetism
Minerals
Numerical methods
Submarine geology
Sediments
bacterium
bicarbonate
carbonate
dilution
explosion
iron oxide
magnetite
measurement method
mineral
optimization
quantitative analysis
sediment analysis
sediment chemistry
Bacteria (microorganisms)
Orgeira, María Julia
Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
topic_facet Citrate-bicarbonate-dithionite extraction
First-order reversal curve
Magnetotactic bacteria and magnetofossils
Pelagic carbonates
Primary and secondary magnetic minerals
Supernova explosion signatures
First-order reversal curves
Magnetic minerals
Magnetotactic Bacteria
Pelagic carbonates
Supernova explosion
Chemical detection
Extraction
Iron oxides
Magnetic hysteresis
Magnetic variables measurement
Magnetism
Minerals
Numerical methods
Submarine geology
Sediments
bacterium
bicarbonate
carbonate
dilution
explosion
iron oxide
magnetite
measurement method
mineral
optimization
quantitative analysis
sediment analysis
sediment chemistry
Bacteria (microorganisms)
description We present a novel technique for quantitative unmixing of primary and secondary ferrimagnetic minerals in sediments. Hysteresis and high-resolution first-order reversal curve (FORC) measurements are performed on sediment samples before and after digestion in a citrate-bicarbonate-dithionite (CBD) solution optimized for maximum selective extraction of secondary fine-grained iron oxides. The difference between magnetic measurements of untreated and CBD-treated sample materials is used to calculate the original magnetic signature of CBD-extractable minerals. A combination of selective chemical extraction and magnetic measurements suited for the detection of single-domain particles provides a cross-check between chemical and magnetic unmixing of primary and secondary iron oxides and resolves the non-uniqueness problem of numerical unmixing methods. A quantitative magnetic characterization of secondary ferrimagnetic minerals in a magnetofossil-rich pelagic carbonate is presented for the first time. It can be used for calibration of recently developed fast magnetic unmixing techniques. CBD-based Fe extraction from sediments with minimal clastic and/or aeolian inputs, such as pelagic carbonates, is particularly suited for the search for cosmogenic 60Fe signatures from supernova explosions, because 60Fe dilution by dissolved primary Fe-bearing minerals is minimized. © 2013 Elsevier B.V.
author Orgeira, María Julia
author_facet Orgeira, María Julia
author_sort Orgeira, María Julia
title Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
title_short Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
title_full Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
title_fullStr Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
title_full_unstemmed Characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
title_sort characterization of primary and secondary magnetite in marine sediment by combining chemical and magnetic unmixing techniques
publishDate 2013
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09218181_v110_n_p321_Ludwig
http://hdl.handle.net/20.500.12110/paper_09218181_v110_n_p321_Ludwig
work_keys_str_mv AT orgeiramariajulia characterizationofprimaryandsecondarymagnetiteinmarinesedimentbycombiningchemicalandmagneticunmixingtechniques
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