Nano-magnetite aggregates in red soil on low magnetic bedrock

Main Author: Zhang, Qi
Other Authors: Appel, Erwin, Hu, Shouyun, Pennington, Robert, Meyer, Jannik, Neumann, Udo, Burchard, Michael, Allstaedt, Frederik
Format: Dataset
Terbitan: Mendeley , 2020
Subjects:
Online Access: https:/data.mendeley.com/datasets/m4gvh8p4cf
ctrlnum 0.17632-m4gvh8p4cf.1
fullrecord <?xml version="1.0"?> <dc><creator>Zhang, Qi</creator><title>Nano-magnetite aggregates in red soil on low magnetic bedrock </title><publisher>Mendeley</publisher><description> This Dataset includes supporting materials for a paper that is submitted to JGR-Solid Earth. Soil and lake sediments are important paleoclimate archives and the sediments are often related to soil input. To better understand such settings, we studied the magnetic properties of red soil, its low-magnetic bedrock, and sub-recent sediments of Caohai Lake (CL) in Heqing Basin (HB), China. Red soil is highly magnetic with susceptibilities (&#xAB55;) of ~10-5 m3/kg, dominated by pedogenic nano-magnetite (~10-15 nm) arranged in aggregates of ~100 nm, causing superparamagnetic (SP) behavior that tails into the stable single-domain (SSD) range. For some samples, the SIRM was thermally demagnetized in a TD48 (ASC Scientific) furnace. we obtained detailed IRM acquisition curves with 46 steps up to 2.0 T and applied unmixing with log-normal distributions using the MAX UnMix routine of Maxbauer et al. (2016). Datasets are ready for acquisition curves modeling. TEM results and frequency dependence &#xAB55;(f) suggest partial disintegration of the aggregates and increased alteration of the nanoparticles during the transfer of red soil material to CL. we subjected ten samples to citrate-bicarbonate-dithionite (CBD) treatment, which removes fine iron oxide particles in the samples (Hunt et al., 1995). X-ray diffraction (XRD) analysis of the magnetic extracts was performed, data for figure plotting and model setups are available in these datasets. </description><subject>Lake Sediment</subject><subject>Catchment</subject><subject>Magnetite</subject><contributor>Appel, Erwin</contributor><contributor>Hu, Shouyun</contributor><contributor>Pennington, Robert</contributor><contributor>Meyer, Jannik</contributor><contributor>Neumann, Udo</contributor><contributor>Burchard, Michael</contributor><contributor>Allstaedt, Frederik</contributor><type>Other:Dataset</type><identifier>10.17632/m4gvh8p4cf.1</identifier><rights>Creative Commons Attribution 4.0 International</rights><rights>http://creativecommons.org/licenses/by/4.0</rights><relation>https:/data.mendeley.com/datasets/m4gvh8p4cf</relation><date>2020-02-20T08:47:06Z</date><date>2020-05-20T00:00:00Z</date><recordID>0.17632-m4gvh8p4cf.1</recordID></dc>
format Other:Dataset
Other
author Zhang, Qi
author2 Appel, Erwin
Hu, Shouyun
Pennington, Robert
Meyer, Jannik
Neumann, Udo
Burchard, Michael
Allstaedt, Frederik
title Nano-magnetite aggregates in red soil on low magnetic bedrock
publisher Mendeley
publishDate 2020
topic Lake Sediment
Catchment
Magnetite
url https:/data.mendeley.com/datasets/m4gvh8p4cf
contents This Dataset includes supporting materials for a paper that is submitted to JGR-Solid Earth. Soil and lake sediments are important paleoclimate archives and the sediments are often related to soil input. To better understand such settings, we studied the magnetic properties of red soil, its low-magnetic bedrock, and sub-recent sediments of Caohai Lake (CL) in Heqing Basin (HB), China. Red soil is highly magnetic with susceptibilities (ꭕ) of ~10-5 m3/kg, dominated by pedogenic nano-magnetite (~10-15 nm) arranged in aggregates of ~100 nm, causing superparamagnetic (SP) behavior that tails into the stable single-domain (SSD) range. For some samples, the SIRM was thermally demagnetized in a TD48 (ASC Scientific) furnace. we obtained detailed IRM acquisition curves with 46 steps up to 2.0 T and applied unmixing with log-normal distributions using the MAX UnMix routine of Maxbauer et al. (2016). Datasets are ready for acquisition curves modeling. TEM results and frequency dependence ꭕ(f) suggest partial disintegration of the aggregates and increased alteration of the nanoparticles during the transfer of red soil material to CL. we subjected ten samples to citrate-bicarbonate-dithionite (CBD) treatment, which removes fine iron oxide particles in the samples (Hunt et al., 1995). X-ray diffraction (XRD) analysis of the magnetic extracts was performed, data for figure plotting and model setups are available in these datasets.
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institution Universitas Islam Indragiri
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library Teknologi Pangan UNISI
library_id 2816
collection Artikel mulono
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city INDRAGIRI HILIR
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repoId IOS7969
first_indexed 2020-04-08T08:17:08Z
last_indexed 2020-04-08T08:17:08Z
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