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A new methodology for precise cadmium isotope analyses of seawater

A new methodology for precise cadmium isotope analyses of seawater
A new methodology for precise cadmium isotope analyses of seawater
Previous studies have revealed considerable Cd
isotope fractionations in seawater, which can be used to
study the marine cycling of this micronutrient element. The
low Cd concentrations that are commonly encountered in
nutrient-depleted surface seawater, however, pose a particular
challenge for precise Cd stable isotope analyses. In this
study, we have developed a new procedure for Cd isotope
analyses of seawater, which is suitable for samples as large
as 20 L and Cd concentrations as low as 1 pmol/L. The
procedure involves the use of a 111Cd–113Cd double spike,
co-precipitation of Cd from seawater using Al(OH)3, and
subsequent Cd purification by column chromatography. To
save time, seawater samples with higher Cd contents can be
processed without co-precipitation. The Cd isotope analyses
are carried out by multiple collector inductively coupled
plasma mass spectrometry (MC-ICP-MS). The performance
of this technique was verified by analyzing multiple
aliquots of a large seawater sample that was collected from
the English Channel, the SAFe D1 seawater reference
material, and several samples from the GEOTRACES
Atlantic intercalibration exercise. The overall Cd yield of
the procedure is consistently better than 85% and the
methodology can routinely provide ?114/110Cd data with a
precision of about ±0.5 ? (2sd, standard deviation) when at
least 20–30 ng of natural Cd is available for analysis.
However, even seawater samples with Cd contents of only
1–3 ng can be analyzed with a reproducibility of about ±3
to ±5 ?. A number of experiments were furthermore
conducted to verify that the isotopic results are accurate to within the quoted uncertainty.
Isotopes, Stable isotopes, Mass fractionation, Geochemistry, Marine geochemistry, Chemical oceanography
1618-2642
883-893
Xue, Zichen
6acfcf55-4fd3-432e-a051-66a1929b6dc0
Rehkämper, Mark
08591eef-a2d5-48de-9fc6-b5c0cf54f6e5
Schönbächler, Maria
57152b5e-5f2c-4119-ac26-c7db771ab9c1
Statham, Peter J.
51458f15-d6e2-4231-8bba-d0567f9e440c
Coles, Barry J.
01b0f38f-d584-4a79-af72-70c5ed4c928e
Xue, Zichen
6acfcf55-4fd3-432e-a051-66a1929b6dc0
Rehkämper, Mark
08591eef-a2d5-48de-9fc6-b5c0cf54f6e5
Schönbächler, Maria
57152b5e-5f2c-4119-ac26-c7db771ab9c1
Statham, Peter J.
51458f15-d6e2-4231-8bba-d0567f9e440c
Coles, Barry J.
01b0f38f-d584-4a79-af72-70c5ed4c928e

Xue, Zichen, Rehkämper, Mark, Schönbächler, Maria, Statham, Peter J. and Coles, Barry J. (2012) A new methodology for precise cadmium isotope analyses of seawater. Analytical and Bioanalytical Chemistry, 402 (2), 883-893. (doi:10.1007/s00216-011-5487-0).

Record type: Article

Abstract

Previous studies have revealed considerable Cd
isotope fractionations in seawater, which can be used to
study the marine cycling of this micronutrient element. The
low Cd concentrations that are commonly encountered in
nutrient-depleted surface seawater, however, pose a particular
challenge for precise Cd stable isotope analyses. In this
study, we have developed a new procedure for Cd isotope
analyses of seawater, which is suitable for samples as large
as 20 L and Cd concentrations as low as 1 pmol/L. The
procedure involves the use of a 111Cd–113Cd double spike,
co-precipitation of Cd from seawater using Al(OH)3, and
subsequent Cd purification by column chromatography. To
save time, seawater samples with higher Cd contents can be
processed without co-precipitation. The Cd isotope analyses
are carried out by multiple collector inductively coupled
plasma mass spectrometry (MC-ICP-MS). The performance
of this technique was verified by analyzing multiple
aliquots of a large seawater sample that was collected from
the English Channel, the SAFe D1 seawater reference
material, and several samples from the GEOTRACES
Atlantic intercalibration exercise. The overall Cd yield of
the procedure is consistently better than 85% and the
methodology can routinely provide ?114/110Cd data with a
precision of about ±0.5 ? (2sd, standard deviation) when at
least 20–30 ng of natural Cd is available for analysis.
However, even seawater samples with Cd contents of only
1–3 ng can be analyzed with a reproducibility of about ±3
to ±5 ?. A number of experiments were furthermore
conducted to verify that the isotopic results are accurate to within the quoted uncertainty.

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More information

Published date: 2012
Keywords: Isotopes, Stable isotopes, Mass fractionation, Geochemistry, Marine geochemistry, Chemical oceanography
Organisations: Ocean Biochemistry & Ecosystems

Identifiers

Local EPrints ID: 210877
URI: http://eprints.soton.ac.uk/id/eprint/210877
ISSN: 1618-2642
PURE UUID: aa71aaf5-8d3f-48cb-84da-dc06bd5ee1c1

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Date deposited: 10 Feb 2012 11:57
Last modified: 14 Mar 2024 04:50

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Contributors

Author: Zichen Xue
Author: Mark Rehkämper
Author: Maria Schönbächler
Author: Barry J. Coles

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