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Combined uncertainty estimation for the determination of the dissolved iron amount content in seawater using flow injection with chemiluminescence detection

Combined uncertainty estimation for the determination of the dissolved iron amount content in seawater using flow injection with chemiluminescence detection
Combined uncertainty estimation for the determination of the dissolved iron amount content in seawater using flow injection with chemiluminescence detection

This work assesses the components contributing to the combined uncertainty budget associated with the measurement of the Fe amount content by flow injection chemiluminescence (FI-CL) in <0.2 μm filtered and acidified seawater samples. Amounts of loaded standard solutions and samples were determined gravimetrically by differential weighing. Up to 5% variations in the loaded masses were observed during measurements, in contradiction to the usual assumptions made when operating under constant loading time conditions. Hence signal intensities (V) were normalised to the loaded mass and plots of average normalised intensities (in V kg-1) vs. values of the Fe amount content (in nmol kg-1) added to a “low level” iron seawater matrix were used to produce the calibration graphs. The measurement procedure implemented and the uncertainty estimation process developed were validated from the agreement obtained with consensus values for three SAFe and GEOTRACES reference materials (D2, GS, and GD). Relative expanded uncertainties for peak height and peak area based results were estimated to be around 12% and 10% (coverage factor k 5 2), respectively. The most important contributory factors were the uncertainty on the sensitivity coefficient (i.e., calibration slope) and the within-sequence-stability (i.e., the signal stability over several hours of operation; here 32 h). For GD, using peak height measurements, these factors contributed respectively 69.7% and 21.6% while the short-term repeatability accounted for only 7.9%. Therefore, an uncertainty estimation based on the intensity repeatability alone, as is often done in FI-CL studies, is not a realistic estimation of the overall uncertainty of the procedure.

1541-5856
673-686
Floor, Geerke H.
4b3e2643-a4ad-48f2-bcb0-cdcd7e70ee47
Clough, Robert
3cd2d6d7-3b64-4192-b021-a71441e6222a
Lohan, Maeve C.
6ca10597-2d0f-40e8-8e4f-7619dfac5088
Ussher, Simon J.
089623db-1a7d-42b8-87d1-1f17395373b1
Worsfold, Paul J.
27675f89-7eee-45c5-821e-a381d8db9693
Quétel, Christophe R.
2bccf3ae-93d7-4a58-9126-27b51555f824
Floor, Geerke H.
4b3e2643-a4ad-48f2-bcb0-cdcd7e70ee47
Clough, Robert
3cd2d6d7-3b64-4192-b021-a71441e6222a
Lohan, Maeve C.
6ca10597-2d0f-40e8-8e4f-7619dfac5088
Ussher, Simon J.
089623db-1a7d-42b8-87d1-1f17395373b1
Worsfold, Paul J.
27675f89-7eee-45c5-821e-a381d8db9693
Quétel, Christophe R.
2bccf3ae-93d7-4a58-9126-27b51555f824

Floor, Geerke H., Clough, Robert, Lohan, Maeve C., Ussher, Simon J., Worsfold, Paul J. and Quétel, Christophe R. (2015) Combined uncertainty estimation for the determination of the dissolved iron amount content in seawater using flow injection with chemiluminescence detection. Limnology and Oceanography: Methods, 13 (12), 673-686. (doi:10.1002/lom3.10057).

Record type: Article

Abstract

This work assesses the components contributing to the combined uncertainty budget associated with the measurement of the Fe amount content by flow injection chemiluminescence (FI-CL) in <0.2 μm filtered and acidified seawater samples. Amounts of loaded standard solutions and samples were determined gravimetrically by differential weighing. Up to 5% variations in the loaded masses were observed during measurements, in contradiction to the usual assumptions made when operating under constant loading time conditions. Hence signal intensities (V) were normalised to the loaded mass and plots of average normalised intensities (in V kg-1) vs. values of the Fe amount content (in nmol kg-1) added to a “low level” iron seawater matrix were used to produce the calibration graphs. The measurement procedure implemented and the uncertainty estimation process developed were validated from the agreement obtained with consensus values for three SAFe and GEOTRACES reference materials (D2, GS, and GD). Relative expanded uncertainties for peak height and peak area based results were estimated to be around 12% and 10% (coverage factor k 5 2), respectively. The most important contributory factors were the uncertainty on the sensitivity coefficient (i.e., calibration slope) and the within-sequence-stability (i.e., the signal stability over several hours of operation; here 32 h). For GD, using peak height measurements, these factors contributed respectively 69.7% and 21.6% while the short-term repeatability accounted for only 7.9%. Therefore, an uncertainty estimation based on the intensity repeatability alone, as is often done in FI-CL studies, is not a realistic estimation of the overall uncertainty of the procedure.

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More information

Accepted/In Press date: 21 July 2015
e-pub ahead of print date: 18 September 2015
Published date: 1 December 2015

Identifiers

Local EPrints ID: 413749
URI: http://eprints.soton.ac.uk/id/eprint/413749
ISSN: 1541-5856
PURE UUID: 1391c42a-abeb-48a0-8577-9bc6c3db0d55
ORCID for Maeve C. Lohan: ORCID iD orcid.org/0000-0002-5340-3108

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Date deposited: 04 Sep 2017 16:30
Last modified: 16 Mar 2024 04:13

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Contributors

Author: Geerke H. Floor
Author: Robert Clough
Author: Maeve C. Lohan ORCID iD
Author: Simon J. Ussher
Author: Paul J. Worsfold
Author: Christophe R. Quétel

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