Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy

The weight percentage and mean size of the 10–63 μm terrigenous silt fraction (termed ‘sortable silt’) of fine-grained marine sediments have recently been argued to be proxies for near-bottom palaeocurrent intensity. This paper details the accuracy and precision of the Sedigraph 5100 and the Coulter...

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Published in:Sedimentology
Main Authors: Bianchi, G. G., Hall, Ian Robert, McCave, I. N., Joseph, L.
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley-Blackwell 1999
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/30543/
https://doi.org/10.1046/j.1365-3091.1999.00256.x
id ftunivcardiff:oai:https://orca.cardiff.ac.uk:30543
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spelling ftunivcardiff:oai:https://orca.cardiff.ac.uk:30543 2023-05-15T16:51:21+02:00 Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy Bianchi, G. G. Hall, Ian Robert McCave, I. N. Joseph, L. 1999-12 https://orca.cardiff.ac.uk/id/eprint/30543/ https://doi.org/10.1046/j.1365-3091.1999.00256.x unknown Wiley-Blackwell Bianchi, G. G., Hall, Ian Robert https://orca.cardiff.ac.uk/view/cardiffauthors/A002402L.html orcid:0000-0001-6960-1419 orcid:0000-0001-6960-1419, McCave, I. N. and Joseph, L. 1999. Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy. Sedimentology 46 (6) , pp. 1001-1014. 10.1046/j.1365-3091.1999.00256.x https://doi.org/10.1046/j.1365-3091.1999.00256.x doi:10.1046/j.1365-3091.1999.00256.x GC Oceanography Article PeerReviewed 1999 ftunivcardiff https://doi.org/10.1046/j.1365-3091.1999.00256.x 2022-10-20T22:40:33Z The weight percentage and mean size of the 10–63 μm terrigenous silt fraction (termed ‘sortable silt’) of fine-grained marine sediments have recently been argued to be proxies for near-bottom palaeocurrent intensity. This paper details the accuracy and precision of the Sedigraph 5100 and the Coulter Multisizer IIe in determining the weight percentage and mean size of the sortable silt at abundances characteristic of deep-ocean sediments. Three sortable silt standards and a fine silt/clay diluent were generated from natural deep-sea sediment of the Iceland Basin. These were used to produce silty clays with standard additions of sortable silt ranging from 1% to 20% of the total by weight. Accuracy was measured relative to the size of the pure spike measured by each instrument. At sortable silt abundance >5%, the Sedigraph and the Coulter Multisizer estimate both weight percentage and mean grain size precisely and accurately, while below 5%, instrumental noise degrades their performance. On the basis of the Sedigraph results, a series of percentage errors is defined, which may be applied to sortable silt mean size and weight percentage estimates used in palaeoceanographic near-bottom current reconstruction. It is suggested that, ideally, palaeocurrent reconstructions should be based on Sedigraph determinations of the 0–63 μm grain size distribution, yielding both mean and abundance, or on Coulter Multisizer determinations of the sortable silt grain size mean. The Coulter Multisizer may prove especially useful in regions of very depleted (<5%) sortable silt component. Article in Journal/Newspaper Iceland Cardiff University: ORCA (Online Research @ Cardiff) Coulter ENVELOPE(-58.033,-58.033,-83.283,-83.283) Sedimentology 46 6 1001 1014
institution Open Polar
collection Cardiff University: ORCA (Online Research @ Cardiff)
op_collection_id ftunivcardiff
language unknown
topic GC Oceanography
spellingShingle GC Oceanography
Bianchi, G. G.
Hall, Ian Robert
McCave, I. N.
Joseph, L.
Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy
topic_facet GC Oceanography
description The weight percentage and mean size of the 10–63 μm terrigenous silt fraction (termed ‘sortable silt’) of fine-grained marine sediments have recently been argued to be proxies for near-bottom palaeocurrent intensity. This paper details the accuracy and precision of the Sedigraph 5100 and the Coulter Multisizer IIe in determining the weight percentage and mean size of the sortable silt at abundances characteristic of deep-ocean sediments. Three sortable silt standards and a fine silt/clay diluent were generated from natural deep-sea sediment of the Iceland Basin. These were used to produce silty clays with standard additions of sortable silt ranging from 1% to 20% of the total by weight. Accuracy was measured relative to the size of the pure spike measured by each instrument. At sortable silt abundance >5%, the Sedigraph and the Coulter Multisizer estimate both weight percentage and mean grain size precisely and accurately, while below 5%, instrumental noise degrades their performance. On the basis of the Sedigraph results, a series of percentage errors is defined, which may be applied to sortable silt mean size and weight percentage estimates used in palaeoceanographic near-bottom current reconstruction. It is suggested that, ideally, palaeocurrent reconstructions should be based on Sedigraph determinations of the 0–63 μm grain size distribution, yielding both mean and abundance, or on Coulter Multisizer determinations of the sortable silt grain size mean. The Coulter Multisizer may prove especially useful in regions of very depleted (<5%) sortable silt component.
format Article in Journal/Newspaper
author Bianchi, G. G.
Hall, Ian Robert
McCave, I. N.
Joseph, L.
author_facet Bianchi, G. G.
Hall, Ian Robert
McCave, I. N.
Joseph, L.
author_sort Bianchi, G. G.
title Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy
title_short Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy
title_full Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy
title_fullStr Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy
title_full_unstemmed Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy
title_sort measurement of the sortable silt current speed proxy using the sedigraph 5100 and coulter multisizer iie: precision and accuracy
publisher Wiley-Blackwell
publishDate 1999
url https://orca.cardiff.ac.uk/id/eprint/30543/
https://doi.org/10.1046/j.1365-3091.1999.00256.x
long_lat ENVELOPE(-58.033,-58.033,-83.283,-83.283)
geographic Coulter
geographic_facet Coulter
genre Iceland
genre_facet Iceland
op_relation Bianchi, G. G., Hall, Ian Robert https://orca.cardiff.ac.uk/view/cardiffauthors/A002402L.html orcid:0000-0001-6960-1419 orcid:0000-0001-6960-1419, McCave, I. N. and Joseph, L. 1999. Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy. Sedimentology 46 (6) , pp. 1001-1014. 10.1046/j.1365-3091.1999.00256.x https://doi.org/10.1046/j.1365-3091.1999.00256.x
doi:10.1046/j.1365-3091.1999.00256.x
op_doi https://doi.org/10.1046/j.1365-3091.1999.00256.x
container_title Sedimentology
container_volume 46
container_issue 6
container_start_page 1001
op_container_end_page 1014
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