Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate

Sediment profiling imaging (SPI) is a versatile and widely used method to visually assess the quality of seafloor habitats (e.g., around fish farms and oil and gas rigs) and has been developed and used by both academics and consultancy companies over the last 50 years. Previous research has shown th...

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Main Authors: Annabell Moser, Iain Pheasant, William N. MacPherson, Bhavani E. Narayanaswamy, Andrew K. Sweetman
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-04-01
Series:Frontiers in Marine Science
Subjects:
SPI
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2021.582076/full
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spelling doaj-05c2a46764df482e955814f5e139c8992021-04-20T05:26:03ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452021-04-01810.3389/fmars.2021.582076582076Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating PlateAnnabell Moser0Iain Pheasant1William N. MacPherson2Bhavani E. Narayanaswamy3Andrew K. Sweetman4Deep-Sea Ecology and Biogeochemistry Research Group, Lyell Centre for Earth and Marine Science and Technology, Heriot-Watt University, Edinburgh, United KingdomBritish Geological Survey (BGS) Scotland, Lyell Centre, Edinburgh, United KingdomSchool of Engineering and Physical Sciences, Heriot-Watt University, Edinburgh, United KingdomThe Scottish Association for Marine Science, Scottish Marine Institute, Oban, United KingdomDeep-Sea Ecology and Biogeochemistry Research Group, Lyell Centre for Earth and Marine Science and Technology, Heriot-Watt University, Edinburgh, United KingdomSediment profiling imaging (SPI) is a versatile and widely used method to visually assess the quality of seafloor habitats (e.g., around fish farms and oil and gas rigs) and has been developed and used by both academics and consultancy companies over the last 50 years. Previous research has shown that inserting the flat viewport of an SPI camera into the sediment can have an impact on particle displacement pushing oxygenated surface sediments to deeper sediment depths and making anthropogenically-disturbed sediment appear healthier than they may actually be. To investigate the particle displacement that occurs when a flat plate is inserted into seafloor sediments, a testing device, termed the SPI purpose-built sediment chamber (SPI-PUSH) was designed and used in a series of experiments to quantify smearing where luminophores were used to demonstrate the extent of particle displacement caused by a flat plate being pushed into the sediment. Here, we show that the plate of the SPI-PUSH caused significant smearing, which varied with sediment type and the luminophore grain size. The mean particle smearing measured directly behind the inserted plate was 2.9 ± 1.5 cm for mud sediments with sand-like luminophores, 4.3 ± 2.5 cm for fine sand sediments with sand-like luminophores and 1.9 ± 1.1 cm for medium sand sediments with mud-like luminophores. When the mean depth of particle smearing was averaged over a larger sediment volume (11 cm3) next to the inserted plate, substantial differences were seen between the plate-insertion experiments and controls highlighting the potential extent of smearing artefacts that may be produced when a SPI camera penetrates the seafloor. This experimental data shows that future studies using the SPI camera, or any other periscope-like device (e.g., planar optodes) need to acknowledge that smearing may be significant. Furthermore, it highlights that a correction factor may need to be applied to these data (e.g., the depth of apparent redox potential discontinuity layer) to correctly interpret SPI camera images and better determine the effect of anthropogenic impacts on seafloor habitats.https://www.frontiersin.org/articles/10.3389/fmars.2021.582076/fullsediment profile imagingsedimentSPIsmearingparticle displacementaRPD
collection DOAJ
language English
format Article
sources DOAJ
author Annabell Moser
Iain Pheasant
William N. MacPherson
Bhavani E. Narayanaswamy
Andrew K. Sweetman
spellingShingle Annabell Moser
Iain Pheasant
William N. MacPherson
Bhavani E. Narayanaswamy
Andrew K. Sweetman
Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate
Frontiers in Marine Science
sediment profile imaging
sediment
SPI
smearing
particle displacement
aRPD
author_facet Annabell Moser
Iain Pheasant
William N. MacPherson
Bhavani E. Narayanaswamy
Andrew K. Sweetman
author_sort Annabell Moser
title Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate
title_short Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate
title_full Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate
title_fullStr Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate
title_full_unstemmed Sediment Profile Imaging: Laboratory Study Into the Sediment Smearing Effect of a Penetrating Plate
title_sort sediment profile imaging: laboratory study into the sediment smearing effect of a penetrating plate
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2021-04-01
description Sediment profiling imaging (SPI) is a versatile and widely used method to visually assess the quality of seafloor habitats (e.g., around fish farms and oil and gas rigs) and has been developed and used by both academics and consultancy companies over the last 50 years. Previous research has shown that inserting the flat viewport of an SPI camera into the sediment can have an impact on particle displacement pushing oxygenated surface sediments to deeper sediment depths and making anthropogenically-disturbed sediment appear healthier than they may actually be. To investigate the particle displacement that occurs when a flat plate is inserted into seafloor sediments, a testing device, termed the SPI purpose-built sediment chamber (SPI-PUSH) was designed and used in a series of experiments to quantify smearing where luminophores were used to demonstrate the extent of particle displacement caused by a flat plate being pushed into the sediment. Here, we show that the plate of the SPI-PUSH caused significant smearing, which varied with sediment type and the luminophore grain size. The mean particle smearing measured directly behind the inserted plate was 2.9 ± 1.5 cm for mud sediments with sand-like luminophores, 4.3 ± 2.5 cm for fine sand sediments with sand-like luminophores and 1.9 ± 1.1 cm for medium sand sediments with mud-like luminophores. When the mean depth of particle smearing was averaged over a larger sediment volume (11 cm3) next to the inserted plate, substantial differences were seen between the plate-insertion experiments and controls highlighting the potential extent of smearing artefacts that may be produced when a SPI camera penetrates the seafloor. This experimental data shows that future studies using the SPI camera, or any other periscope-like device (e.g., planar optodes) need to acknowledge that smearing may be significant. Furthermore, it highlights that a correction factor may need to be applied to these data (e.g., the depth of apparent redox potential discontinuity layer) to correctly interpret SPI camera images and better determine the effect of anthropogenic impacts on seafloor habitats.
topic sediment profile imaging
sediment
SPI
smearing
particle displacement
aRPD
url https://www.frontiersin.org/articles/10.3389/fmars.2021.582076/full
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