Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean

The abyssal seafloor in the Clarion-Clipperton Zone (CCZ) in the NE Pacific hosts the largest abundance of polymetallic nodules in the deep sea and is being targeted as an area for potential deep-sea mining. During nodule mining, seafloor sediment will be brought into suspension by mining equipment,...

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Main Authors: Sabine Haalboom, Timm Schoening, Peter Urban, Iason-Zois Gazis, Henko de Stigter, Benjamin Gillard, Matthias Baeye, Martina Hollstein, Kaveh Purkiani, Gert-Jan Reichart, Laurenz Thomsen, Matthias Haeckel, Annemiek Vink, Jens Greinert
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-06-01
Series:Frontiers in Marine Science
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Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.882155/full
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author Sabine Haalboom
Timm Schoening
Peter Urban
Iason-Zois Gazis
Henko de Stigter
Benjamin Gillard
Matthias Baeye
Martina Hollstein
Kaveh Purkiani
Gert-Jan Reichart
Gert-Jan Reichart
Laurenz Thomsen
Matthias Haeckel
Annemiek Vink
Jens Greinert
Jens Greinert
author_facet Sabine Haalboom
Timm Schoening
Peter Urban
Iason-Zois Gazis
Henko de Stigter
Benjamin Gillard
Matthias Baeye
Martina Hollstein
Kaveh Purkiani
Gert-Jan Reichart
Gert-Jan Reichart
Laurenz Thomsen
Matthias Haeckel
Annemiek Vink
Jens Greinert
Jens Greinert
author_sort Sabine Haalboom
collection DOAJ
description The abyssal seafloor in the Clarion-Clipperton Zone (CCZ) in the NE Pacific hosts the largest abundance of polymetallic nodules in the deep sea and is being targeted as an area for potential deep-sea mining. During nodule mining, seafloor sediment will be brought into suspension by mining equipment, resulting in the formation of sediment plumes, which will affect benthic and pelagic life not naturally adapted to any major sediment transport and deposition events. To improve our understanding of sediment plume dispersion and to support the development of plume dispersion models in this specific deep-sea area, we conducted a small-scale, 12-hour disturbance experiment in the German exploration contract area in the CCZ using a chain dredge. Sediment plume dispersion and deposition was monitored using an array of optical and acoustic turbidity sensors and current meters placed on platforms on the seafloor, and by visual inspection of the seafloor before and after dredge deployment. We found that seafloor imagery could be used to qualitatively visualise the redeposited sediment up to a distance of 100 m from the source, and that sensors recording optical and acoustic backscatter are sensitive and adequate tools to monitor the horizontal and vertical dispersion of the generated sediment plume. Optical backscatter signals could be converted into absolute mass concentration of suspended sediment to provide quantitative data on sediment dispersion. Vertical profiles of acoustic backscatter recorded by current profilers provided qualitative insight into the vertical extent of the sediment plume. Our monitoring setup proved to be very useful for the monitoring of this small-scale experiment and can be seen as an exemplary strategy for monitoring studies of future, upscaled mining trials. We recommend that such larger trials include the use of AUVs for repeated seafloor imaging and water column plume mapping (optical and acoustical), as well as the use of in-situ particle size sensors and/or particle cameras to better constrain the effect of suspended particle aggregation on optical and acoustic backscatter signals.
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spelling doaj.art-7d743ad247de40868df2a528116ddc002022-12-22T02:31:39ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-06-01910.3389/fmars.2022.882155882155Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific OceanSabine Haalboom0Timm Schoening1Peter Urban2Iason-Zois Gazis3Henko de Stigter4Benjamin Gillard5Matthias Baeye6Martina Hollstein7Kaveh Purkiani8Gert-Jan Reichart9Gert-Jan Reichart10Laurenz Thomsen11Matthias Haeckel12Annemiek Vink13Jens Greinert14Jens Greinert15Department of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research, Texel, NetherlandsGEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, GermanyGEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, GermanyGEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, GermanyDepartment of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research, Texel, NetherlandsJacobs University, Bremen, GermanyRoyal Belgian Institute of Natural Sciences, Brussels, BelgiumBundesanstalt für Geowissenschaften und Rohstoffe (BGR), Hannover, GermanyMARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, GermanyDepartment of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research, Texel, NetherlandsFaculty of Geosciences, Utrecht University, Utrecht, NetherlandsJacobs University, Bremen, GermanyGEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, GermanyBundesanstalt für Geowissenschaften und Rohstoffe (BGR), Hannover, GermanyGEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, GermanyChristian-Albrechts University Kiel, Kiel, GermanyThe abyssal seafloor in the Clarion-Clipperton Zone (CCZ) in the NE Pacific hosts the largest abundance of polymetallic nodules in the deep sea and is being targeted as an area for potential deep-sea mining. During nodule mining, seafloor sediment will be brought into suspension by mining equipment, resulting in the formation of sediment plumes, which will affect benthic and pelagic life not naturally adapted to any major sediment transport and deposition events. To improve our understanding of sediment plume dispersion and to support the development of plume dispersion models in this specific deep-sea area, we conducted a small-scale, 12-hour disturbance experiment in the German exploration contract area in the CCZ using a chain dredge. Sediment plume dispersion and deposition was monitored using an array of optical and acoustic turbidity sensors and current meters placed on platforms on the seafloor, and by visual inspection of the seafloor before and after dredge deployment. We found that seafloor imagery could be used to qualitatively visualise the redeposited sediment up to a distance of 100 m from the source, and that sensors recording optical and acoustic backscatter are sensitive and adequate tools to monitor the horizontal and vertical dispersion of the generated sediment plume. Optical backscatter signals could be converted into absolute mass concentration of suspended sediment to provide quantitative data on sediment dispersion. Vertical profiles of acoustic backscatter recorded by current profilers provided qualitative insight into the vertical extent of the sediment plume. Our monitoring setup proved to be very useful for the monitoring of this small-scale experiment and can be seen as an exemplary strategy for monitoring studies of future, upscaled mining trials. We recommend that such larger trials include the use of AUVs for repeated seafloor imaging and water column plume mapping (optical and acoustical), as well as the use of in-situ particle size sensors and/or particle cameras to better constrain the effect of suspended particle aggregation on optical and acoustic backscatter signals.https://www.frontiersin.org/articles/10.3389/fmars.2022.882155/fullClarion-Clipperton Zone (CCZ)deep-sea miningpolymetallic nodulessediment plumeplume monitoringdredge experiment
spellingShingle Sabine Haalboom
Timm Schoening
Peter Urban
Iason-Zois Gazis
Henko de Stigter
Benjamin Gillard
Matthias Baeye
Martina Hollstein
Kaveh Purkiani
Gert-Jan Reichart
Gert-Jan Reichart
Laurenz Thomsen
Matthias Haeckel
Annemiek Vink
Jens Greinert
Jens Greinert
Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean
Frontiers in Marine Science
Clarion-Clipperton Zone (CCZ)
deep-sea mining
polymetallic nodules
sediment plume
plume monitoring
dredge experiment
title Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean
title_full Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean
title_fullStr Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean
title_full_unstemmed Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean
title_short Monitoring of Anthropogenic Sediment Plumes in the Clarion-Clipperton Zone, NE Equatorial Pacific Ocean
title_sort monitoring of anthropogenic sediment plumes in the clarion clipperton zone ne equatorial pacific ocean
topic Clarion-Clipperton Zone (CCZ)
deep-sea mining
polymetallic nodules
sediment plume
plume monitoring
dredge experiment
url https://www.frontiersin.org/articles/10.3389/fmars.2022.882155/full
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