Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation

Offshore freshened groundwater (OFG) has been documented in many continental margins worldwide. OFG systems are dynamic, expanding and contracting with falling and rise sea-levels. OFG has long been thought to be an important geomorphic agent in continental margins, either via active discharge at th...

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Main Authors: Saadatkhah, Nader, Kassim, Azman, Siat, Qurratu Aini, Micallef, Aaron
Format: Article
Language:English
Published: Elsevier B.V. 2023
Subjects:
Online Access:http://eprints.utm.my/105442/1/AzmanKassim2023_SaltLeachingbyFreshwateranditsImpact.pdf
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author Saadatkhah, Nader
Kassim, Azman
Siat, Qurratu Aini
Micallef, Aaron
author_facet Saadatkhah, Nader
Kassim, Azman
Siat, Qurratu Aini
Micallef, Aaron
author_sort Saadatkhah, Nader
collection ePrints
description Offshore freshened groundwater (OFG) has been documented in many continental margins worldwide. OFG systems are dynamic, expanding and contracting with falling and rise sea-levels. OFG has long been thought to be an important geomorphic agent in continental margins, either via active discharge at the seafloor, which can erode depressions, or the generation of excess pore pressure, which can deform sediments and cause slope failure. It has also been proposed that OFG flow can drive the loss of sediment shear strength via salt leaching, when seawater in pores is replaced by freshwater. Here, we measure changes in the geotechnical properties of seafloor clayey silt due to salt leaching using flushing experiments, and assess the implications of these changes on the stability of siliciclastic continental margins with 2D limit equilibrium modelling. We document a ∼ 50% decrease in undrained cohesive strength of seafloor sediment after flushing, as well as a decrease in its shear strength, bulk density, and moisture content, which is similar to that reported for subaerial quick clays undergoing salt leaching. When applied to a theoretical submarine domain 300 m wide by 100 m high, we estimate that salt leaching can trigger slope failure when the thickness of the flushed layer is >3.5 m or when the slope gradient is >3°. Such conditions are primarily satisfied on the continental slope or the shallow seafloor close to the shoreline. Salt leaching by OFG flow merits consideration as a potential mechanism destablising submarine sedimentary slopes.
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spelling utm.eprints-1054422024-04-30T07:17:29Z http://eprints.utm.my/105442/ Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation Saadatkhah, Nader Kassim, Azman Siat, Qurratu Aini Micallef, Aaron TA Engineering (General). Civil engineering (General) Offshore freshened groundwater (OFG) has been documented in many continental margins worldwide. OFG systems are dynamic, expanding and contracting with falling and rise sea-levels. OFG has long been thought to be an important geomorphic agent in continental margins, either via active discharge at the seafloor, which can erode depressions, or the generation of excess pore pressure, which can deform sediments and cause slope failure. It has also been proposed that OFG flow can drive the loss of sediment shear strength via salt leaching, when seawater in pores is replaced by freshwater. Here, we measure changes in the geotechnical properties of seafloor clayey silt due to salt leaching using flushing experiments, and assess the implications of these changes on the stability of siliciclastic continental margins with 2D limit equilibrium modelling. We document a ∼ 50% decrease in undrained cohesive strength of seafloor sediment after flushing, as well as a decrease in its shear strength, bulk density, and moisture content, which is similar to that reported for subaerial quick clays undergoing salt leaching. When applied to a theoretical submarine domain 300 m wide by 100 m high, we estimate that salt leaching can trigger slope failure when the thickness of the flushed layer is >3.5 m or when the slope gradient is >3°. Such conditions are primarily satisfied on the continental slope or the shallow seafloor close to the shoreline. Salt leaching by OFG flow merits consideration as a potential mechanism destablising submarine sedimentary slopes. Elsevier B.V. 2023-01 Article PeerReviewed application/pdf en http://eprints.utm.my/105442/1/AzmanKassim2023_SaltLeachingbyFreshwateranditsImpact.pdf Saadatkhah, Nader and Kassim, Azman and Siat, Qurratu Aini and Micallef, Aaron (2023) Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation. Marine Geology, 455 (NA). pp. 1-10. ISSN 0025-3227 http://dx.doi.org/10.1016/j.margeo.2022.106959 DOI:10.1016/j.margeo.2022.106959
spellingShingle TA Engineering (General). Civil engineering (General)
Saadatkhah, Nader
Kassim, Azman
Siat, Qurratu Aini
Micallef, Aaron
Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation
title Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation
title_full Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation
title_fullStr Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation
title_full_unstemmed Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation
title_short Salt leaching by freshwater and its impact on seafloor stability: an experimental investigation
title_sort salt leaching by freshwater and its impact on seafloor stability an experimental investigation
topic TA Engineering (General). Civil engineering (General)
url http://eprints.utm.my/105442/1/AzmanKassim2023_SaltLeachingbyFreshwateranditsImpact.pdf
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AT kassimazman saltleachingbyfreshwateranditsimpactonseafloorstabilityanexperimentalinvestigation
AT siatqurratuaini saltleachingbyfreshwateranditsimpactonseafloorstabilityanexperimentalinvestigation
AT micallefaaron saltleachingbyfreshwateranditsimpactonseafloorstabilityanexperimentalinvestigation