The Impacts of Loading From Acid Sulfate Soils on Boreal Estuarine Sediments

dc.contributor.authorDalhem, Krister
dc.contributor.authorKehusmaa, Karoliina
dc.contributor.authorVirtasalo, Joonas J.
dc.contributor.authorÅström, Mats
dc.contributor.authorÖsterholm, Peter
dc.contributor.organizationfi=geologia|en=Geology |
dc.contributor.organization-code1.2.246.10.2458963.20.72020864681
dc.converis.publication-id491739736
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/491739736
dc.date.accessioned2025-08-27T23:23:14Z
dc.date.available2025-08-27T23:23:14Z
dc.description.abstractEstuaries play a vital role in the coastal environment by filtering pollutants and nutrients from catchment runoff. In areas where acid sulfate (AS) soils are abundant, the importance of the estuary as a coastal filter is heightened as AS soils typically stress the marine environment with acidic metal-laden drainage waters. In this study, we took sediment cores from a shallow estuary in Western Finland and used geochemical and palaeoecological methods to investigate how the estuary is affected by loading from AS soils. An overall decrease in diatom species richness and diversity in the estuarine sediments was found, with a clear change from species preferring pelagic conditions to species indicative of more eutrophic conditions. The change coincides with human disturbance during the early 20th century when extensive drainage and rework of forests and peatlands into agricultural use increased. Geochemical analyses show a significant enrichment of Cd, Ni, Co, Zn and Al in the estuarine sediments which correspond to the metal loads originating from the catchment AS soils. Our calculations, however, show that in comparison to the total load of soluble metals from the catchment area, more than 80% of chalcophiles and 70% of Al are transported further out to sea. We hypothesised that a precipitation gradient driven by changes in pH and salinity due to seawater mixing would form along a transect towards the estuary outlet. Instead, we found that physical sedimentation processes are stronger drivers for element transport, as enrichment takes place only in low-energy hydrodynamic conditions at greater water depths. Glacioisostatic land uplift and significant particle transport from the catchment area are further isolating the estuary, effectively moving the saline gradient seawards and diminishing the role of the estuary as a coastal filter. We also found that the estuarine sediments are hypersulfidic and contain stores of potential acidity significantly larger than conventional AS soils. Without proper management, disturbance of the estuarine sediments can cause disastrous consequences at a local level.
dc.identifier.eissn1365-2389
dc.identifier.jour-issn1351-0754
dc.identifier.olddbid203893
dc.identifier.oldhandle10024/186920
dc.identifier.urihttps://www.utupub.fi/handle/11111/35326
dc.identifier.urlhttps://doi.org/10.1111/ejss.70075
dc.identifier.urnURN:NBN:fi-fe2025082790263
dc.language.isoen
dc.okm.affiliatedauthorKehusmaa, Karoliina
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherWILEY
dc.publisher.countryUnited Kingdomen_GB
dc.publisher.countryBritanniafi_FI
dc.publisher.country-codeGB
dc.publisher.placeHOBOKEN
dc.relation.articlenumbere70075
dc.relation.doi10.1111/ejss.70075
dc.relation.ispartofjournalEuropean Journal of Soil Science
dc.relation.issue2
dc.relation.volume76
dc.source.identifierhttps://www.utupub.fi/handle/10024/186920
dc.titleThe Impacts of Loading From Acid Sulfate Soils on Boreal Estuarine Sediments
dc.year.issued2025

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