Different continuous freshwater contributions to submarine groundwater discharge at a coastal peatland, southern Baltic Sea
The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contr...
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| Published in | Isotopes in environmental and health studies Vol. 61; no. 1; pp. 42 - 60 |
|---|---|
| Main Authors | , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
England
Taylor & Francis
02.01.2025
Taylor & Francis Ltd |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1025-6016 1477-2639 1477-2639 |
| DOI | 10.1080/10256016.2024.2422864 |
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| Abstract | The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ
2
H, δ
18
O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.
The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium-helium (
3
H-
3
He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land-ocean continuum in times of current climate change. |
|---|---|
| AbstractList | The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ
2
H, δ
18
O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.
The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium-helium (
3
H-
3
He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land-ocean continuum in times of current climate change. The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ2H, δ18O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium–helium (3H–3He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land–ocean continuum in times of current climate change. The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ ²H, δ ¹⁸O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period. The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium–helium (³H–³He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land–ocean continuum in times of current climate change. The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope ( H, O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium-helium ( H- He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land-ocean continuum in times of current climate change. The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ2H, δ18O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium-helium (3H-3He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land-ocean continuum in times of current climate change.The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ2H, δ18O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium-helium (3H-3He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land-ocean continuum in times of current climate change. |
| Author | Böttcher, Michael Ernst Ehlert von Ahn, Cátia M. Roeser, Patricia Schmiedinger, Iris Saban, Rhodelyn Sültenfuß, Jürgen Jenner, Anna-Kathrina Reckhardt, Anja |
| Author_xml | – sequence: 1 givenname: Anna-Kathrina orcidid: 0009-0007-8876-0942 surname: Jenner fullname: Jenner, Anna-Kathrina organization: Leibniz Institute for Baltic Sea Research – sequence: 2 givenname: Rhodelyn orcidid: 0009-0007-0660-9270 surname: Saban fullname: Saban, Rhodelyn organization: Leibniz Institute for Baltic Sea Research – sequence: 3 givenname: Cátia M. orcidid: 0000-0001-7524-5908 surname: Ehlert von Ahn fullname: Ehlert von Ahn, Cátia M. organization: Leibniz Institute for Baltic Sea Research – sequence: 4 givenname: Patricia orcidid: 0000-0002-5604-1827 surname: Roeser fullname: Roeser, Patricia organization: Leibniz Institute for Baltic Sea Research – sequence: 5 givenname: Iris surname: Schmiedinger fullname: Schmiedinger, Iris organization: Leibniz Institute for Baltic Sea Research – sequence: 6 givenname: Jürgen orcidid: 0000-0003-3169-0422 surname: Sültenfuß fullname: Sültenfuß, Jürgen organization: University of Bremen – sequence: 7 givenname: Anja orcidid: 0000-0002-7079-5895 surname: Reckhardt fullname: Reckhardt, Anja organization: Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky Universität Oldenburg – sequence: 8 givenname: Michael Ernst orcidid: 0000-0002-8877-0303 surname: Böttcher fullname: Böttcher, Michael Ernst email: michael.boettcher@io-warnemuende.de, dermeboe@proton.me organization: University of Rostock |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/39527094$$D View this record in MEDLINE/PubMed |
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| Keywords | groundwater dating coastline hydrochemistry water isotopes long-term observation porewater temperate climate Peatland Submarine groundwater discharge Baltic Sea |
| Language | English |
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| Snippet | The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate... |
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| SubjectTerms | Baltic Sea Biogeochemistry Climate change Coastal waters coastline coasts Deuterium - analysis Discharge Environmental Monitoring Estuaries Fresh water Fresh Water - analysis Fresh Water - chemistry freshwater Geologic Sediments - analysis Geologic Sediments - chemistry Groundwater Groundwater - analysis Groundwater - chemistry groundwater dating Groundwater discharge Groundwater runoff Helium hydrochemistry Hydrology Isotope composition Lances long-term observation North Sea Oxygen Isotopes - analysis Peatland Peatlands Pore water porewater River flow rivers Runoff Salinity Salinity effects Seawater - analysis Seawater - chemistry sediments Stable isotopes Submarine groundwater discharge Surface runoff Surface water Surface-groundwater relations temperate climate Tritium water isotopes Water Movements |
| Title | Different continuous freshwater contributions to submarine groundwater discharge at a coastal peatland, southern Baltic Sea |
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