Geochemical processes at a fresh/seawater interface in a shallow sandy aquifer

Martin Søgaard Andersen, Vibeke Margrethe Nyvang Iversen, Diederik Jan Postma

    Research output: Chapter in Book/Report/Conference proceedingConference abstract in proceedingsResearch

    Abstract

    Chemical processes in a natural fresh-/seawater mixing zone were studied in a shallow sandy aquifer. The dominant redox-processes are sulfate reduction and methanogenesis. Methanogenesis produces CO2, which causes calcite dissolution. The produced calcium induces ion exchange with sodium. The final result of these interactions between different types of geochemical processes is an anoxic groundwater enriched in bicarbonate and sodium.
    Original languageEnglish
    Title of host publicationInternational Conference on Saltwater Intrusion and Coastal Aquifers Monitoring, Modelling, and Management. : Proceedings
    VolumeCD-ROM
    Place of PublicationEssaouira, Morocco
    PublisherSWICA
    Publication date2001
    Publication statusPublished - 2001
    EventInternational Conference on Saltwater Intrusion and Coastal Aquifers Monitoring, Modelling, and Management. - Essaouira, Morocco
    Duration: 1 Jan 2001 → …
    Conference number: 1

    Conference

    ConferenceInternational Conference on Saltwater Intrusion and Coastal Aquifers Monitoring, Modelling, and Management.
    Number1
    CityEssaouira, Morocco
    Period01/01/2001 → …

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