Research article Special Issues

Characterization of the Kringelmomyra peatland: geotechnical, hydrogeological, and ecological aspects

  • Received: 17 February 2025 Revised: 30 June 2025 Accepted: 09 June 2025 Published: 12 August 2025
  • Peats are abundant in the Northern Hemisphere and tropics, yet soil mechanics traditionally emphasize sands, clays, and silts, often overlooking peats. Despite this, engineering challenges related to peats, such as differential settlements and landslides, impact society. Understanding peat behavior is crucial for addressing modern issues like infrastructure resilience, CO2 emissions, and climate change adaptation, and for developing less intrusive construction methods that reduce peatland degradation. Kringelmomyra is a peatland in northern Norway where the surcharging method is being used to construct a new highway. This paper presents its geotechnical, hydrogeological, and ecological characteristics, initial quantitative data on potential changes in hydrogeology, and the remaining plant biodiversity resulting from road construction. Geotechnical testing and hydrogeological monitoring reveal complex peat stratification and minimal initial hydrogeological impact. The endangered peat moss Sphagnum venustum was found at the site, highlighting the need to monitor the impact at the site in the coming years. Continued interdisciplinary monitoring is essential to understand long-term effects and ensure sustainable construction practices on peatlands.

    Citation: Priscilla Paniagua, Bjørn Kristian Fiskvik Bache, Simon Ross Stenger, Magni Olsen Kyrkjeeide, Elin Johanne Slettum, Michael Long. Characterization of the Kringelmomyra peatland: geotechnical, hydrogeological, and ecological aspects[J]. AIMS Geosciences, 2025, 11(3): 686-703. doi: 10.3934/geosci.2025029

    Related Papers:

  • Peats are abundant in the Northern Hemisphere and tropics, yet soil mechanics traditionally emphasize sands, clays, and silts, often overlooking peats. Despite this, engineering challenges related to peats, such as differential settlements and landslides, impact society. Understanding peat behavior is crucial for addressing modern issues like infrastructure resilience, CO2 emissions, and climate change adaptation, and for developing less intrusive construction methods that reduce peatland degradation. Kringelmomyra is a peatland in northern Norway where the surcharging method is being used to construct a new highway. This paper presents its geotechnical, hydrogeological, and ecological characteristics, initial quantitative data on potential changes in hydrogeology, and the remaining plant biodiversity resulting from road construction. Geotechnical testing and hydrogeological monitoring reveal complex peat stratification and minimal initial hydrogeological impact. The endangered peat moss Sphagnum venustum was found at the site, highlighting the need to monitor the impact at the site in the coming years. Continued interdisciplinary monitoring is essential to understand long-term effects and ensure sustainable construction practices on peatlands.



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    [1] Yu ZC (2012) Northern peatland carbon stocks and dynamics: a review. Biogeosciences 9: 4071–4085. https://doi.org/10.5194/bg-9-4071-2012 doi: 10.5194/bg-9-4071-2012
    [2] Nichols JE, Peteet DM (2019) Rapid expansion of northern peatlands and doubled estimate of carbon storage. Nat Geosci 12: 917–921. https://doi.org/10.1038/s41561-019-0454-z doi: 10.1038/s41561-019-0454-z
    [3] Girkin NT, Cooper HV, Ledger MJ, et al. (2022) Tropical peatlands in the Anthropocene: The present and the future. Anthropocene 40: 100354. https://doi.org/10.1016/j.ancene.2022.100354 doi: 10.1016/j.ancene.2022.100354
    [4] Villa JA, Bernal B (2018) Carbon sequestration in wetlands, from science to practice: An overview of the biogeochemical process, measurement methods, and policy framework. Ecol Eng 114: 115–128. https://doi.org/10.1016/j.ecoleng.2017.06.037 doi: 10.1016/j.ecoleng.2017.06.037
    [5] IPCC, Summary for Policymakers of IPCC Special Report on Global Warming of 1.5℃ approved by governments, 2018. Available from: https://www.ipcc.ch/2018/10/08/summary-for-policymakers-of-ipcc-special-report-on-global-warming-of-1-5c-approved-by-governments/.
    [6] Bossio DA, Cook-Patton SC, Ellis PW, et al. (2020) The role of soil carbon in natural climate solutions. Nature Sustainability 3: 391–398.
    [7] Page SE, Baird AJ (2016) Peatlands and Global Change: Response and Resilience. Annu Rev Env Resour 41: 35–57. https://doi.org/10.1146/annurev-environ-110615-085520 doi: 10.1146/annurev-environ-110615-085520
    [8] Bryn A, Strand GH, Angeloff M, et al. (2018). Land cover in Norway based on an area frame survey of vegetation types. Norsk Geogr Tidsskr 72: 131–145. https://doi.org/10.1080/00291951.2018.1468356 doi: 10.1080/00291951.2018.1468356
    [9] Carlsten P (1988) Peat Geotechnical Properties and Up-to-Date Methods of Design and Construction, State-of-the-Art-Report Preprint, Swedish Geotechnical Institute Report 215.
    [10] Carlsten P (1995) Construction methods for roads in peatlands areas. XI European Conference for Soil Mechanics and Foundation Engineering, Danish Geotechnical Institute, Copenhagen, Denmark, 8–13.
    [11] Paniagua P, Long M, L'Heureux JS (2021) Geotechnical characterization of Norwegian peat: database. IOP Conference Series: Earth and Environmental Science, 18th Nordic Geotechnical Meeting, Helsinki, Finland. 710: 012016. https://doi.org/10.1088/1755-1315/710/1/012016
    [12] Paniagua P, Long M, Trafford A, et al. (2024) The Tiller-Flotten peat site: A natural peat soil deposit aimed for geotesting, 19th Nordic Geotechnical Meeting, Göteborg. 618–621.
    [13] Long M, Paniagua P, Grimstad G, et al. (2022) Engineering properties of Norwegian peat for calculation of settlements. Eng Geol 308: 106799. https://doi.org/10.1016/j.enggeo.2022.106799 doi: 10.1016/j.enggeo.2022.106799
    [14] Long M, von der Tann L, Ritter S, et al. (2024) Centrifuge modelling of sand and sawdust embankments on peat for sustainable infrastructure development. Proceedings of the XVIII ECSMGE 2024—Geotechnical Engineering Challenges to Meet Current and Emerging Needs of Society, CRC Press. https://doi.org/10.1201/9781003431749-96
    [15] Ritter S, von der Tann L, Dahl M, et al. (2024) Settlement behaviour of peat underneath a sand and sawdust embankment: centrifuge modelling, 5th European Conference on Physical Modelling in Geotechnics, Delft, The Netherlands.
    [16] Hov S, Paniagua P, Sætre C, et al. (2023) Stabilisation of Soft Clay, Quick Clay and Peat by Industrial By-Products and Biochars. Appl Sci 13: 9048. https://doi.org/10.3390/app13169048 doi: 10.3390/app13169048
    [17] NPRA (2022) Bygger veg på myr med 90% mindre utslipp. Building a road on bog with 90% less emissions. Available from: https://www.vegvesen.no/vegprosjekter/europaveg/e6brattasenlien/nyhetsarkiv/bygger-veg-pa-myr-med-mindre-utslipp/.
    [18] NGF, Guidelines for carrying out total soundings. Rev 1. Norwegian Geotechnical Society, 2018. Available from: https://ngf.no/wp-content/uploads/2020/02/NGF-Melding-9-Totalsondering-Rev-1-2018.pdf.
    [19] NGF, Guidelines for carrying out piezocone tests. Rev. 3. Norwegian Geotechnical Society, 2010. Available from: https://ngf.no/wp-content/uploads/2015/03/5_NGF-Melding-5-CPTU-_revisjon-3.pdf.
    [20] NGF, Guidelines for sampling. Norwegian Geotechnical Society, 2013. Available from: https://ngf.no/wp-content/uploads/2015/03/NGF-Melding-11-Provetaking-2014.pdf.
    [21] NGI, Beslutningsnotat for bygging av veg over Kringelmomyra. Decision memorandum for the construction of a road above Kringelmomyra. E6 Svenningelv-Lien Technical Note N-GEOT-02. Rev. 0. In Norwegian. 2021. Available from: NGI Document center ngi@ngi.no.
    [22] von Post L, Granlund LE (1926) Södra Sveriges Torvtillgånger, I. Sver Geo Unders C35, 19.
    [23] NGI, FOU Kringelmomyra: Resultater fra overvåkning fra juli 2022 og 2023. R & D Kringelmomyra: Results of monitoring from July 2022 and 2023. Technical note 20220382-03-TN. Rev. 0, 2024. In Norwegian. Available from: NGI Document center ngi@ngi.no.
    [24] NGI, Georadar Kringelmomyra. E6 Svenningelv-Lien N-GEOT-16. Rev. 0, 2022. In Norwegian. Available from: NGI Document center ngi@ngi.no.
    [25] Halvorsen R, Skarpaas O, Bryn A, et al. (2020) Towards a Systematics of Ecodiversity: The Ecosyst Framework. Global Ecol Biogeogr 29: 1887–1906. https://doi.org/10.1111/geb.13164 doi: 10.1111/geb.13164
    [26] Høitomt T, Blom HH, Brynjulvsrud JG, et al. (2021) Moser: Vurdering av sylfidetorvmose Sphagnum (Acutifolia) venustum for Norge. Rødlista for arter 2021. Artsdatabanken. Available from: https://lister.artsdatabanken.no/rodlisteforarter/2021/19679.
    [27] NGI, Bygging av flytende veg over myr. Building of a floating road on peat. E6 Svenningelv-Lien Technical note N-PGL-03. Rev. 0. 2023. In Norwegian. Available from: NGI Document center ngi@ngi.no.
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