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Proceedings of the International Association of Hydrological Sciences An open-access publication for refereed proceedings in hydrology
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Levelling and extensometers are applied to monitor subsidence in a cultivated peatland in Overijssel, The Netherlands, in the period end 2018 to end 2019. Preliminary results show vertical movements in the order of centimeters related to seasonal dynamics (rise in autumn/winter, subsidence in spring/summer) and shorter-term dynamics related to groundwater level fluctuations. Additional data collection is needed to assess long term net subsidence.
PIAHS | Articles | Volume 382
Proc. IAHS, 382, 189–194, 2020
https://doi.org/10.5194/piahs-382-189-2020
Proc. IAHS, 382, 189–194, 2020
https://doi.org/10.5194/piahs-382-189-2020

Pre-conference publication 22 Apr 2020

Pre-conference publication | 22 Apr 2020

Monitoring shallow subsidence in cultivated peatlands

Sanneke van Asselen et al.

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Cited articles

De Mulder, E. F. J., Geluk, M. C., Ritsema, I., Westerhoff, W. E., and Wong, T. E.: De Ondergrond van Nederland, Geologie van Nederland, deel 7, Nederlands Instituut voor Toegepaste Geowetenschappen TNO, Utrecht, 379 pp., 2003 (in Dutch). 
Erkens, G., van der Meulen, M. J., and Middelkoop, H.: Double trouble: subsidence and CO2 respiration due to 1,000 years of Dutch coastal peatlands cultivation, Hydrogeol. J., 24, 551–568, 2016. 
Pleijter, M. and van den Akker, J. J. H.: Onderwaterdrains in het veenweidegebied: toelichting op de methode en meetinrichting, Wageningen Environmental Research report nr 1586, 2007 (in Dutch).  
Poland, J. F.: Guidebook to Studies of Land Subsidence Due to Ground-water Withdrawal, UNESCO report, ISBN 92-3-102213-X, 1984. 
Sneed, M. and Brandt, J. T.: Land subsidence in the San Joaquin Valley, California, USA, 2007–2014, Proc. IAHS, 372, 23–27, 2015. 
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Short summary
Levelling and extensometers are applied to monitor subsidence in a cultivated peatland in Overijssel, The Netherlands, in the period end 2018 to end 2019. Preliminary results show vertical movements in the order of centimeters related to seasonal dynamics (rise in autumn/winter, subsidence in spring/summer) and shorter-term dynamics related to groundwater level fluctuations. Additional data collection is needed to assess long term net subsidence.
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