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Mettrop IS, Cusell C, Kooijman AM, et al. Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens. PLoS One. 2015;10(12):e0144006doi: 10.1371/journal.pone.0144006.
Mettrop, I. S., Cusell, C., Kooijman, A. M., & Lamers, L. P. (2015). Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens. PloS one, 10(12), e0144006. https://doi.org/10.1371/journal.pone.0144006
Mettrop, Ivan S, et al. "Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens." PloS one vol. 10,12 (2015): e0144006. doi: https://doi.org/10.1371/journal.pone.0144006
Mettrop IS, Cusell C, Kooijman AM, Lamers LP. Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens. PLoS One. 2015 Dec 04;10(12):e0144006. doi: 10.1371/journal.pone.0144006. eCollection 2015. PMID: 26637121; PMCID: PMC4670166.
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PLoS One. 2015 Dec 04;10(12):e0144006. doi: 10.1371/journal.pone.0144006. eCollection 2015.

Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens.

PloS one

Ivan S Mettrop, Casper Cusell, Annemieke M Kooijman, Leon P M Lamers

Affiliations

  1. Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, P.O. Box 94248, NL-1090 GE, Amsterdam, The Netherlands.
  2. Department of Aquatic Ecology & Environmental Biology, Institute for Water and Wetland Research, Radboud University Nijmegen, NL-6525, Nijmegen, The Netherlands.

PMID: 26637121 PMCID: PMC4670166 DOI: 10.1371/journal.pone.0144006

Abstract

In regions with intensive agriculture, water level fluctuation in wetlands has generally become constricted within narrow limits. Water authorities are, however, considering the re-establishment of fluctuating water levels as a management tool in biodiverse, base-rich fens ('rich fens'). This includes temporary inundation with surface water from ditches, which may play an important role in counteracting acidification in order to conserve and restore biodiversity. Inundation may result in an increased acid neutralizing capacity (ANC) for two reasons: infiltration of base-rich inundation water into peat soils, and microbial alkalinity generation under anaerobic conditions. The main objectives of this study were to test whether short-term (2 weeks) summer inundation is more effective than short-term winter inundation to restore the ANC in the upper 10 cm of non-floating peat soils, and to explain potential differences. Large-scale field experiments were conducted for five years in base-rich fens and Sphagnum-dominated poor fens. Winter inundation did not result in increased porewater ANC, because infiltration was inhibited in the waterlogged peat and evapotranspiration rates were relatively low. Also, low temperatures limit microbial alkalinity generation. In summer, however, when temperature and evapotranspiration rates are higher, inundation resulted in increased porewater Ca and HCO3- concentrations, but only in areas with characteristic rich fen bryophytes. This increase was not only due to stronger infiltration into the soil, but also to higher microbial alkalinity generation under anaerobic conditions. In contrast, porewater ANC did not increase in Sphagnum-plots as a result of the ability of Sphagnum spp. to acidify their environment. In both rich and poor fens, flooding-induced P-mobilization remained sufficiently low to safeguard P-limited vegetation. NO3(-) and NH4(+) dynamics showed no considerable changes either. In conclusion, short-term summer inundation with base-rich and nutrient-poor surface water is considered beneficial in the management of non-floating rich fens, and much more effective than winter inundation.

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