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Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens
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 includ...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2015
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4670166/ https://www.ncbi.nlm.nih.gov/pubmed/26637121 http://dx.doi.org/10.1371/journal.pone.0144006 |
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author | Mettrop, Ivan S. Cusell, Casper Kooijman, Annemieke M. Lamers, Leon P. M. |
author_facet | Mettrop, Ivan S. Cusell, Casper Kooijman, Annemieke M. Lamers, Leon P. M. |
author_sort | Mettrop, Ivan S. |
collection | PubMed |
description | 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 HCO(3) (-) 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. NO(3) (-) and NH(4) (+) 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. |
format | Online Article Text |
id | pubmed-4670166 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2015 |
publisher | Public Library of Science |
record_format | MEDLINE/PubMed |
spelling | pubmed-46701662015-12-10 Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens Mettrop, Ivan S. Cusell, Casper Kooijman, Annemieke M. Lamers, Leon P. M. PLoS One Research Article 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 HCO(3) (-) 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. NO(3) (-) and NH(4) (+) 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. Public Library of Science 2015-12-04 /pmc/articles/PMC4670166/ /pubmed/26637121 http://dx.doi.org/10.1371/journal.pone.0144006 Text en © 2015 Mettrop et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited. |
spellingShingle | Research Article Mettrop, Ivan S. Cusell, Casper Kooijman, Annemieke M. Lamers, Leon P. M. Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens |
title | Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens |
title_full | Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens |
title_fullStr | Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens |
title_full_unstemmed | Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens |
title_short | Short-Term Summer Inundation as a Measure to Counteract Acidification in Rich Fens |
title_sort | short-term summer inundation as a measure to counteract acidification in rich fens |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4670166/ https://www.ncbi.nlm.nih.gov/pubmed/26637121 http://dx.doi.org/10.1371/journal.pone.0144006 |
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