The effects of salinization on aerobic and anaerobic decomposition and mineralization in peat meadows: the roles of peat type and land use.
Peat soils comprise a large part of the western and northern Netherlands. Drainage for agriculture has caused increased soil aeration which has stimulated decomposition and, hence, soil subsidence, currently amounting to 1-2 cm/yr. River water is supplied to these peat areas in summer to prevent drying out of the peat soils. Saltwater intrusion and evaporation make this surface water slightly brackish during drought periods. In addition, brackish seepage can surface more easily during such dry periods. We performed an incubation experiment in which the effects of salinization on aerobic decomposition and mineralization of shallow peat samples and anaerobic decomposition and mineralization of deep peat samples were studied. We considered four different types of peat samples: peat sampled in agricultural peat meadows and in nature reserves, originally formed under either eutrophic or oligotrophic conditions. The aerobic decomposition was approximately reduced by 50% after salinization, whereas the anaerobic decomposition rates remained unchanged. Remarkably, the response to salinization did not differ between the peat types and land uses. Ammonium concentrations increased while nitrate concentrations decreased after salinization, probably as a result of reduced nitrification. Especially in the oligotrophic peat, ammonium concentrations increased substantially. Phosphate concentrations increased, possibly caused by changes in desorption and adsorption processes due to higher ion concentrations. DOC concentrations decreased in the brackish samples due to precipitation. Furthermore, the eutrophic peat samples showed increasing sulfate concentrations, both in oxic and anoxic incubations, which was attributed to pyrite oxidation. Independently of salinization, nitrification rates were higher in the agricultural, fertilized, peat soils. In conclusion, while salinization might reduce subsidence rates, it will have adverse effects on water quality.
Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, The Netherlands. Electronic address: k.brouns@uu.nl.
Karlijn
K
Brouns
Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, The Netherlands.
Jos T A
JT
Verhoeven
Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, The Netherlands.
Mariet M
MM
Hefting
D000332:Aerobiosis; D000383:Agriculture; D000641:Ammonia / Q000032:analysis; D000693:Anaerobiosis; D002244:Carbon / Q000032:analysis; D002245:Carbon Dioxide / Q000032:analysis; D055864:Droughts; D005618:Fresh Water; D065948:Grassland; D008697:Methane / Q000032:analysis; D009426:Netherlands; D058465:Nitrification; D010710:Phosphates / Q000032:analysis; D054712:Salinity; D012987:Soil / Q000737:chemistry; D012988:Soil Microbiology
D010710:Phosphates; D012987:Soil; D002245:Carbon Dioxide; D002244:Carbon; D000641:Ammonia; D008697:Methane
Climate change; Decomposition; Mineralization; Peat soils; Salinization; Subsidence