The short-term effects of management changes on watertable position and nutrients in shallow groundwater in a harvested peatland forest

• Published in: Journal of environmental management Vol. 142; pp. 46 - 52
• Main Authors: Finnegan, J., Regan, J.T., Fenton, O., Lanigan, G.J., Brennan, R.B., Healy, M.G.
• Format: Journal Article
• Language: English
• Published: Kidlington Elsevier Ltd 01.09.2014; Elsevier; Academic Press Ltd
• Subjects: Animal, plant and microbial ecology; Applied ecology; Biological and medical sciences; Clearfelling; Coniferophyta; Conservation, protection and management of environment and wildlife; Forestry; Forestry - methods; Fundamental and applied biological sciences. Psychology; General aspects; General forest ecology; Generalities. Production, biomass. Quality of wood and forest products. General forest ecology; Groundwater; Groundwater - analysis; Nutrients; Peat; Phosphorus - analysis; Soil; Trees; Watertable; Nutrients; Groundwater; Peat; Watertable; Forestry; Clearfelling; Short term; Forests; Position; Environmental management; Peat bog; Aquifers; Clearcutting; Nutrient; Ground water
• ISSN: 0301-4797; 1095-8630
• DOI: 10.1016/j.jenvman.2014.04.008

Management changes such as drainage, fertilisation, afforestation and harvesting (clearfelling) of forested peatlands influence watertable (WT) position and groundwater concentrations of nutrients. This study investigated the impact of clearfelling of a peatland forest on WT and nutrient concentrations. Three areas were examined: (1) a regenerated riparian peatland buffer (RB) clearfelled four years prior to the present study (2) a recently clearfelled coniferous forest (CF) and (3) a standing, mature coniferous forest (SF), on which no harvesting took place. The WT remained consistently below 0.3 m during the pre-clearfelling period. Results showed there was an almost immediate rise in the WT after clearfelling and a rise to 0.15 m below ground level (bgl) within 10 months of clearfelling. Clearfelling of the forest increased dissolved reactive phosphorus concentrations (from an average of 28–230 μg L−1) in the shallow groundwater, likely caused by leaching from degrading brash mats. •An upland peat forest was studied before and after harvesting (clearfelling).•Watertable fluctuations and groundwater nutrient concentrations were studied.•Clearfelling of a forest on blanket peat raised the watertable.