Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)

A simple dynamic soil model developed to analyse the effects of atmospheric deposition and nutrient cycling on terrestrial ecosystems, SMART 2, was applied to the Kangasvaara catchment in eastern Finland. Given the historical deposition and forest growth patterns and reasonable values for the input...

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Main Authors: J. Kämäri, K. Rankinen, L. Finér, S. Piirainen, M. Posch
Format: Article
Language:English
Published: Copernicus Publications 1998-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/2/485/1998/hess-2-485-1998.pdf
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spelling doaj-2f0b5dce8d964ad0b92f6d05f554d4ad2020-11-24T21:31:54ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79381998-01-0124485495Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)J. KämäriJ. KämäriK. RankinenL. FinérS. PiirainenM. PoschA simple dynamic soil model developed to analyse the effects of atmospheric deposition and nutrient cycling on terrestrial ecosystems, SMART 2, was applied to the Kangasvaara catchment in eastern Finland. Given the historical deposition and forest growth patterns and reasonable values for the input parameters, SMART 2 was calibrated successfully to reproduce present-day soil and Kangasvaara catchment on the soil and runoff water chemistry under a future deposition scenario (GRP scenario). These impacts were also compared to the effects of further reducing the deposition of sulphur and nitrate under the maximum feasible reduction (MFR) scenario. The model demonstrates the consequences of breaking the nutrient cycle, and predicts that final cutting results in increased leaching of inorganic nitrogen and base cations from the cut part of the catchment for about 10 years. The resulting concentrations in the stream will depend on the ability of the buffer zones surrounding the stream to capture and utilize these nutrients.http://www.hydrol-earth-syst-sci.net/2/485/1998/hess-2-485-1998.pdf
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language English
format Article
sources DOAJ
author J. Kämäri
J. Kämäri
K. Rankinen
L. Finér
S. Piirainen
M. Posch
spellingShingle J. Kämäri
J. Kämäri
K. Rankinen
L. Finér
S. Piirainen
M. Posch
Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)
Hydrology and Earth System Sciences
author_facet J. Kämäri
J. Kämäri
K. Rankinen
L. Finér
S. Piirainen
M. Posch
author_sort J. Kämäri
title Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)
title_short Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)
title_full Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)
title_fullStr Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)
title_full_unstemmed Modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (Kangasvaara, eastern Finland)
title_sort modelling the response of soil and runoff chemistry to forest harvesting in a low deposition area (kangasvaara, eastern finland)
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 1998-01-01
description A simple dynamic soil model developed to analyse the effects of atmospheric deposition and nutrient cycling on terrestrial ecosystems, SMART 2, was applied to the Kangasvaara catchment in eastern Finland. Given the historical deposition and forest growth patterns and reasonable values for the input parameters, SMART 2 was calibrated successfully to reproduce present-day soil and Kangasvaara catchment on the soil and runoff water chemistry under a future deposition scenario (GRP scenario). These impacts were also compared to the effects of further reducing the deposition of sulphur and nitrate under the maximum feasible reduction (MFR) scenario. The model demonstrates the consequences of breaking the nutrient cycle, and predicts that final cutting results in increased leaching of inorganic nitrogen and base cations from the cut part of the catchment for about 10 years. The resulting concentrations in the stream will depend on the ability of the buffer zones surrounding the stream to capture and utilize these nutrients.
url http://www.hydrol-earth-syst-sci.net/2/485/1998/hess-2-485-1998.pdf
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