Full text of this article is only available in PDF format.

Raija Laiho (email), Sakari Sarkkola, Seppo Kaunisto, Jukka Laine, Kari Minkkinen

Macroscale variation in peat element concentrations in drained boreal peatland forests

Laiho R., Sarkkola S., Kaunisto S., Laine J., Minkkinen K. (2008). Macroscale variation in peat element concentrations in drained boreal peatland forests. Silva Fennica vol. 42 no. 4 article id 233. https://doi.org/10.14214/sf.233

Abstract

Information on the variation in soil element concentrations at different spatial scales is needed for, e.g., designing efficient sampling strategies, upscaling the processes related to carbon cycling, and planning land use and management. In spite of intensive land use, such information concerning peat soils is still scarce. We analyzed the variation in peat mineral element concentrations in boreal peatland forests drained 50–60 years earlier. We wanted to quantify the proportions of variation deriving from differences between regions and peatland basins and from within-peatland heterogeneity, and to model the variation using relatively easily measurable site and soil characteristics. We utilized 878 peat samples representing the 0–20 cm layer and collected from 289 sites in 79 peatland basins. The sites represented three different drained peatland forest site types. The two strongest gradients in the element composition captured by principal component analysis were correlated with both the North-South gradient and the site type variation, and the East-West gradient. In general, most of the variation in the element concentrations was contributed by differences among peatland basins, and variation within the floristically determined sites. Most of the element concentrations were best modeled when either the bulk density or the ash content of the peat, or both, were used in addition to site type and geographical location. The explanatory power remained modest for most element concentrations. As for the P concentrations in soil, however, our models provide means for estimating a large part of the variation among drained pine mire sites.

Keywords
drainage; peat soil; nutrient deficiencies; spatial variation; soil nutrients

Author Info
  • Laiho, University of Helsinki, Department of Forest Ecology, FI-00014 University of Helsinki, Finland E-mail raija.laiho@helsinki.fi (email)
  • Sarkkola, Finnish Forest Research Institute, Vantaa Research Unit, P.O. Box 18, FI-01301 Vantaa, Finland E-mail ss@nn.fi
  • Kaunisto, Finnish Forest Research Institute, Parkano Research Unit, Kaironiementie 54, FI-39700 Parkano, Finland E-mail sk@nn.fi
  • Laine, Finnish Forest Research Institute, Parkano Research Unit, Kaironiementie 54, FI-39700 Parkano, Finland E-mail jl@nn.fi
  • Minkkinen, University of Helsinki, Department of Forest Ecology, FI-00014 University of Helsinki, Finland E-mail km@nn.fi

Received 15 February 2008 Accepted 25 August 2008 Published 31 December 2008

Views 4560

Available at https://doi.org/10.14214/sf.233 | Download PDF

Creative Commons License CC BY-SA 4.0

Register
Click this link to register to Silva Fennica.
Log in
If you are a registered user, log in to save your selected articles for later access.
Contents alert
Sign up to receive alerts of new content

Your selected articles
Your search results
Kaunisto S., Sarjala T. (1997) Critical needle potassium concentrations indicat.. Silva Fennica vol. 31 no. 4 article id 5633
Sarjala T., Kaunisto S. (1996) Effect of different potassium sources on the sea.. Silva Fennica vol. 30 no. 4 article id 5565
Laiho R., Sarkkola S. et al. (2008) Macroscale variation in peat element concentrati.. Silva Fennica vol. 42 no. 4 article id 233
Kaunisto S., Sarjala T. (2003) Foliar potassium concentrations of bilberry, bog.. Silva Fennica vol. 37 no. 3 article id 492