Abstract

Peatland drainage based on ditch systems is a widely used forestry management practice in the boreal and hemiboreal forests to improve tree growth. This study investigated the morphological variation in absorptive roots (first- and second-order roots) across the distance gradient from the ditch with four sampling plots (5, 15, 40, and 80 m) in six drained peatland forests dominated by Downy birch and Norway spruce. The dominating tree species had a significant effect on the variation in absorptive root morphological traits. The absorptive roots of birch were thinner with a higher specific root area and length (SRA and SRL), higher branching intensity (BI), and lower root tissue density (RTD) than spruce. The distance from the ditch affected the absorptive root morphological traits (especially SRA and RTD), but this effect was not dependent on tree species and was directionally consistent between birch and spruce. With increased distance from the ditch (from plot 5 to plot 80), the mean SRA increased by about 10% in birch and 5% in spruce; by contrast, the mean RTD decreased by about 10% in both tree species, indicating a potential shift in nutrient foraging. However, soil physical and chemical properties were not dependent on the distance from the ditch. We found a species-specific response in absorptive root morphological traits to soil properties such as peat depth, pH, and temperature. Our results should be considered when evaluating the importance of morphological changes in absorptive roots when trees acclimate to a changing climate.

Highlights

  • Peatland drainage has been an essential component of forestry management practices in boreal and hemiboreal zones [1,2]

  • This study investigated the morphological variation in absorptive roots across the distance gradient from the ditch with four sampling plots (5, 15, 40, and 80 m) in six drained peatland forests dominated by Downy birch and Norway spruce

  • Irrespective of tree species, specific root area (SRA) increased while root tissue density (RTD) decreased toward higher distances from the ditch, indicating an acclimation in absorptive roots of trees to soil differences along with distances from the ditch

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Summary

Introduction

Peatland drainage has been an essential component of forestry management practices in boreal and hemiboreal zones [1,2]. Most of the available research is concerned with studying fine root production, fine root growth, and phenology in forested peatlands [11,12], while very little is known about the morphology of fine roots, especially the absorptive roots (defined as first- and second-order roots) [13,14] of trees growing in peat soils. These studies are scarce in the drained peatland forests

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