Available Nutrients Can Accumulate in Permanent Skid Trails

Forests. 2017;8(10):358 DOI 10.3390/f8100358

 

Journal Homepage

Journal Title: Forests

ISSN: 1999-4907 (Print)

Publisher: MDPI AG

LCC Subject Category: Science: Botany: Plant ecology

Country of publisher: Switzerland

Language of fulltext: English

Full-text formats available: PDF, HTML

 

AUTHORS

Kenton P. Stutz (Chair of Soil Ecology, Institute of Forest Sciences, University of Freiburg, D-79085 Freiburg, Germany)
Helmer Schack-Kirchner (Chair of Soil Ecology, Institute of Forest Sciences, University of Freiburg, D-79085 Freiburg, Germany)
Gerald Kändler (Department of Biometry, Forest Research Institute of Baden-Württemberg, D-79100 Freiburg, Germany)
Lea Landes (Chair of Soil Ecology, Institute of Forest Sciences, University of Freiburg, D-79085 Freiburg, Germany)
Martin Linz (Chair of Soil Ecology, Institute of Forest Sciences, University of Freiburg, D-79085 Freiburg, Germany)
Hannes Warlo (Chair of Soil Ecology, Institute of Forest Sciences, University of Freiburg, D-79085 Freiburg, Germany)
Friederike Lang (Chair of Soil Ecology, Institute of Forest Sciences, University of Freiburg, D-79085 Freiburg, Germany)

EDITORIAL INFORMATION

Blind peer review

Editorial Board

Instructions for authors

Time From Submission to Publication: 11 weeks

 

Abstract | Full Text

Forest harvesting removes and redistributes nutrients through felling and forwarding. Substantial quantities of nutrients can accumulate in brash mats on permanent skid trails, but their availability and uptake after multiple thinnings on soils susceptible to leaching are unknown. In this study, we modeled the deposition of base cations and phosphorus on a permanent skid trail after five thinnings of a Picea abies (L.) Karst. stand, and measured the resulting nutrient stocks in both the forest floor and mineral soil. An estimated 35%, 44%, 41%, and 61% of harvested Ca, K, Mg, and P, respectively, were redistributed to the skid trail. Of those deposited stocks, 32–65% of nutrients remained in decomposed brash material on the skid trail. Mineral soil stocks for Ca, K, and P were significantly higher in the skid trail than in the stand, which included minor increases in bioavailable pools. Skid trail root densities were not lower than the stand while bulk densities were only partially higher. Both would not limit nutrient uptake. There were no significant relations between needle nutrient concentrations and distance to the skid trail. Altogether, these results indicate that nutrient uptake from the skid trail was minimal despite their accumulation, chemical availability, and physical accessibility. This suggests that other factors such as liming and frequent thinning disturbances can repress uptake of available nutrients on skid trails.