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Short-term effects of experimental burning on soil nutrients in the Cantabrian heathlands
Authors:E. Marcos  C. Villalón  L. Calvo  E. Luis-Calabuig
Affiliation:1. Department of Biology, CESAM (Centre for Environmental and Marine Studies), University of Aveiro, Aveiro, Portugal;2. Department of Environment and Planning, CESAM (Centre for Environmental and Marine Studies), University of Aveiro, Aveiro, Portugal;1. GRAM (Grup de Recerca Ambiental Mediterrània), Department of Geography, University of Barcelona, Montalegre, 6, 08001 Barcelona, Spain;2. Environmental Management Centre, Mykolas Romeris University, Vilnius, Lithuania;1. Escuela Politécnica Superior, Universidad de Zaragoza, Ctra de Cuarte s/n, 22071 Huesca, Spain;2. Departament de Medi Ambient i Ciències del Sòl, Universitat de Lleida, Av. Rovira Roure, 191, 25198 Lleida, Spain
Abstract:The aim of this study is to determine the short-term effects of fire on nitrogen and phosphorus soil concentration in heathland sites dominated by Calluna vulgaris in the Cantabrian Mountain range (NW Spain). Three C. vulgaris heathlands sites (San Isidro, Riopinos I and Riopinos II) were selected. In June 2005, one plot (20 m × 20 m) per site was subjected to an experimental fire and the other was used as a control. Immediately after the fire, ten ash samples and ten soil samples (at a depth of 5 cm) were collected and thoroughly mixed. Soil moisture, temperature, total N, NH4+, NO3?, total P, available P and pH were determined in each sample. The quantity of ashes deposited was 300 g/m2, with a pH of 9, low N content but higher P concentrations. Significant differences in temperature and soil moisture were detected between the fire-treated and control plots. No significant differences for soil pH, total and available P, total N and NO3? concentration were found between the treatments. However, the concentration of ammoniacal-N indicated a significant increase 11 months post-fire and was produced by the changes in environmental soil conditions after the fire. Our results show that low intensity fires do not modify the concentration of N and P in the soil. However, post-fire conditions favour an increase in ammoniacal-N one year later.
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