Temporal changes in soil aggregates and water erosion after a wildfire in a Mediterranean pine forest

The evolution of soil structure after a forest fire was studied on two zone s representatives of a typical Mediterranean Pine forest. These zones were in opposite slope orientation but with similar topographical and pedologica l characteristics. Changes in soil macro-aggregation and water stable micro -aggregation were monitored seasonally during a year after the fire. The wa ter erosion patterns were also studied from August 1993, immediately after the fire, to the end of 1996. The first 5 cm of soil depth were the most af fected by fire temperature, showing clear differences on aggregate distribu tion and temporal variability between zones. In the north-facing soil, a su bstantial and gradual recovery on soil aggregation was observed mainly in t he fraction greater than 5-mm diameter; this reached an increase of 27% in mass of aggregates. In the south slope, the evolution of aggregation was sm ooth and restricted to the fraction minor than 0.1 mm. These differences be tween zones are reflected also in their values on soil cohesiveness and com paction, being lesser in the south-oriented soils. Values of erosion parame ters show that both zones have the higher soil losses during the immediate period (4 months) after the fire, being more important in the south zone. T his zone produced more sediment and runoff (52.42% and 29.95%, respectively ) than north-facing soils for the whole period studied. (C) 2001 Elsevier S cience B.V. All rights reserved.