In this study, we compared the effectiveness of two treatments, straw mulching (2.3 Mg ha−1) and
seeding (4 g m−2), in reducing soil erosion after an experimental fire in a gorse (Ulex europaeus L.)
shrubland. Straw mulch provided an initial ground cover of 87%.
Themaximumtemperature reached at themineral soil surface during fire was positively related to accumulated
sediment yield during the first year after fire, supporting the importance of soil heating (or its surrogate, soil burn
severity) to explain post-fire erosion.
The first year after fire only straw mulch application significantly reduced soil erosion relative to the untreated
burned soils (89%). Seeding did not affect soil erosion after fire. The mean sediment yield after the seeding treatment
(2.9 Mg ha−1) was similar to that in the untreated burned plots (3.6 Mg ha−1).
Maximum concentrated precipitation (rainfall N 20mmaccumulated in one or two consecutive days) and antecedent
soil moisture were the variables most strongly associated with soil losses in the untreated burned and
seeded soils. Rainfall intensity-related variables did not explain soil loss variability. In the mulched soil, only
the maximum concentrated rainfall was related to sediment yield.
Total vegetation cover recovery was quite fast, particularly between 6 and 12 months after fire, and 70% of the
ground was covered by the end of the study. However, when the erosion rate was maximal, the cover provided
by vegetation was very low. Seeding contribution to total vegetation cover was small and we did not find any
differences in the mean vegetation cover between treatments although mulching delayed vegetation cover
recovery slightly.
In summary, seeding failed to reduce soil loss after fire, and the cover, directly in contact with the ground was a
key factor in reducing post-fire soil loss.