B. Soto et F. Diazfierros, RUNOFF AND SOIL-EROSION FROM AREAS OF BURNT SCRUB - COMPARISON OF EXPERIMENTAL RESULTS WITH THOSE PREDICTED BY THE WEPP MODEL, Catena, 31(4), 1998, pp. 257-270
The effects of burning on runoff and soil erosion from scrub-bearing h
illslopes in northwest Spain were investigated by monitoring of experi
mental plots over a 4-year period. At the beginning of this period, tw
o plots (BP1 and BP2) were subjected to low-intensity controlled burns
, and two plots left as controls; in the year following the controlled
burns, however, one of the control plots (plot WF) was burnt in a wil
dfire of higher intensity than the controlled burns. Runoff and erosio
n losses from the BP plots were only slightly higher than from the con
trol plot, with the loss in no case exceeding 300 g m(-2) yr(-1). Eros
ion losses from plot WF were considerably higher (1314 g m(-2) over th
e 1st year post-burning, 8.5 times higher than from the control plot).
These results were compared with those predicted using the Water Eros
ion Prediction Project (WEPP) hillslope model (Version 95.7). In gener
al, WEPP predictions of total runoff volume over the study period were
acceptable: coefficients of determination for the regression of predi
cted on observed values were 0.41, 0.68, 0.66 and 0.57 for the control
plot and plots BP1, BP2 and WF, respectively. Erosion losses were lik
ewise predicted with reasonable accuracy, though the model showed a co
nsistent tendency to under-estimate, particularly with plot WF. (C) 19
98 Elsevier Science B.V.