C. Martin et Y. Chevalier, Post forest-fire hydrochemical behaviour of the Rimbaud catchment (Massif des Maures, France), Z GEOMORPH, 43(3), 1999, pp. 359-381
In August 1990, a forest fire devastated 84 % of the Rimbaud catchment area
(1.46 km(2)). This catchment presents a substratum composed of gneiss. Its
relief is sharp. Soils are skeletal. The forest fire destroyed a maquis (w
ith treelike heather and arbustus) interspersed with cork oaks and maritime
pines. The fire's effects on the chemical composition of the runoff have r
emained light in terms of low flows. On the other hand, mineralization has
greatly increased during flood, especially at the beginning of the 1990-91
water year. The paper reports on the observations conducted during four yea
rs after the fire. Dissolved outputs and hydrochemical balances are compare
d with results obtained on the same catchment before the forest fire, and o
n the Boussicaut catchment (0.74 km(2)), which is very close by, but which
was not burnt.