M. Bonell, SELECTED CHALLENGES IN RUNOFF GENERATION RESEARCH IN FORESTS FROM THEHILLSLOPE TO HEADWATER DRAINAGE-BASIN SCALE, Journal of the american water resources association, 34(4), 1998, pp. 765-785
When faced with practical forest land management issues such as the im
pacts of logging or forest conversion to other land uses, planners ide
ally require a comprehensive understanding of within drainage basin hy
drological processes to determine the most vulnerable areas to increas
ed storm runoff and erosion. Land managers in particular need to know
the source areas and magnitude of inputs to the storm hydrograph, in t
erms of water quantity, sediment and solute transport; and the routing
of such hydrographs from headwater to larger drainage basins. The lat
ter includes an overall assessment at various scales of the impacts of
forest disturbance and conversion on the water balance. This paper wi
ll focus on runoff generation in terms of identifying the various path
ways and source areas. Such aspects will be linked with the need for a
more comprehensive effort towards the field testing of so-called 'phy
sically based' models of runoff generation. Some of the controversial
issues arising from the difficulties in reconciling results from hydro
chemical investigations with complementary hydrometric studies will be
highlighted. Subsequently, attention will be given to topographic-wet
ness models, which have promising applications in forestland managemen
t. In addition, alternative simple models for application at the catch
ment scale will be assessed. The latter is in recognition that at smal
ler scales, heterogeneity both in time and space of soil hydraulic pro
perties demand a greater number of parameters in modelling. Such consi
derations can even prove an obstacle in terms of the confident applica
tion of 'physically bases models.