Hs. Wheater et al., HYDROLOGICAL FLOW PATHS AT THE ALLT A-MHARCAIDH CATCHMENT - AN ANALYSIS OF PLOT AND CATCHMENT SCALE OBSERVATIONS, Hydrological processes, 7(4), 1993, pp. 359-371
An integrated programme of hydrological monitoring at the 10 km2 Allt
a' Mharcaidh catchment in north-east Scotland has been based on observ
ations at plot, hillslope and catchment scale. The resonse of the prin
cipal soil types has been characterized from a combination of throughf
low and three-dimensional tensiometer data at plot scale, and plot seq
uences have been used to investigate hillslope scale effects. Seep eme
rgence is associated with downslope drainage and local topographic con
vergence; in parallel preferential pathways generate a highly dynamic
throughflow response. Catchment and subcatchment hydrographs mirror th
e twin dynamic observed at hillslope scale, and a unified hypothesis o
f response is presented which is consistent with all scales of observa
tions.