Rh. Crockford et al., CHEMISTRY OF RAINFALL, THROUGHFALL AND STEMFLOW IN A EUCALYPT FOREST AND A PINE PLANTATION IN SOUTH-EASTERN AUSTRALIA .2. THROUGHFALL, Hydrological processes, 10(1), 1996, pp. 13-24
A rainfall event-based study allowed the examination of factors affect
ing the amounts and chemical concentrations of throughfall. The amount
and frequency of antecedent rainfall was of influence in both forests
, in that concentrations were higher with dry antecedent conditions. T
he debarking season influenced throughfall in the eucalypt forest. Pot
assium was the dominant cation in the throughfall of both forests, bei
ng 50% of the sum of the major cations (Ca, Mg, Na and K) for the pine
s and 70% for the eucalypts. The largest difference was in sodium, bei
ng 29% of the combined cations for the pines and 10% for the eucalypts
. There was net uptake of hydrogen ions from rainfall for both forests
, i.e. throughfall was less acid than rainfall, but release occurred f
or a significant proportion of events and was associated with higher r
ainfall pH. There was a small net input of NH4-N and NO3-N by the euca
lypts. A more substantial input of both ions occurred in the pines. Ho
wever, uptake and release of both ions occurred for different events i
n both forests. Throughfall samples taken during events showed that th
e chemical concentration was related to variations in the intensity an
d continuity of the rainfall, particularly for the major cations. NH4-
N and NO3-N did not always follow the cation trends through time.