Smc. Robertson et al., Water chemistry of throughfall and soil water under four tree species at Gisburn, northwest England, before and after felling, FOREST ECOL, 129(1-3), 2000, pp. 101-117
The chemistry of throughfall, from intact canopies and felling debris, and
soil waters beneath four tree species, alder (Alnus glutinosa), Scots pine
(Pinus sylvestris), Norway spruce (Picea abies) and oak (Quercus petraea),
and an unplanted control plot, was monitored before and after felling at a
site on humic gley soils in the north of England. The results show clear di
fferences in solute concentrations below the four species both before and a
fter felling. Before felling the concentrations of the mainly atmospherical
ly derived ions (Na+, Mg2+, SO42-, Cl-) were larger in both throughfall and
soil waters below the conifers than the hardwoods. There were smaller inte
r species differences in the concentrations of solutes mainly controlled by
within system processes (K+, NO3-, PO4-, DOC); NO3- concentrations were la
rgest below the alder. Following felling, concentrations of the mainly atmo
spherically derived solutes declined below all four species and the inter-s
pecies differences reduced sharply so that in the second year after felling
there was little difference between species. Concentrations of the solutes
controlled by within system processes mainly increased after felling. The
largest increase in K+ concentrations was below the conifers, which had fol
iage at the time of felling; most of the K was retained in the upper soil e
xcept below spruce. Nitrate concentrations declined below alder after felli
ng while increasing below the other species. The largest increase was below
spruce and the increased concentrations were seen in the lower horizons be
low both conifer species, suggesting that there would probably be leakage t
o ground- or surface waters. The factors leading to the reduction in nitrat
e concentrations below alder merit further research. PO43- released from th
e felling debris and litter layer was retained in the upper soil. (C) 2000
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