Ba. Olsson et al., EFFECTS OF DIFFERENT FOREST HARVEST INTENSITIES ON THE POOLS OF EXCHANGEABLE CATIONS IN CONIFEROUS FOREST SOILS, Forest ecology and management, 84(1-3), 1996, pp. 135-147
Effects of harvest intensity on exchangeable cations (1 M NH4Cl extrac
ts) were examined in four coniferous forest soils in Sweden, 15-16 yea
rs after clear-felling. Logging residues were harvested at three inten
sities, applied experimentally in a randomized block design (n = 4): (
i) conventional stem-only harvest, (ii) branches and stems harvested b
ut needles left on the ground and() whole-tree harvesting where all ab
ove-stump biomass was harvested, Two of the sites were located in nort
hern Sweden, and the other two were in southern Sweden. In each region
one site was occupied by a pure Scots pine stand (Pinus sylvestris L.
) and the other by a pure Norway spruce stand (Picea abies (L.) Karst.
).Whole-tree harvesting resulted in a lower level of base saturation,
especially in the humus layer, Compared with base saturation levels in
the stem-only harvest treatment, the reductions were 19%, 16% and 8%
at the southern sites with spruce and pine and at the northern spruce
site, respectively. At the northern pine site no significant treatment
effect was detected. Analyses across all study sites of element pools
in the humus and 0-20 cm mineral soil layers indicated that reduction
s in base saturation generally were associated with depletions of exch
angeable pools of K, Ca and Mg. In addition, effective cation exchange
capacity per unit area was in general lower after whole-tree harvesti
ng compared with the other treatments, Effects on exchangeable pools o
f Mn and Zn were similar to those observed for base cations. Exchangea
ble pools of acidic cations were generally not affected, but at the so
uthern sites pools of acidic cations increased with harvest intensity.
No significant differences in soil pH(H2O) were detected between trea
tments. A relatively high proportion of the Ca left on site in the for
m of slash was recovered in the soil ca. 15 years after felling, This
was not the case for K. Furthermore, the nutrient load recovered in th
e soil was lower at the southern site with Norway spruce than at the o
ther sites, Apart from these inter-site differences, the results were
consistent across all study sites.