C - Lublin
C - Lublin
C - Lublin
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Regional data on Pb concentrations in wood biomass have been obtained on the<br />
base of special wood sampling in background area. As can see from Table 2, Pb<br />
concentrations in stem wood are lower for all tree types in comparison with the<br />
values obtained for branches and bark. The differences equal 4-6 times. As can be<br />
mentioned in (Remezov et al., 1959), concentrations of the element in different tree<br />
parts are maintained during all vegetation period if environmental conditions are<br />
not changed. So, the same data can be used for estimations of metal removing with<br />
biomass for trees of either age.<br />
Table 2. Data on Pb accumulation in wood biomass of the main tree types in the<br />
central Russia (based on: Zolotareva et al., 1983; Priputina et al., 2003)<br />
Tree Type Compartments Samples number Pb, mg/kg<br />
stem 16 0.51<br />
Spruce<br />
branches 14 3.00<br />
bark 6 2.00<br />
stem 11 0.38<br />
Pine<br />
branches 10 1.75<br />
bark 7 1.70<br />
stem 10 0.43<br />
Oak<br />
branches 10 2.70<br />
bark 4 5.00<br />
stem 10 0.68<br />
Birch<br />
branches 15 2.54<br />
bark 10 1.45<br />
As known, there are differences in the rates of annual biomass growth for the<br />
trees of different ages (as well as tree compartments) that can be taken into<br />
consideration in regional estimations (Fig.1). The results of wood productivity<br />
simulations (based on EFIMOD) show that average rates of annual biomass growth<br />
at age of 50-80(100) years are higher in 1.5-2 times in comparison with average<br />
data calculated for 10-100(150) years period. Taking into account the differences<br />
of Pb concentrations in the wood of stem/braches the fluxes of metal removal with<br />
biomass uptake have been calculated for pure stands of the main tree types: Spruce,<br />
Pine, Oak, Birch (Tab.3).<br />
Data presented in this paper had been used for preliminary calculating and<br />
mapping of critical loads of Pb for forest ecosystems in the basin of the Upper Oka.<br />
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