Tw. Berger et G. Glatzel, DEPOSITION OF ATMOSPHERIC CONSTITUENTS AND ITS IMPACT ON NUTRIENT BUDGETS OF OAK FORESTS (QUERCUS-PETRAEA AND QUERCUS-ROBUR) IN LOWER AUSTRIA, Forest ecology and management, 70(1-3), 1994, pp. 183-193
Geochemical processes in central European oak ecosystems (Qercus petra
ea and Quercus robur) suffering stand decline were studied in two oak
stands of the Weinviertel, Lower Austria, about 30 km north of Vienna.
Stores of chemical elements were determined by soil and biomass inven
tories. Deposition input was monitored over a 2 year period by bulk sa
mpling of throughfall. Soil solution chemistry was studied by tension
lysimetry over a 1 year period. Mineral nutrition of oak was judged by
foliar analysis. Bulk deposition rates were 10-12 kg N ha(-1) year(-1
) and 15-20 kg S ha(-1) year(-1). Total annual nitrogen gain is high.
Both systems lose calcium and magnesium. Foliar nutrient levels indica
te sufficient nutrition with main mineral nutrients, except for magnes
ium, which is in moderately low supply. Based on these findings, the h
ypothesis that pollutant deposition has been the cause of a sudden and
severe appearance of decline symptoms in the second half of the 1980s
must be dismissed. The data on deposition rates and ecosystem nutrien
t status, however, indicate that the soil of both systems is acidifyin
g, nitrogen stores are increasing, and magnesium pools are depleted. I
f deposition of pollutants continues at current rates, a slow but stea
dy degradation of many oak ecosystems in the Austrian Weinviertel is i
nevitable.