Phenolic compounds have been identified previously as potentially resp
onsible for allelopathic interferences in spruce forest at high altitu
de. They have now been analyzed in canopy leachates, snow, and soil so
lutions collected from the three layers of the podsolic soil: OA, E, a
nd B. Leachates were characterized by high tanning capacity and by p-h
ydroxyacetophenone (found at 10(-6) M) also detected as the major (10(
-7) M) monomeric compound in snow. At least 10 phenolic monomers, incl
uding vanillic, p-hydroxybenzoic, and protocatechuic acids were identi
fied in capillary waters extracted from the OA layer with their sum re
aching 2 x 10(-6) M. These monomers were only a small part (1%) of the
total phenolics. In soil solutions, significant decreases in phenolic
concentrations with depth were observed between the E and B layers, w
ith qualitative modifications of the phenolic pattern. Spruce leachate
s and soil solutions exhibited high temporal variability, resulting in
transitory allelopathic potential towards both aerial and subterranea
n parts of spruce seedlings. The occurrence of various and soluble phe
nolic compounds in the whole forest system, including p-hydroxyacetoph
enone, which persist from green needles to soil solutions, suggests th
at they could be involved in complex and interactive processes occurri
ng during organic matter accumulation on the coniferous forest floor.