402-4 Where and How European Beech Deadwood Influences Soil.
See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Forest, Range, and Wildland Soils General Session III Oral
Abstract:
Preliminary tests indicate that deadwood influenced soil organic matter, chemical and physical properties not equally under various climatic, management and decay conditions. Water extractable organic C (OC), aromaticity and free particulate OC near deadwood increased the most at moder-silicate sites, long-time protected stands and very decayed stems. Aggregate-occluded particulate OC increased only for very decayed stems, while mineral-bound C did not change under any conditions. In contrast, total organic N decreased at mull-calcareous sites, harvested stands and moderately decayed stems. Changes to porosity and pore-diameter distributions were mostly limited to mull/moder-calcareous/silicate conditions; only meso-pores (10-0.2 μm) decreased in percent volume also at medium-term harvested stands and moderately decayed stems. Results for CuO-oxidized lignin, exchangeable cations and organic layer properties will also be presented.
We hope to elucidate forest management-relevant interactions between deadwood, site conditions, decomposition and harvesting.
See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Forest, Range, and Wildland Soils General Session III Oral