We conclude that the changes of SOM stability with distance were the effect of modification of ion-exchange relationships (particularly base cations versus Al 3+ with H +) rather than forest stand species or intrinsic SOM properties (like functional groups, the recalcitrance of bindings etc.). We suggest that the combined effect of Ca and Na ions, originating from winter de-icing, caused the depletion of Al and hydrogen (H) in the soil close to the forest edge and, therefore, resulted in lower SOM stability expressed as the decreased DOC and pyrophosphate-extractable carbon content, as well as the release of CO 2. In the fir site, the humic and fulvic acids, the dissolved organic carbon (DOC) content and aluminum (Al) to C t ratio were depleted in close proximity to the highway. In both sites, we observed increased soil pH and CO 2 respiration in the vicinity of the highway, as well as increased ratios of exchangeable calcium (Ca), magnesium (Mg) and sodium (Na) to C t. The stoichiometric ratios of chosen chemical parameters to total carbon (C t) were calculated. We also conducted a comprehensive analysis of soil chemical properties. Soil CO 2 respiration was determined using closed chamber incubation with an alkali trap. From each site, samples were taken at 2, 12 and 22 m from the forest edge. Two study sites were established in Scots pine and Silver fir stands, located close to the S7 highway in central Poland, which was opened to traffic in 1984. The aim of this study was to test the hypotheses that a roadway will (1) modify the composition of the cation exchange capacity of adjacent forest soils, and (2) significantly decrease the stability of SOM.

Soil CO 2 respiration is an important indicator of SOM biological stability. Roadways traverse many forest areas and they often have harmful effects on forest soils, including the modified stability of soil organic matter (SOM).

Road to 56 focus trees