Organically bound halogens in coniferous forest soil -Distribution pattern and evidence of in situ production

We examined organically bound halogens in a coniferous soil profile and in Norway spruce litter enclosed in litter bags and subjected to degradation in field. Throughout the soil profile the total amount of organically bound halogens (TOX, μg Cl/g soil) was related to organic matter, i.e. amounts decreased with increasing depth. In contrast, the organic chlorine to organic carbon ratio (mg Clorg:g Corg) increased with increasing depth, and a pronounced increase in this ratio was observed in the transition between the O-horizon and the A-horizon, strongly indicating that in situ production of organically bound halogens occur in soil. This conclusion was strengtened by the results of the litter bag study, which clearly showed that a net-production of organically bound halogens occurred during decomposition of the spruce needle litter. Furthermore, this part of the study showed that organically bound halogens are not a static factor of organic matter. On the contrary, the results strongly indicated that during decomposition of organic matter, organically bound halogens are subjected to both production, i.e. incorporation of inorganic halides into organic matter, and mineralisation, i.e. release of inorganic halides from organic matter. A method previously developed in our laboratory to determine TOX in soil was further evaluated; there were no indications that inorganic halides interfere with the determination.