Phosphorus and base cation accumulation and release patterns in decomposing Scots pine,Norway spruce and silver birch stumps

Tree stumps are integral constituents of managed forest ecosystems, but their role in nutrient cycling is poorly understood. We studied phosphorus (P), potassium (K), calcium (Ca) and magnesium (Mg) dynamics in decomposing Scots pine (Pinus sylvestris), Norway spruce (Picea abies), and silver birch (Betula pendula) stumps in southern Finland in a chronosequence of 0-, 5-, 10-, 20-, 30- and 40-year-old clear-cut areas. Along with the decomposition of pine and spruce stumps, the amount of P in stumps increased, but K and Ca were released, and the amount of Mg initially decreased and then increased. All nutrients, except K, accumulated in birch stumps during the first ten years, but were released thereafter. After 40 years of decomposition, pine and spruce stumps contained 180% and 202% of their initial amounts of P, respectively. In addition, the amounts of Mg were larger than the initial amounts in 40-year decomposed pine (126%) and spruce (202%) stumps. In contrast, birch stumps lost 64% and 75%, respectively, of their initial amounts of P and Mg over a 40-year period. The stumps of all the species were found to release K and Ca. Pine, spruce and birch stumps lost 48%, 64% and 87% of their initial amount of K, and 49%, 35% and 42% of their initial amount of Ca, respectively, during the 40-year period. The results indicate that decomposing stumps of the major tree species in Fennoscandian forests are long-term nutrient pools and they serve as P sinks, thus potentially reducing P leaching after clear-cutting.