Effect of drought experiments using roof installations on acidification/nitrification of soils

• Published in: Forest ecology and management 1998-02, Vol.101 (1), p.95-109
• Main Authors: Lamersdorf, N.P., Beier, C., Blanck, K., Bredemeier, M., Cummins, T., Farrell, E.P., Kreutzer, K., Rasmussen, L., Ryan, M., Weis, W., Xu, Y.-J.
• Format: Article
• Language: English
• Subjects: ACIDIFICACION; ACIDIFICATION; AZOTE; CHIMIE DU SOL; DROUGHT; Drought effects; MINERALISATION; MINERALIZACION; MINERALIZATION; NITRIFICACION; NITRIFICATION; Nitrification pulses; NITROGEN; Nitrogen mineralization; NITROGENO; Norway spruce; Nutrient losses; PICEA ABIES; QUIMICA DEL SUELO; Roof experiments; SECHERESSE; SEQUIA; SOIL CHEMISTRY; SOIL SOLUTION; Soil solution chemistry; SOLUCIONES DEL SUELO; SOLUTION DU SOL
• ISSN: 0378-1127; 1872-7042
• DOI: 10.1016/S0378-1127(97)00128-X

Within the framework of the EU-funded EXMAN (EXperimental MANipulation of Forest Ecosystems) project drought experiments were conducted at four different European Norway Spruce ( Picea abies (L.) Karst.) plantations in the year 1992–1995. The aim of the project was to investigate if there is an additional risk of soil acidification due to nitrification/acidification pulses after extended periods of summer droughts. The sites included (Ballyhooly/BH, southwest of Ireland. Klosterhede/KH, west coast of Denmark, Höglwald/HW, northwest of Munich, and Solling/SL, central Germany) cover considerable gradients of climatic and air pollution regimes. Artificial droughts were produced by using different types of roof constructions installed below the forest canopy (non-permanent constructions in BH and HW, permanent installations in KH and SL). Each drought was started in spring time and dry conditions were maintained until the soil water tension was below a potential of −700 hPa at 70 cm depth in the mineral soil. Results given are focused on changes in the soil solution concentrations during the rewetting of severely dried out soils. No marked nitrification pulses were observed after any of the droughts carried out at any site. Only single lysimeters/sample locations showed the hypothesized reaction with increasing aluminum concentrations and decreasing pH values, but spatial heterogeneity was high during rewetting. In the first soil solution samples after the drought, occasionally distinct peaks of NH 4 +, DOC and K +, and partly also N org and HPO 4 2− appeared. For the BH site the respective potassium concentrations increased 10 to 20 times compared to the level of the control plot. Presented data indicate a certain potential for nitrification pulses at the BH and KH site, but probably due to a fast root uptake, below the rooting zone no nitrate was determined. At the HW site, the drought induced reactions in the soil solution composition were only visible in humus water samples. At SL, nitrate concentrations were generally reduced at the drought plot. During rewetting in 1992 samples from a single lysimeter indicated a clear nitrification pulse. Applied flux calculations for SL showed a significant increase of the nitrate budget but a distinct decrease of the potassium budget. It is concluded that drought phases can influence the element cycling, but there seems to be no risk that forest soils will be subjected to pronounced acidification after summer droughts