Throughfall deposition is an important pathway via which particles, aerosols and gases can move from the atmosphere to the forest floor, which can greatly impact forest biodiversity and functioning. Although throughfall deposition biochemistry has been well studied in forest ecosystems, less is known about how throughfall deposition is modified by tree species diversity. To disentangle the effects of tree species identity and diversity on throughfall deposition, we installed rain gauges in a 10-year-old tree diversity experiment. With these rain gauges, we monitored throughfall biweekly, and performed chemical analyses monthly for all the major ions (Na, Cl, SO-S, K, Ca, Mg, PO-P, NO-N and NH-N), for a period of one year. Based on these data, we analysed species identity (i.e. whether throughfall deposition depended on the tree species present in the overstorey), and diversity effects (i.e. whether throughfall deposition depended on tree species richness). We confirmed species identity effects on throughfall deposition. Presence of pine led to higher throughfall deposition of inorganic nitrogen, and lower amounts of phosphorus, calcium and magnesium reaching the forest floor. Additionally, species characteristics and stand structural characteristics, i.e. basal area and canopy cover, emerged as key factors driving throughfall deposition of sodium, chloride, nitrate, sulphate and potassium. Tree species diversity effects on throughfall deposition were also present, mostly via increased basal area and canopy cover, leading to increased throughfall deposition of inorganic nitrogen, sulphate, chloride, sodium and potassium. Our findings thus suggest that tree species diversity enhances throughfall deposition of most ions that we analysed, potentially increasing nutrient availability for below-canopy plant communities. Given that inorganic nitrogen and sulphur are major atmospheric pollutants, increased deposition in mixed plots might affect ecosystem functioning. Further research will be needed to determine the extent of this impact.
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http://dx.doi.org/10.1016/j.scitotenv.2022.156947 | DOI Listing |
Sci Total Environ
January 2025
Forest Ecology and Forest Management Group, Wageningen University and Research Centre, PO Box 47, Wageningen 6700AA, the Netherlands.
Atmospheric nutrient deposition plays a crucial role in supplying nutrients to forests on poor soils, making it a key factor in maintaining nutrient stocks and forest productivity. We compared total atmospheric deposition in production forests of European beech (Fagus sylvatica), Douglas fir (Pseudotsuga menziesii), and Scots pine (Pinus sylvestris) by measuring bulk deposition and throughfall while accounting for canopy exchange. We assessed the differences in total deposition resulting from forest management practices such as high-thinning, shelterwood and clearcutting, on forest structure for both macronutrients and micronutrients in areas exposed to high nutrient deposition.
View Article and Find Full Text PDFPlants (Basel)
August 2024
Forestry and Game Management Research Institute (FGMRI), Department of Forest Ecology, Strnady 136, 25202 Jíloviště, Czech Republic.
The Ore Mountains were historically one of the most polluted areas in Europe, where high sulphur dioxide concentrations and a high level of atmospheric deposition led to a vast decline in Norway spruce stands in the mountain ridge plateau. In this article, we evaluate the trends in the atmospheric deposition load, soil chemistry, tree nutrition, crown defoliation and height increment in a network of twenty research plots monitored for last thirty years in this region. The decrease in sulphur and nitrogen deposition was most pronounced at the end of 1990s.
View Article and Find Full Text PDFTree Physiol
September 2024
Research and Innovation Centre, Fondazione Edmund Mach, 38010 San Michele all'Adige, TN, Italy.
Atmospheric nitrogen (N) deposition has notably increased since the industrial revolution, doubling N inputs to terrestrial ecosystems. This could mitigate N limitations in forests, potentially enhancing productivity and carbon sequestration. However, excessive N can lead to forest N saturation, causing issues like soil acidification, nutrient imbalances, biodiversity loss, increased tree mortality and a potential net greenhouse gas emission.
View Article and Find Full Text PDFEnviron Res
December 2024
Institute for Adriatic Crops and Karst Reclamation, Put Duilova 11, 21000, Split, Croatia. Electronic address:
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