The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland

The chemical composition of throughfall depends on the age of the Norway spruce (Picea abies Karst) stands and season of the year. The pH of throughfall decreased and the amount of hydrogen ion in throughfall deposited to the soil increased with increasing age of spruce stands, especially in the win...

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Main Authors: Stanislaw Malek, Aleksander Astel
Format: Article
Language:English
Published: Hindawi Limited 2007-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1100/tsw.2007.90
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spelling doaj-d622ada83eae40aebd30cf27d161e1542020-11-25T01:39:52ZengHindawi LimitedThe Scientific World Journal1537-744X2007-01-01718119110.1100/tsw.2007.90The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern PolandStanislaw Malek0Aleksander Astel1Department of Forest Ecology, Forest Faculty, Agricultural University of Cracow, Al. 29 Listopada 46, 31–425 Krakêw, PolandEnvironmental Chemistry Research Unit, Biology and Environmental Protection Institute, Pomeranian Academy, 22a Arciszewskiego Str., 76-200 Słupsk, PolandThe chemical composition of throughfall depends on the age of the Norway spruce (Picea abies Karst) stands and season of the year. The pH of throughfall decreased and the amount of hydrogen ion in throughfall deposited to the soil increased with increasing age of spruce stands, especially in the winter season. Concentrations of K+, H+, SO42−, Mn2+, and NH4+ in throughfall were higher than bulk precipitation for the whole year and K+, H+, and Mn2+ concentrations were higher in throughfall in winter and the growing season. This indicates that these ions were washed out or washed from the surface of needles and/or the bark, and that NO3−, NH4+, Ca2+, Mg2+, Fe2+, and Zn2+ were absorbed in the canopy. The effect of high nitrogen deposition, above critical loads, and an increase in the amount of sulfur and in the sum of the strong acids (S-SO42− and N-NO3−) that reached the soil with throughfall may have implications for the vitality of spruce stands, especially in older age classes. The application of Principal Component Analysis (PCA) has led to identification of five factors responsible for the data structure (“mineral dust”, “acidic emissions”, “heavy metals-dust particles”, “ammonium [NH4+]”, and “H+”). They explain more than 60% of the total variance system. The strong positive correlation between stand age class and ionic concentrations in throughfall occurs for all year and the winter period for ions within the following categories: “acidic emissions”, SO42− + NO3−; “heavy metals-dust particles”, Fe2+ + Mn2+ + Zn2+; “mineral dust”, Na+ + K+ + Ca+2 + Mg2+; “NH4+”; and “H+”. The strength of the relationship decreases in the growing period, probably due to processes occurring in the canopy (adsorption, leaching, etc.).http://dx.doi.org/10.1100/tsw.2007.90
collection DOAJ
language English
format Article
sources DOAJ
author Stanislaw Malek
Aleksander Astel
spellingShingle Stanislaw Malek
Aleksander Astel
The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland
The Scientific World Journal
author_facet Stanislaw Malek
Aleksander Astel
author_sort Stanislaw Malek
title The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland
title_short The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland
title_full The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland
title_fullStr The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland
title_full_unstemmed The Effect of Stand Age on Throughfall Chemistry in Spruce Stands in the Potok Dupniański Catchment in the Silesian Beskid Mountains, Southern Poland
title_sort effect of stand age on throughfall chemistry in spruce stands in the potok dupniański catchment in the silesian beskid mountains, southern poland
publisher Hindawi Limited
series The Scientific World Journal
issn 1537-744X
publishDate 2007-01-01
description The chemical composition of throughfall depends on the age of the Norway spruce (Picea abies Karst) stands and season of the year. The pH of throughfall decreased and the amount of hydrogen ion in throughfall deposited to the soil increased with increasing age of spruce stands, especially in the winter season. Concentrations of K+, H+, SO42−, Mn2+, and NH4+ in throughfall were higher than bulk precipitation for the whole year and K+, H+, and Mn2+ concentrations were higher in throughfall in winter and the growing season. This indicates that these ions were washed out or washed from the surface of needles and/or the bark, and that NO3−, NH4+, Ca2+, Mg2+, Fe2+, and Zn2+ were absorbed in the canopy. The effect of high nitrogen deposition, above critical loads, and an increase in the amount of sulfur and in the sum of the strong acids (S-SO42− and N-NO3−) that reached the soil with throughfall may have implications for the vitality of spruce stands, especially in older age classes. The application of Principal Component Analysis (PCA) has led to identification of five factors responsible for the data structure (“mineral dust”, “acidic emissions”, “heavy metals-dust particles”, “ammonium [NH4+]”, and “H+”). They explain more than 60% of the total variance system. The strong positive correlation between stand age class and ionic concentrations in throughfall occurs for all year and the winter period for ions within the following categories: “acidic emissions”, SO42− + NO3−; “heavy metals-dust particles”, Fe2+ + Mn2+ + Zn2+; “mineral dust”, Na+ + K+ + Ca+2 + Mg2+; “NH4+”; and “H+”. The strength of the relationship decreases in the growing period, probably due to processes occurring in the canopy (adsorption, leaching, etc.).
url http://dx.doi.org/10.1100/tsw.2007.90
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