The chemical composition of throughfall beneath oak, birch and pine canopies in Northwest Germany

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Martina Herrmann
  • Jürgen Pust
  • Richard Pott

Research Organisations

External Research Organisations

  • LWL-Museum für Naturkunde
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Details

Original languageEnglish
Pages (from-to)273-285
Number of pages13
JournalPlant ecology
Volume184
Issue number2
Early online date8 Dec 2005
Publication statusPublished - Jun 2006

Abstract

The chemical composition of rainwater is altered upon its passage through tree canopies. In order to investigate how rainwater chemistry is affected by canopy-dependent processes in characteristic forest types of Northwest German sandy lowland regions - oak-birch-forests, Betula pubescens Ehrh. swamp forests, and stands of Pinus sylvestris L. - comparative studies on the chemical composition of throughfall were carried out at seven forest sites, situated in close proximity within a nature reserve. Additionally, rainwater was sampled at three heathland sites for analysis of open-field precipitation and at three sites along an oak-birch-forest edge. Throughfall concentrations of most of the parameters analysed were significantly higher than open-field concentrations, especially with regard to electric conductivity, NH4-N, K +, and KMnO4-index. Ion concentrations in throughfall were the lowest in a 10-year-old stand of Betula pendula Roth. and Pinus sylvestris and in a Betula pubescens swamp forest and were highest beneath a stand of Pinus sylvestris. Except for Na+, Cl-, and NO 3 - , ion concentrations in both throughfall and open-field precipitation increased during the growing season (May-October). In throughfall, Ca2+, Mg2+, K+, and Mn2+ were strongly correlated. Enrichment ratios between throughfall and open-field deposition varied among sites and elements and were the highest for K ‰+, Mg2‰+, and Mn2‰+. Estimates of canopy leaching indicated high leaching rates of K ‰+ and Mn2‰+ and moderate leaching of Mg2‰+. The contribution of foliar leaching to throughfall deposition was higher at the deciduous than at the coniferous stands.

Keywords

    Betula pubescens swamp forest, Foliar leaching, Oak-birch-forests, Rainwater chemistry, Stands of Pinus sylvestris

ASJC Scopus subject areas

Cite this

The chemical composition of throughfall beneath oak, birch and pine canopies in Northwest Germany. / Herrmann, Martina; Pust, Jürgen; Pott, Richard.
In: Plant ecology, Vol. 184, No. 2, 06.2006, p. 273-285.

Research output: Contribution to journalArticleResearchpeer review

Herrmann M, Pust J, Pott R. The chemical composition of throughfall beneath oak, birch and pine canopies in Northwest Germany. Plant ecology. 2006 Jun;184(2):273-285. Epub 2005 Dec 8. doi: 10.1007/s11258-005-9072-5
Herrmann, Martina ; Pust, Jürgen ; Pott, Richard. / The chemical composition of throughfall beneath oak, birch and pine canopies in Northwest Germany. In: Plant ecology. 2006 ; Vol. 184, No. 2. pp. 273-285.
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abstract = "The chemical composition of rainwater is altered upon its passage through tree canopies. In order to investigate how rainwater chemistry is affected by canopy-dependent processes in characteristic forest types of Northwest German sandy lowland regions - oak-birch-forests, Betula pubescens Ehrh. swamp forests, and stands of Pinus sylvestris L. - comparative studies on the chemical composition of throughfall were carried out at seven forest sites, situated in close proximity within a nature reserve. Additionally, rainwater was sampled at three heathland sites for analysis of open-field precipitation and at three sites along an oak-birch-forest edge. Throughfall concentrations of most of the parameters analysed were significantly higher than open-field concentrations, especially with regard to electric conductivity, NH4-N, K +, and KMnO4-index. Ion concentrations in throughfall were the lowest in a 10-year-old stand of Betula pendula Roth. and Pinus sylvestris and in a Betula pubescens swamp forest and were highest beneath a stand of Pinus sylvestris. Except for Na+, Cl-, and NO 3 - , ion concentrations in both throughfall and open-field precipitation increased during the growing season (May-October). In throughfall, Ca2+, Mg2+, K+, and Mn2+ were strongly correlated. Enrichment ratios between throughfall and open-field deposition varied among sites and elements and were the highest for K ‰+, Mg2‰+, and Mn2‰+. Estimates of canopy leaching indicated high leaching rates of K ‰+ and Mn2‰+ and moderate leaching of Mg2‰+. The contribution of foliar leaching to throughfall deposition was higher at the deciduous than at the coniferous stands.",
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AU - Herrmann, Martina

AU - Pust, Jürgen

AU - Pott, Richard

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N2 - The chemical composition of rainwater is altered upon its passage through tree canopies. In order to investigate how rainwater chemistry is affected by canopy-dependent processes in characteristic forest types of Northwest German sandy lowland regions - oak-birch-forests, Betula pubescens Ehrh. swamp forests, and stands of Pinus sylvestris L. - comparative studies on the chemical composition of throughfall were carried out at seven forest sites, situated in close proximity within a nature reserve. Additionally, rainwater was sampled at three heathland sites for analysis of open-field precipitation and at three sites along an oak-birch-forest edge. Throughfall concentrations of most of the parameters analysed were significantly higher than open-field concentrations, especially with regard to electric conductivity, NH4-N, K +, and KMnO4-index. Ion concentrations in throughfall were the lowest in a 10-year-old stand of Betula pendula Roth. and Pinus sylvestris and in a Betula pubescens swamp forest and were highest beneath a stand of Pinus sylvestris. Except for Na+, Cl-, and NO 3 - , ion concentrations in both throughfall and open-field precipitation increased during the growing season (May-October). In throughfall, Ca2+, Mg2+, K+, and Mn2+ were strongly correlated. Enrichment ratios between throughfall and open-field deposition varied among sites and elements and were the highest for K ‰+, Mg2‰+, and Mn2‰+. Estimates of canopy leaching indicated high leaching rates of K ‰+ and Mn2‰+ and moderate leaching of Mg2‰+. The contribution of foliar leaching to throughfall deposition was higher at the deciduous than at the coniferous stands.

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