Bulk deposition and throughfall fluxes of elements in the Bohemian Forest (central Europe) from 1998 to 2009

We measured element concentrations and fluxes in bulk precipitation (two sites) and throughfall (four sites) in Norway spruce mountain stands in the Bohemian Forest (Czech Republic) from 1991–2009, with the aim to evaluate net atmospheric inputs of nutrients to the area, and long-term trends in acidic deposition. The average net atmospheric inputs of nutrients were 11, 4, 9, 62, 62, 45, 26, and 0.7-1.3 mmol/m2/yr for Ca, Mg, K, nitrate, ammonium, total organic N, S, and total P (TP), respectively. The TP deposition was affected by a notable contribution from local dust and pollen sources. Throughfall pH increased from 3.6–3.7 in 1991–1994 to 4.7–5.0 in 2006–2009, due to average declines in the sulphate plus nitrate concentrations by 202 µeq/l and the H concentration by 147 µeq/l. The decline in throughfall concentrations of sulphate (by 184 µeq/l) was the dominant driving force for the pH increase.

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Publication Details

Journal
Työväentutkimus Vuosikirja
Published
2024-12-12
DOI
https://doi.org/10.60910/sjtg-bays
Citations
28
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.38
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article

Bulk deposition and throughfall fluxes of elements in the Bohemian Forest (central Europe) from 1998 to 2009

Jiřı́ Kopáček, Petr Porcal, Josef Hejzlar, Jan Turek
28 citations
Työväentutkimus Vuosikirja
Geology and Paleoclimatology Research
0.38
article

Bulk deposition and throughfall fluxes of elements in the Bohemian Forest (central Europe) from 1998 to 2009

Jiřı́ Kopáček, Petr Porcal, Josef Hejzlar, Jan Turek
article en
28 citations

Abstract

We measured element concentrations and fluxes in bulk precipitation (two sites) and throughfall (four sites) in Norway spruce mountain stands in the Bohemian Forest (Czech Republic) from 1991–2009, with the aim to evaluate net atmospheric inputs of nutrients to the area, and long-term trends in acidic deposition. The average net atmospheric inputs of nutrients were 11, 4, 9, 62, 62, 45, 26, and 0.7-1.3 mmol/m2/yr for Ca, Mg, K, nitrate, ammonium, total organic N, S, and total P (TP), respectively. The TP deposition was affected by a notable contribution from local dust and pollen sources. Throughfall pH increased from 3.6–3.7 in 1991–1994 to 4.7–5.0 in 2006–2009, due to average declines in the sulphate plus nitrate concentrations by 202 µeq/l and the H concentration by 147 µeq/l. The decline in throughfall concentrations of sulphate (by 184 µeq/l) was the dominant driving force for the pH increase.

Työväentutkimus Vuosikirja
Life in Land
Openalex Percentile: Top 47%
Geology and Paleoclimatology Research
0.38
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