Abstract
Aluminium (Al) speciation is a characteristic that can be used as a tool for describing the soil acidification process. The question that was answered is how tree species (beech vs spruce) and type of soil horizon affect Al speciation. Our hypotesis is that spruce and beech forest vegetation are able to modify the chemical characteristics of organic horizon, hence the content of Al species. Moreover, these characteristics are seasonally dependent. To answer these questions, a detailed chromatographic speciation of Al in forest soils under contrasting tree species was performed. The Jizera Mountains area (Czech Republic) was chosen as a representative mountainous soil ecosystem. A basic forestry survey was performed on the investigated area. Soil and precipitation samples (throughfall, stemflow) were collected under both beech and spruce stands at monthly intervals from April to November during the years 2008–2011. Total aluminium content and Al speciation, pH, and dissolved organic carbon were determined in aqueous soil extracts and in precipitation samples. We found that the most important factors affecting the chemistry of soils, hence content of the Al species, are soil horizons and vegetation cover. pH strongly affects the amount of Al species under both forests. Fermentation (F) and humified (H) organic horizons contain a higher content of water extractable Al and Al3+ compared to organo-mineral (A) and mineral horizons (B). With increasing soil profile depth, the amount of water extractable Al, Al3+ and moisture decreases. The prevailing water-extractable species of Al in all studied soils and profiles under both spruce and beech forests were organically bound monovalent Al species. Distinct seasonal variations in organic and mineral soil horizons were found under both spruce and beech forests. Maximum concentrations of water-extractable Al and Al3+ were determined in the summer, and the lowest in spring.
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Abbreviations
- A horizon:
-
Organo-mineral soil horizon
- Al(X)1+ :
-
Contains mainly Al(org.)≤1+ and Al(OH)2 +, Al(SO4)+, AlF2 +, etc.
- Al(Y)2+ :
-
Contains Al(OH)2+, (AlF)2+, etc.
- Al3+ :
-
Contains Al3+ and transformed Al hydroxy-polymers
- AlH2O :
-
Total water-extractable Al
- ANOVA:
-
Analysis of variance
- au CM:
-
Aluminic Cambisols
- B horizon:
-
Spodic or cambic mineral horizon
- DOC:
-
Dissolved organic carbon
- DOM:
-
Dissolved organic matter
- EMEP:
-
European Monitoring and Evaluation Programme
- et PZ:
-
Entic Podzol
- F horizon:
-
Fermentation organic horizon
- H horizon:
-
Humified organic horizon
- H. G.:
-
Homogenous group
- ha PZ:
-
Haplic Podzol
- HPLC-IC:
-
High-performance liquid chromatography equipped with ionic column
- IC:
-
Ion chromatography
- ICP:
-
Forest Manual International Co-operative Programme Forest Manual
- NOx:
-
Nitrogen oxides
- PRP:
-
Permanent research plots
- PVC:
-
Polyvinyl chloride
- rpm:
-
Revolutions per minute
- SOM:
-
Soil organic matter
- Std. dev.:
-
Standard deviation
- VOSS:
-
Type of throughfall collector with a zig-zag adapter
- w/v :
-
Weight per volume
- WRB:
-
World Reference Base for Soil Resources
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Acknowledgments
The research was supported by grants from the Internal Grant Agency of Czech University of Life Sciences Prague (CIGA) (no. 20132005), and the Ministry of Agriculture (no. QI92A216). We are also grateful to Foundation “Nadání Josefa, Marie a Zdeňky Hlávkových” for financial support. Special thanks belong to Petr Skřivan (Geological Institute AV ČR) for valuable advice. The authors declare that they have no conflict of interest.
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The all co-authors were informed about submitting of manuscript “The variations of aluminium species in mountainous forest soils and its implications to soil acidification” by Bradová, M., Tejnecký, V., Borůvka, L., Němeček, K., Ash, Ch., Šebek, O., Svoboda, M., Zenáhlíková, J. and Drábek, O. All co-authors consent with submission of this manuscript.
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Bradová, M., Tejnecký, V., Borůvka, L. et al. The variations of aluminium species in mountainous forest soils and its implications to soil acidification. Environ Sci Pollut Res 22, 16676–16687 (2015). https://doi.org/10.1007/s11356-015-4855-2
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DOI: https://doi.org/10.1007/s11356-015-4855-2