Articles | Volume 5, issue 2
https://doi.org/10.5194/soil-5-205-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/soil-5-205-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Spatially resolved soil solution chemistry in a central European atmospherically polluted high-elevation catchment
Daniel A. Petrash
CORRESPONDING AUTHOR
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Frantisek Buzek
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Martin Novak
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Bohuslava Cejkova
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Pavel Kram
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Tomas Chuman
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Jan Curik
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Frantisek Veselovsky
Czech Geological Survey, Department of Rock Geochemistry,
Geologicka 6, 152 00, Prague 5, Czech Republic
Marketa Stepanova
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Oldrich Myska
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Pavla Holeckova
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
Leona Bohdalkova
Czech Geological Survey, Department of Environmental Geochemistry
and Biogeochemistry, Geologicka 6, 152 00, Prague 5, Czech Republic
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Daniel A. Petrash, Ingrid M. Steenbergen, Astolfo Valero, Travis B. Meador, Tomáš Pačes, and Christophe Thomazo
Biogeosciences, 19, 1723–1751, https://doi.org/10.5194/bg-19-1723-2022, https://doi.org/10.5194/bg-19-1723-2022, 2022
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We spectroscopically evaluated the gradients of dissolved C, N, S, Fe and Mn in a newly formed redox-stratified lake. The lake features an intermediate redox state between nitrogenous and euxinic conditions that encompasses vigorous open sulfur cycling fuelled by the reducible Fe and Mn stocks of the anoxic sediments. This results in substantial bottom water loads of dissolved iron and sulfate. Observations made in this ecosystem have relevance for deep-time paleoceanographic reconstructions.
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We investigated the role that OM quality plays in the stability of the OM-Fe association in freshwater sediments. It was found that non-humic components enhance OM-Fe stability, while humic components enhance the reductive dissolution of OM-Fe. This information is useful for predicting the fate of OM-Fe in freshwater systems with discrete sources of OM. Stable OM-Fe complexes improve aqueous environments by reducing the release of greenhouse gases, heavy metals and excess nutrients, such as P.
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SOIL, 9, 623–640, https://doi.org/10.5194/soil-9-623-2023, https://doi.org/10.5194/soil-9-623-2023, 2023
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Biological N2 fixation helps to sustain carbon accumulation in peatlands and to remove CO2 from the atmosphere. Changes in N2 fixation may affect the dynamics of global change. Increasing inputs of reactive N from air pollution should lead to downregulation of N2 fixation. Data from three N-polluted peat bogs show an interplay of N2-fixation rates with 10 potential drivers of this process. N2 fixation was measurable only at one site characterized by high phosphorus and low sulfate availability.
Luboš Vrtiška, Jaromír Tvrdý, Jakub Plášil, Jiří Sejkora, Radek Škoda, Nikita V. Chukanov, Andreas Massanek, Jan Filip, Zdeněk Dolníček, and František Veselovský
Eur. J. Mineral., 34, 223–238, https://doi.org/10.5194/ejm-34-223-2022, https://doi.org/10.5194/ejm-34-223-2022, 2022
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The study of the original material of beraunite from the type locality Hrbek, Czech Rep., from collections of the TU Bergakademie Freiberg (Germany) and National Museum Prague (Czech Republic) proved the identity of the minerals beraunite and eleonorite. Because the name beraunite has priority, we consider the name eleonorite to be redundant and proposed to abolish it. The proposal 21-D approved by the IMA discredited eleonorite and accepted the formula of beraunite Fe3+6(PO4)4O(OH)4·6H2O.
Daniel A. Petrash, Ingrid M. Steenbergen, Astolfo Valero, Travis B. Meador, Tomáš Pačes, and Christophe Thomazo
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We spectroscopically evaluated the gradients of dissolved C, N, S, Fe and Mn in a newly formed redox-stratified lake. The lake features an intermediate redox state between nitrogenous and euxinic conditions that encompasses vigorous open sulfur cycling fuelled by the reducible Fe and Mn stocks of the anoxic sediments. This results in substantial bottom water loads of dissolved iron and sulfate. Observations made in this ecosystem have relevance for deep-time paleoceanographic reconstructions.
Nana O.-A. Osafo, Jiří Jan, Petr Porcal, Daniel A. Petrash, and Jakub Borovec
Biogeosciences Discuss., https://doi.org/10.5194/bg-2020-296, https://doi.org/10.5194/bg-2020-296, 2020
Manuscript not accepted for further review
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We investigated the role that OM quality plays in the stability of the OM-Fe association in freshwater sediments. It was found that non-humic components enhance OM-Fe stability, while humic components enhance the reductive dissolution of OM-Fe. This information is useful for predicting the fate of OM-Fe in freshwater systems with discrete sources of OM. Stable OM-Fe complexes improve aqueous environments by reducing the release of greenhouse gases, heavy metals and excess nutrients, such as P.
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Nonlinear turnover rates of soil carbon following cultivation of native grasslands and subsequent afforestation of croplands
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W. Marijn van der Meij
SOIL, 8, 381–389, https://doi.org/10.5194/soil-8-381-2022, https://doi.org/10.5194/soil-8-381-2022, 2022
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The development of soils and landscapes can be complex due to changes in climate and land use. Computer models are required to simulate this complex development. This research presents a new method to analyze and visualize the results of these models. This is done with the use of evolutionary pathways (EPs), which describe how soil properties change in space and through time. I illustrate the EPs with examples from the field and give recommendations for further use of EPs in soil model studies.
Kaihua Liao, Juan Feng, Xiaoming Lai, and Qing Zhu
SOIL, 8, 309–317, https://doi.org/10.5194/soil-8-309-2022, https://doi.org/10.5194/soil-8-309-2022, 2022
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The influence of the conversion from conventional tillage (CT) to conservation tillage (CS; including no tillage, NT, and reduced tillage, RT) on the saturated hydraulic conductivity (Ksat) of soils is not well understood and still debated. This study has demonstrated that quantifying the effects of tillage conversion on soil Ksat needed to consider experimental conditions, especially the measurement technique and conversion period.
Leigh Ann Winowiecki, Aida Bargués-Tobella, Athanase Mukuralinda, Providence Mujawamariya, Elisée Bahati Ntawuhiganayo, Alex Billy Mugayi, Susan Chomba, and Tor-Gunnar Vågen
SOIL, 7, 767–783, https://doi.org/10.5194/soil-7-767-2021, https://doi.org/10.5194/soil-7-767-2021, 2021
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Achieving global restoration targets requires scaling of context-specific restoration options on the ground. We implemented the Land Degradation Surveillance Framework in Rwanda to assess indicators of soil and land health, including soil organic carbon (SOC), erosion prevalence, infiltration capacity, and tree biodiversity. Maps of soil erosion and SOC were produced at 30 m resolution with high accuracy. These data provide a rigorous biophysical baseline for tracking changes over time.
Guillermo Hernandez-Ramirez, Thomas J. Sauer, Yury G. Chendev, and Alexander N. Gennadiev
SOIL, 7, 415–431, https://doi.org/10.5194/soil-7-415-2021, https://doi.org/10.5194/soil-7-415-2021, 2021
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We evaluated how sequestration of soil carbon changes over the long term after converting native grasslands into croplands and also from annual cropping into trees. Soil carbon was reduced by cropping but increased with tree planting. This decrease in carbon storage with annual cropping happened over centuries, while trees increase soil carbon over just a few decades. Growing trees in long-term croplands emerged as a climate-change-mitigating action, effective even within a person’s lifetime.
Abdul-Wahab Mossa, Dawd Gashu, Martin R. Broadley, Sarah J. Dunham, Steve P. McGrath, Elizabeth H. Bailey, and Scott D. Young
SOIL, 7, 255–268, https://doi.org/10.5194/soil-7-255-2021, https://doi.org/10.5194/soil-7-255-2021, 2021
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Zinc deficiency is a widespread nutritional problem in human populations, especially in sub-Saharan Africa (SSA). Crop Zn depends in part on soil Zn. The Zn status of soils from the Amahara region, Ethiopia, was quantified by measuring pseudo-total, available, soluble and isotopically exchangeable Zn, and soil geochemical properties were assessed. Widespread phyto-available Zn deficiency was observed. The results could be used to improve agronomic interventions to tackle Zn deficiency in SSA.
Mirjam Schaller, Igor Dal Bo, Todd A. Ehlers, Anja Klotzsche, Reinhard Drews, Juan Pablo Fuentes Espoz, and Jan van der Kruk
SOIL, 6, 629–647, https://doi.org/10.5194/soil-6-629-2020, https://doi.org/10.5194/soil-6-629-2020, 2020
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In this study geophysical observations from ground-penetrating radar with pedolith physical and geochemical properties from pedons excavated in four study areas of the climate and ecological gradient in the Chilean Coastal Cordillera are combined. Findings suggest that profiles with ground-penetrating radar along hillslopes can be used to infer lateral thickness variations in pedolith horizons and to some degree physical and chemical variations with depth.
Marijke Struijk, Andrew P. Whitmore, Simon R. Mortimer, and Tom Sizmur
SOIL, 6, 467–481, https://doi.org/10.5194/soil-6-467-2020, https://doi.org/10.5194/soil-6-467-2020, 2020
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Crop residues are widely available on-farm resources containing carbon and nutrients, but, as soil amendments, their decomposition does not always benefit the soil. We applied mixtures of crop residues that are chemically different from each other and found significantly increased soil organic matter and available nitrogen levels. Applying crop residue mixtures has practical implications involving the removal, mixing and reapplication rather than simply returning crop residues to soils in situ.
W. Marijn van der Meij, Arnaud J. A. M. Temme, Jakob Wallinga, and Michael Sommer
SOIL, 6, 337–358, https://doi.org/10.5194/soil-6-337-2020, https://doi.org/10.5194/soil-6-337-2020, 2020
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We developed a model to simulate long-term development of soils and landscapes under varying rainfall and land-use conditions to quantify the temporal variation of soil patterns. In natural landscapes, rainfall amount was the dominant factor influencing soil variation, while for agricultural landscapes, landscape position became the dominant factor due to tillage erosion. Our model shows potential for simulating past and future developments of soils in various landscapes and climates.
Andre Carnieletto Dotto, Jose A. M. Demattê, Raphael A. Viscarra Rossel, and Rodnei Rizzo
SOIL, 6, 163–177, https://doi.org/10.5194/soil-6-163-2020, https://doi.org/10.5194/soil-6-163-2020, 2020
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The objective of this study was to develop a soil grouping system based on spectral, climate, and terrain variables with the aim of developing a quantitative way to classify soils. To derive the new system, we applied the above-mentioned variables using cluster analysis and defined eight groups or "soil environment groupings" (SEGs). The SEG system facilitated the identification of groups with similar characteristics using not only soil but also environmental variables for their distinction.
Tino Colombi, Florian Walder, Lucie Büchi, Marlies Sommer, Kexing Liu, Johan Six, Marcel G. A. van der Heijden, Raphaël Charles, and Thomas Keller
SOIL, 5, 91–105, https://doi.org/10.5194/soil-5-91-2019, https://doi.org/10.5194/soil-5-91-2019, 2019
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The role of soil aeration in carbon sequestration in arable soils has only been explored little, especially at the farm level. The current study, which was conducted on 30 fields that belong to individual farms, reveals a positive relationship between soil gas transport capability and soil organic carbon content. We therefore conclude that soil aeration needs to be accounted for when developing strategies for carbon sequestration in arable soil.
Michael P. Ricketts, Rachel S. Poretsky, Jeffrey M. Welker, and Miquel A. Gonzalez-Meler
SOIL, 2, 459–474, https://doi.org/10.5194/soil-2-459-2016, https://doi.org/10.5194/soil-2-459-2016, 2016
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Soil microbial communities play a key role in the cycling of carbon (C) in Arctic tundra ecosystems through decomposition of organic matter (OM). Climate change predictions include increased temperature and snow accumulation, resulting in altered plant communities and soil conditions. To determine how soil bacteria may respond, we sequenced soil DNA from a long-term snow depth treatment gradient in Alaska. Results indicate that bacteria produce less OM-degrading enzymes under deeper snowpack.
Rebecca Swift, Liza Parkinson, Thomas Edwards, Regina Carr, Jen McComb, Graham W. O'Hara, Giles E. St. John Hardy, Lambert Bräu, and John Howieson
SOIL Discuss., https://doi.org/10.5194/soil-2016-33, https://doi.org/10.5194/soil-2016-33, 2016
Preprint retracted
Marcos H. Easdale
SOIL, 2, 129–134, https://doi.org/10.5194/soil-2-129-2016, https://doi.org/10.5194/soil-2-129-2016, 2016
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Zero Net Land Degradation (ZNLD) was proposed as a new global protocol to combat desertification. This framework aims at reducing the rate of global land degradation and increasing the rate of restoration of already degraded land. However, there is a narrow focus on land and soil, while an essential human dimension to the sustainability of drylands is lacking and should be more adequately tackled. I propose a complementary perspective based on the sustainable livelihood approach.
Jeffrey S. Buyer, Anne Schmidt-Küntzel, Matti Nghikembua, Jude E. Maul, and Laurie Marker
SOIL, 2, 101–110, https://doi.org/10.5194/soil-2-101-2016, https://doi.org/10.5194/soil-2-101-2016, 2016
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Savannas represent most of the world’s livestock grazing land and are suffering worldwide from bush encroachment and desertification. We studied soil under bush and grass in a bush-encroached savanna in Namibia. With bush removal, there were significant changes in soil chemistry and microbial community structure, but these changes gradually diminished with time. Our results indicate that the ecosystem can substantially recover over a time period of approximately 10 years following bush removal.
Alemayehu Adugna and Assefa Abegaz
SOIL, 2, 63–70, https://doi.org/10.5194/soil-2-63-2016, https://doi.org/10.5194/soil-2-63-2016, 2016
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The purpose of our study was to explore the effects of land use changes on the dynamics of soil properties and their implications for land degradation. The result indicates that cultivated land has a lower organic matter, total nitrogen, cation exchange capacity, pH, and exchangeable Ca2+ and Mg2+ contents than forestland and grazing land.
C. Thomas, A. Sexstone, and J. Skousen
SOIL, 1, 621–629, https://doi.org/10.5194/soil-1-621-2015, https://doi.org/10.5194/soil-1-621-2015, 2015
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Surface coal mining disrupts large areas of land and eliminates valuable hardwood forests. Restoring the land to a sustainable forest ecosystem with suitable soils is the goal of reclamation. Soil microbial activity is an indicator of restoration success. We found hydroseeding with herbaceous forage species and fertilization doubled tree growth and microbial biomass carbon (an indicator of microbial activity) compared to non-hydroseed areas. Hydroseeding is an important component of reclamation.
M. Holleran, M. Levi, and C. Rasmussen
SOIL, 1, 47–64, https://doi.org/10.5194/soil-1-47-2015, https://doi.org/10.5194/soil-1-47-2015, 2015
Cited articles
Aber, J. D., Nadelhoffer, K. J., Steudler, P., and Melillo, J. M.: Nitrogen
saturation in northern forest ecosystems: excess nitrogen from fossil fuel
combustion may stress the biosphere, Bioscience 39, 378–386, https://doi.org/10.2307/1311067, 1989.
Akselsson, C., Westling, O., Sverdrup, H., and Gundersen, P.: Nutrient and carbon
budgets in forest soils as decision support in sustainable forest
management, Forest Ecol. Manag., 238, 167–174, 2007.
Akselsson, C., Westling, O., Alveteg, M., Thelin, G., Fransson, A. M.,
and Hellsten, S.: The influence of N load and harvest intensity on the risk of P
limitation in Swedish forest soils, Sci. Total Environ., 404, 284–289,
2008.
Alewell, C.: Predicting Reversibility of Acidification: The European Sulfur
Story, Water Air Soil Poll., 130, 1271–1276, 2001.
Armbruster, M., Abiy, M., and Feger, K. H.: The biogeochemistry of two forested
catchments in the Black Forest and the eastern Ore Mountains
(Germany), Biogeochemisty, 65, 341–368, 2003.
Armbruster, M. and Feger, K.-H.: Temporal trends in the chemical composition of
precipitation, soil seepage and stream water in two forested catchments in
the Black Forest and the eastern Ore, Monit. Nat. Environ. 5, 129–148, 2004.
Basu, N. B, Destouni, G., Jawitz, J. W., Thompson, S. E., Loukinova, N. V., Darracq, A., Zanardo, S., Yaeger, M., Sivapalan, M., Rinaldo, A., and Rao, P. S. C.: Nutrient loads exported from managed catchments reveal emergent
biogeochemical stationarity, Geoph. Res. Lett., 37, L23404, https://doi.org/10.1029/2010GL045168, 2010.
Beauchemin, S. and Simard, R. R.: Soil phosphorus saturation degree, review of
some indices and their suitability for P management in Québec, Canada,
Can. J. Soil Sci., 79, 615–625, 1999.
Blazkova, M.: Black Triangle – The Most Polluted Part of Central Europe, in:
Regional Approaches to Water Pollution in the Environment, edited by: Rijtema P. E. and Elias, V., NATO ASI Series 2, Environment, Kluwer Academic Publishers,
Dordrecht, the Netherlands, 20, 227–249,
https://doi.org/10.1007/978-94-009-0345-6_11, 1996.
Borovec, J. and Jan, J.: Approach for predicting P sorption/desorption
behaviour of potentially eroded topsoil in watercourses, Sci. Total Environ.,
624, 1316–1324, 2018.
Brantley, S. L., White, T., West, N., Williams, J. Z., Forsythe, B., Shapich,
D., Kaye, J., Lin, H., Shi, Y., Kaye, M., and Herndon, E.: Susquehanna Shale
Hills Critical Zone Observatory, Shale Hills in the context of Shaver's
Creek watershed, Vadose Zone J., 17, 180092, https://doi.org/10.2136/vzj2018.04.0092,
2018.
Buzek, F., Hanzlik, J., Hruby, M., and Tryzna, P.: Evaluation of the runoff
components on the slope of an open-cast mine by means of environmental
isotopes 18O and T, J. Hydrol., 127, 23–36, 1991.
Buzek, F., Hruska, J., and Kram, P.: Three component model of runoff generation,
Lysina catchment, Czech Republic, Water Air Soil Poll., 79, 391–408 1995.
Buzek, F., Bystricky, V., Kadlecova, R., Kvitek, T., Ondr, P., Sanda, M., Zajicek, A., and Zlabek, P.: Application of
two-component model of drainage discharge to nitrate contamination, J.
Contam. Hydrol., 106, 99–117, 2009.
CENIA: Zpráva o životním prostředí České republiky, Prague, Czech Republic, available at:
https://www.cenia.cz/wp-content/uploads/2019/03/Zprava-o-zivotnim-prostredi-Ceske-republiky_2017.pdf (last access: 5 May 2019), 2017.
Don, J., Skacel, J., and Gotowala, R.: The boundary zone of the East and West
Sudetes on the 1 : 50 000 scale geological map of the Velke Vrbno, Stare Mesto
and Snieżnik Metamorphic Units, Geologia Sudetica 35, 25–59, 2003.
Galloway, J. N., Aber, J. D., Erisman, J. W., Seitzinger, S. P., Howarth, R. W., Cowling, E. B., and Cosby, B. J.: The nitrogen cascade,
Bioscience, 53, 341–356, 2003.
Galloway, J. N., Townsend, J., Erisman, J. W., et al.: Transformation of the
nitrogen cycle: Recent trends, questions, and potential solutions,
Science, 320, https://doi.org/10.1126/science.1136674, 889–892, 2008.
Godsey, S. E., Kirchner, J. W., and Clow, D. W.: Concentration–discharge
relationships reflect chemostatic characteristics of US catchments, Hydrol.
Process., 23, 1844–1864, 2009.
Gradowski, T. and Thomas, S. C.: Responses of Acer saccharum canopy trees and samplings to P,
K and lime additions under high N deposition, Tree Physiol., 28, 173–185,
2008.
Gundersen, P., Schmidt, I. K., and Raulund-Rasmussen, K.: Leaching of nitrate
from temperate forests effects of air pollution and forest management,
Environ. Rev., 14, 1–57, 2006.
Heuck, C. and Spohn, M.: Carbon, nitrogen and phosphorus net mineralization in
organic horizons of temperate forests, stoichiometry and relations to
organic matter quality, Biogeochemistry, 131, 229–242, 2016.
Holmberg, M., Aherne, J., Austnes, K., Beloica, J., de Marco, A., Dirnböck,
T., Fornasier, F., Goergen, K., Futter, M., Lindroos, A.-J., Kram, P.,
Neirynck, J., Pecka, T., Posch, M., Rowe, E., Scheuschner, T., Schlutow, A.,
Valinia, S., and Forsius, M.: Forest soil C, N and pH response to N and S
deposition and climate change a modelling study at European LTER sites, Sci.
Total Environ., 640–641, 387–399, 2018.
Hruška, J. and Krám, P.: Modelling long-term changes in stream water and soil chemistry in catchments with contrasting vulnerability to acidification (Lysina and Pluhuv Bor, Czech Republic), Hydrol. Earth Syst. Sci., 7, 525–539, https://doi.org/10.5194/hess-7-525-2003, 2003.
Hruska, J., Cudlin, P., and Kram, P.: Relationship between Norway spruce status
and soil solution base cations/aluminium ratios in the Czech Republic, Water, Air Soil Poll., 130, 983–988, 2001, 2001.
Hume, A. M., Chen, H. Y. H., and Taylor, A. R.: Intensive forest harvesting
increases susceptibility of northern forest soils to carbon, nitrogen and
phosphorus loss, J. Appl. Ecol., 55, 246–255, 2018.
Huntington, T. G., Ryan, D. F., and Hamburg, S. P.: Estimating soil nitrogen and
carbon pools in a northern hardwood forest ecosystem, Soil Sci. Soc. Am. J.,
52, 1162–1167, 1988.
Johnson, J., Graf Pannatier, E., Carnicelli, S., Cecchini, G., Clarke, N.,
Cools, N., Hansen, K., Meesenburg, H., Nieminen, T. M., Pihl‐Karlsson, G., and Titeux, H.: The response of soil solution
chemistry in European forests to decreasing acid deposition, Glob. Change
Biol., 24, 3603–3619, 2018.
Kram, P., Hruska, J., Wenner, B. S., Driscoll, C. T., and Johnson, C. E.: The
biogeochemistry of basic cations in two forest catchments with contrasting
lithology in the Czech Republic, Biogeochemistry, 37, 173–202, 1997.
Kram, P., Hruska, J., and Bishop, K.: Monitoring and modeling of long-term changes
of streamwater chemistry in two small catchments with contrasting
vulnerability to acidification, UNESCO Technical Documents in Hydrology, 67,
197–202, 2003.
Kram, P., Hruska, J., and Shanley, J. B.: Streamwater chemistry in three
contrasting monolithologic Czech catchments, Appl. Geochem., 27,
1854–1863, 2012.
Kolar, T., Cermak, P., Oulehle, F., Trnka, M., Stepanek, P., Cudlin, P.,
Hruska, J., Büntgen, U., and Rybnicek, M.: Pollution control enhanced spruce
growth in the “Black Triangle” near the Czech-Polish border, Sci. Total
Environ., 538, 703–711, 2015.
Kopacek, J., Prochazkova, L., Stuchlik, E., and Blazka P.: The nitrogen phosphorus relationship in mountain lakes: influence of atmospheric input, watershed, and pH, Limnol. Oceanogr. 40, 930–937, 1995.
Kopacek, J., Hejzlar, J., Kram, P., Oulehle, F., and Posch, M.: Effect of
industrial dust on precipitation chemistry in the Czech Republic Central
Europe from 1850 to 2013, Water Res., 103, 30–43, 2015.
Lovett, G. and Goodale, C.: A new conceptual model of nitrogen saturation based on
experimental nitrogen addition to an oak forest, Ecosystems, 14, 615–631,
2011.
MacDonald, J. A., Dise, N. B., Matzner, E., Armbruster, M., Gundersen, P., and Forsius, M.: Nitrogen input together with ecosystem nitrogen enrichment predict nitrate leaching from European forests, Global Change Biol. 8, 1028–1033, 2002.
Maloszewski, P. and Zuber, A.: Determining the turnover time of groundwater
systems with the aid of environmental tracers, J. Hydrol., 573–574, 207–231,
https://doi.org/10.1016/0022-1694(82)90147-0, 1982.
Manderscheid, B., Matzner, E., Meiwes, K. J., and Xu, Y.-J.: Long-Term Development
of Element Budgets in a Norway spruce (Picea abies L. Karst) Forest of the German
Solling Area, Water Air Soil Poll. 79, 3–18, 1995.
Manderscheid, B. and Matzner, E.: Spatial and Temporal Variation of Soil
Solution Chemistry and Ion Fluxes through the Soil in a Mature Norway-Spruce
(Picea abies L. Karst Stand), Biogeochemistry, 30, 99–114, 1995.
Matschullat, J., Andreae, H., Lessmann, D., and Malessa, V. S. U.: Catchment
acidification from the top down, Environ. Pollut., 77, 143–150, 1992.
Mayer, B., Prietzel, J., and Krouse, H. R.: The influence of sulfur deposition
rates on sulfate retention patterns and mechanisms in aerated forest soils,
Appl. Geochem., 16, 1003–1019, https://doi.org/10.1016/S0883-2927(01)00010-5, 2001.
McDowell, W. H., Magill, A. H., Aitkenhead-Peterson, J. A., Aber, J. D., Merriam, J. L., and Kaushal, S. S.: Effects of
chronic nitrogen amendment on dissolved organic matter and inorganic
nitrogen in soil solution, Forest Ecol. Manag., 196, 29–41, 2004.
McIntosh, J. C., Schaumberg, C., Perdrial, J., Harpold, A.,
Vázquez-Ortega, A., Rasmussen, C., Vinson, D., Zapata-Rios, X., Brooks,
P. D., Meixner, T., Pelletier, J., Derry, L., and Chorover, J.: Geochemical
evolution of the Critical Zone across variable time scales informs
concentration-discharge relationships: Jemez River Basin Critical Zone
Observatory, Water Resour. Res., 53, 4169–4196, 2017.
Monteith, D. T., Stoddard, J. L., Evans, C. D., de Wit, H. A., Forsius, M., Høgåsen, T., Wilander, A., Skjelkvåle, B. L., Jeffries, D. S., Vuorenmaa, J., and Keller, B.:
Dissolved organic carbon trends resulting from changes in atmospheric
deposition chemistry, Nature, 450, 537–540, 2007.
Moore, J., Lichtner, P. C., White, A. F., and Brantley, S. L.: Using a reactive
transport model to elucidate differences between laboratory and field
dissolution rates in regolith, Geochim. Cosmochim. Ac., 93, 235–261,
2012.
Mörth, C.-M., Torssander, P., Kjønaas, O. J., Stuanes, A. O., Moldan, F., and Giesler, R.: Mineralization of
organic sulfur delays recovery from anthropogenic acidification, Environ.
Sci. Technol. 39, 5234–5240, 2005.
Navratil, T., Kurz, D., Kram, P., Hofmeister, J., and Hruska, J: Acidification and recovery of soil
at a heavily impacted forest catchment (Lysina, Czech Republic) – SAFE
modeling and field results, Ecol. Model., 205, 464–474, https://doi.org/10.1016/j.ecolmodel.2007.03.008, 2007.
Nieminen, T., De Vos, B., Cools, N., König, N., Fischer, R., Iost, S., Meesenburg, H., Nicolas, M., O'Dea, P., Cecchini, G., Ferretti, M., De La Cruz, A., Derome, K., and Lindroos, A. J.: Part XI: Soil
solution collection and analysis, in: edited by: UNECE ICP Forests Programme
Co-ordinating Centre, in: Manual on methods and criteria for harmonized
sampling, assessment, monitoring and analysis of the effects of air
pollution on forests, Thunen Institute of Forest
Ecosystems, Eberswalde, Germany, 2016.
Novak, M., Kirchner, J. W., Groscheova, H., Havel, M., Cerný, J., Krejčc, R., and Buzek, F.: Sulfur isotope
dynamics in two Central European watersheds affected by high atmospheric
deposition of SOx, Geochim. Cosmochim. Ac., 64, 367–383,
https://doi.org/10.1016/0022-1694(82)90147-0, 2000.
Novak, M., Jackova, I., and Prechova, E.: Temporal trends in the isotope
signature of air-borne sulfur in Central Europe, Environ. Sci. Technol., 35,
255–260, https://doi.org/10.1021/es0000753, 2001.
Novak, M., Kirchner, J. W., Fottova, D., Prechova, E., Jackova, I., Kram, P., and Hruska, J.: Isotopic evidence for
processes of sulfur retention/release in 13 forested catchments spanning a
strong pollution gradient Czech Republic, central Europe, Global Biogeochem.
Cy., 19, GB4012, https://doi.org/10.1029/2004GB002396, 2005.
Palmer, S. M., Wellington, B. I., Johnson, C. E., and Driscoll, C. T.: Landscape
influences on aluminum and dissolved organic carbon in streams draining the
Hubbard Brook valley, New Hampshire, USA, Hydrol. Process., 19, 1751–1769,
2005.
Perakis, S. S. and Hedin, L. O.: Nitrogen loss from unpolluted South American
forests mainly via dissolved organic compounds, Nature, 415, 416–419, 2002.
Oulehle, F., Hofmeister, J., Cudlin, P., and Hruska, J: The effect of reduced
atmospheric deposition on soil and soil solution chemistry at a site
subjected to long-term acidification, Nacetin, Czech Republic, Sci. Total
Environ., 370, 532–544, 2006.
Oulehle, F., Chuman, T., Hruska, J., Kram, P., McDowell, W.H., Myska, O.,
Navratil, T., Tesar, M.: Recovery from acidification alters concentrations
and fluxes of solutes from Czech catchments, Biogeochemistry, 132, 251–272,
2017.
Rosenstock, N., Berner, C., Smits, M. M., Kram, P., and Wallander, H.: The role of phosphorus, magnesium and potassium availability in soil fungal exploration of mineral nutrient sources in Norway spruce forests, New Phytol., 211, 542–553, 2016.
Schoumans, O. F.: Determination of the degree of phosphate saturation in
non-calcareous soils, in: Methods of Phosphorus Analysis in Soils, Sediments
and Waters, edited by: Pierzynski, G. M., North Carolina State University,
Raleigh, NC, USA, 31–34, 2000.
Scott, E. E. and Rothstein, D. E.: The dynamic exchange of dissolved organic
matter percolating through six diverse soils, Soil Biol. Biochem.,
69, 83–92, 2014.
Siegenthaler, U.: Stable hydrogen and oxygen isotopes in the water cycle, in:
Lectures in Isotope Geology, edited by: Jager, E. and Hunzike, J. C., Springer-Verlag, Berlin, Germany, 264–273, 1979.
Smith, W. H.: Character and significance of forest tree root exudates,
Ecology, 57, 324–331, 1976.
van Miegroet, H. and Cole, D. W.: The impact of nitrification on soil
acidification and cation leaching in a red alder Alnus rubra ecosystem, J. Environ.
Qual., 13, 586–590, 1984.
Verstraeten, A., Neirynck, J., Cools, N., Roskams, P., Louette, G., De Neve, S., and Sleutel, S.: Multiple nitrogen saturation
indicators yield contradicting conclusions on improving nitrogen status of
temperate forests, Ecol. Indic., 82, 451–462, 2017.
Vega, M., Pardo, R., Barrado, E., and Deban, L.: Assessment of seasonal and
polluting effects on the quality of river water by exploratory data
analysis, Water Res., 32, 3581–3592, 1998.
Waldner, P., Marchetto, A., Thimonier, A., Schmitt, M., Rogora, M., Granke, O., Mues, V., Hansen, K., Karlsson, G. P., Žlindra, D., and Clarke, N.: Detection of temporal
trends in atmospheric deposition of inorganic nitrogen and sulphate to
forests in Europe, Atmos. Environ., 95, 363–374, 2014.
Waldner, P., Thimonier, A., Graf Pannatier, E., Etzold, S., Schmitt, M., Marchetto, A., Rautio, P., Derome, K., Nieminen, T. M., Nevalainen, S., and Lindroos, A. J.: Exceedance of
critical loads and of critical limits impacts tree nutrition across Europe,
Ann. For. Sci., 72, 929–939, 2015.
Wesselink, L. G., Meiwes, K. J., Matzner, E., and Stein, A.: Long-term changes in
water and soil chemistry in spruce and beech Forests, Solling, Germany,
Environ, Sci. Technol., 29, 51–58, 1995.
Winchester, J. A., Pharaoh, T. C., and Verniers, J.: Palaeozoic amalgamation of
Central Europe, Geol. Soc. Spec. Publ., 201, 237–277, 2002.
Short summary
Some 30 years after peak pollution-related soil acidification occurred in central Europe, the forest ecosystem of a small V-shaped mountain valley, UDL, was still out of chemical balance relative to the concurrent loads of anions and cations in precipitation. The spatial variability in soil solution chemistry provided evidence pointing to substrate variability, C and P bioavailability, and landscape as major controls on base metal leaching toward the subsoil level in N-saturated catchments.
Some 30 years after peak pollution-related soil acidification occurred in central Europe, the...