Articles | Volume 8, issue 1
https://doi.org/10.5194/soil-8-1-2022
© Author(s) 2022. 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-8-1-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Original research article
| 
12 Jan 2022
Original research article |
| 12 Jan 2022
| 12 Jan 2022
Phosphorus dynamics during early soil development in a cold desert: insights from oxygen isotopes in phosphate
Zuzana Frkova
University of Luxembourg, Faculty of Science, Technology and
Communication, 6, rue Richard Coudenhove-Kalergi, 1359, Luxembourg
Biology Centre of the Czech Academy of Sciences, Institute of
Hydrobiology, Na Sádkách 7, 370 05 České Budějovice,
Czech Republic
Chiara Pistocchi
Eco&Sols, Montpellier SupAgro, CIRAD, INRAE, IRD, 34060 Montpellier, France
Yuliya Vystavna
Biology Centre of the Czech Academy of Sciences, Institute of
Hydrobiology, Na Sádkách 7, 370 05 České Budějovice,
Czech Republic
Biology Centre of the Czech Academy of Sciences, Institute of Soil
Biology, Na Sádkách 7, 370 05 České Budějovice, Czech
Republic
Katerina Capkova
Biology Centre of the Czech Academy of Sciences, Institute of
Hydrobiology, Na Sádkách 7, 370 05 České Budějovice,
Czech Republic
Czech Academy of Sciences, Institute of Botany v.v.i., Dukelská
135, 379 82 Třeboň, Czech Republic
Jiri Dolezal
Czech Academy of Sciences, Institute of Botany v.v.i., Dukelská
135, 379 82 Třeboň, Czech Republic
Faculty of Science, University of South Bohemia, Na Zlaté stoce
1, 370 05, České Budějovice, Czech Republic
Federica Tamburini
CORRESPONDING AUTHOR
Institute of Agricultural Sciences, ETH Zurich, Research Station
Eschikon 33, 8315 Lindau, Switzerland
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Siobhan Staunton and Chiara Pistocchi
SOIL, 11, 389–394, https://doi.org/10.5194/soil-11-389-2025, https://doi.org/10.5194/soil-11-389-2025, 2025
Short summary
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Mineral phosphate is a finite resource, so ways must be found to optimise the use of native soil P. We have used isotopic dilution to assess how acidification and the addition of citrate or oxalate modify the lability of soil P in four contrasting soils from the Mediterranean region. Acidification did not mobilise soil P, whereas both carboxylate anions promoted soil-P lability. This suggests that soil amendments and the choice of crops that exude carboxylates could optimise P nutrition.
Kirill Korznikov, Dmitriy Kislov, Jiří Doležal, and Jan Altman
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-217, https://doi.org/10.5194/nhess-2024-217, 2025
Manuscript not accepted for further review
Short summary
Short summary
This study investigates the factors behind forest damage caused by extreme winter storm events. By combining satellite data and machine learning, we identified areas affected by the storm and assessed the risk of future disturbances. We found that snow accumulation on coniferous trees was a major cause of damage, with mixedwood forests being particularly vulnerable. Our research helps improve our understanding of forest vulnerabilities to extreme weather events.
Lin Yu, Silvia Caldararu, Bernhard Ahrens, Thomas Wutzler, Marion Schrumpf, Julian Helfenstein, Chiara Pistocchi, and Sönke Zaehle
Biogeosciences, 20, 57–73, https://doi.org/10.5194/bg-20-57-2023, https://doi.org/10.5194/bg-20-57-2023, 2023
Short summary
Short summary
In this study, we addressed a key weakness in current ecosystem models regarding the phosphorus exchange in the soil and developed a new scheme to describe this process. We showed that the new scheme improved the model performance for plant productivity, soil organic carbon, and soil phosphorus content at five beech forest sites in Germany. We claim that this new model could be used as a better tool to study ecosystems under future climate change, particularly phosphorus-limited systems.
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Short summary
Phosphorus (P) is essential for life. We studied microbial processes driving the P cycle in soils developed on the same rock but with different ages (0–100 years) in a cold desert. Compared to previous studies under cold climate, we found much slower weathering of P-containing minerals of soil development, likely due to aridity. However, microbes dominate short-term dynamics and progressively redistribute P from the rock into more available forms, making it available for plants at later stages.
Phosphorus (P) is essential for life. We studied microbial processes driving the P cycle in...
