Articles | Volume 2, issue 1
https://doi.org/10.5194/soil-2-83-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/soil-2-83-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Original research article
| 
29 Feb 2016
Original research article |
| 29 Feb 2016
Soil properties and not inputs control carbon : nitrogen : phosphorus ratios in cropped soils in the long term
Emmanuel Frossard
CORRESPONDING AUTHOR
Group of Plant Nutrition, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
Nina Buchmann
Group of Grassland Sciences, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
Else K. Bünemann
Group of Plant Nutrition, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
Delwende I. Kiba
Group of Plant Nutrition, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
INERA, Ouagadougou, Burkina Faso
François Lompo
INERA, Ouagadougou, Burkina Faso
Astrid Oberson
Group of Plant Nutrition, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
Federica Tamburini
Group of Plant Nutrition, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
Ouakoltio Y. A. Traoré
Group of Plant Nutrition, Institute of Agricultural
Sciences, ETH Zurich, Switzerland
INERA, Ouagadougou, Burkina Faso
Related authors
Tegawende Léa Jeanne Ilboudo, Lucien NGuessan Diby, Delwendé Innocent Kiba, Tor Gunnar Vågen, Leigh Ann Winowiecki, Hassan Bismarck Nacro, Johan Six, and Emmanuel Frossard
EGUsphere, https://doi.org/10.5194/egusphere-2022-209, https://doi.org/10.5194/egusphere-2022-209, 2022
Preprint withdrawn
Short summary
Short summary
Our results showed that at landscape level SOC stock variability was mainly explained by clay content. We found significant linear positive relationships between VC and SOC stocks for the land uses annual croplands, perennial croplands, grasslands and bushlands without soil depth restrictions until 110 cm. We concluded that in the forest-savanna transition zone, soil properties and topography determine land use, which in turn affects the stocks of SOC and TN and to some extent the VC stocks.
Jasmin Fetzer, Emmanuel Frossard, Klaus Kaiser, and Frank Hagedorn
Biogeosciences, 19, 1527–1546, https://doi.org/10.5194/bg-19-1527-2022, https://doi.org/10.5194/bg-19-1527-2022, 2022
Short summary
Short summary
As leaching is a major pathway of nitrogen and phosphorus loss in forest soils, we investigated several potential drivers in two contrasting beech forests. The composition of leachates, obtained by zero-tension lysimeters, varied by season, and climatic extremes influenced the magnitude of leaching. Effects of nitrogen and phosphorus fertilization varied with soil nutrient status and sorption properties, and leaching from the low-nutrient soil was more sensitive to environmental factors.
Philipp Baumann, Juhwan Lee, Emmanuel Frossard, Laurie Paule Schönholzer, Lucien Diby, Valérie Kouamé Hgaza, Delwende Innocent Kiba, Andrew Sila, Keith Sheperd, and Johan Six
SOIL, 7, 717–731, https://doi.org/10.5194/soil-7-717-2021, https://doi.org/10.5194/soil-7-717-2021, 2021
Short summary
Short summary
This work delivers openly accessible and validated calibrations for diagnosing 26 soil properties based on mid-infrared spectroscopy. These were developed for four regions in Burkina Faso and Côte d'Ivoire, including 80 fields of smallholder farmers. The models can help to site-specifically and cost-efficiently monitor soil quality and fertility constraints to ameliorate soils and yields of yam or other staple crops in the four regions between the humid forest and the northern Guinean savanna.
Jolanda E. Reusser, René Verel, Daniel Zindel, Emmanuel Frossard, and Timothy I. McLaren
Biogeosciences, 17, 5079–5095, https://doi.org/10.5194/bg-17-5079-2020, https://doi.org/10.5194/bg-17-5079-2020, 2020
Short summary
Short summary
Inositol phosphates (IPs) are a major pool of organic P in soil. However, information on their diversity and abundance in soil is limited. We isolated IPs from soil and characterised them using solution nuclear magnetic resonance (NMR) spectroscopy. For the first time, we provide direct spectroscopic evidence for the existence of a multitude of lower-order IPs in soil extracts previously not detected with NMR. Our findings will help provide new insight into the cycling of IPs in ecosystems.
Julian Helfenstein, Chiara Pistocchi, Astrid Oberson, Federica Tamburini, Daniel S. Goll, and Emmanuel Frossard
Biogeosciences, 17, 441–454, https://doi.org/10.5194/bg-17-441-2020, https://doi.org/10.5194/bg-17-441-2020, 2020
Short summary
Short summary
In this article we provide estimates of mean residence times of phosphorus in inorganic soil phosphorus pools. These values improve our understanding of the dynamics of phosphorus cycling and can be used to improve global land surface models.
Julian Helfenstein, Jannes Jegminat, Timothy I. McLaren, and Emmanuel Frossard
Biogeosciences, 15, 105–114, https://doi.org/10.5194/bg-15-105-2018, https://doi.org/10.5194/bg-15-105-2018, 2018
Short summary
Short summary
Soil solution phosphorus (P) turnover is essential for describing the bioavailability of this important nutrient. Here, we provide a derivation of calculating soil solution P turnover using parameters obtained from isotope exchange kinetic experiments. We then calculated and analyzed soil solution P turnover for 217 soils and for 18 long-term P fertilizer field experiments worldwide. Our study thus provides important insights on P dynamics in soils.
C. von Sperber, F. Tamburini, B. Brunner, S. M. Bernasconi, and E. Frossard
Biogeosciences, 12, 4175–4184, https://doi.org/10.5194/bg-12-4175-2015, https://doi.org/10.5194/bg-12-4175-2015, 2015
Tegawende Léa Jeanne Ilboudo, Lucien NGuessan Diby, Delwendé Innocent Kiba, Tor Gunnar Vågen, Leigh Ann Winowiecki, Hassan Bismarck Nacro, Johan Six, and Emmanuel Frossard
EGUsphere, https://doi.org/10.5194/egusphere-2022-209, https://doi.org/10.5194/egusphere-2022-209, 2022
Preprint withdrawn
Short summary
Short summary
Our results showed that at landscape level SOC stock variability was mainly explained by clay content. We found significant linear positive relationships between VC and SOC stocks for the land uses annual croplands, perennial croplands, grasslands and bushlands without soil depth restrictions until 110 cm. We concluded that in the forest-savanna transition zone, soil properties and topography determine land use, which in turn affects the stocks of SOC and TN and to some extent the VC stocks.
Jasmin Fetzer, Emmanuel Frossard, Klaus Kaiser, and Frank Hagedorn
Biogeosciences, 19, 1527–1546, https://doi.org/10.5194/bg-19-1527-2022, https://doi.org/10.5194/bg-19-1527-2022, 2022
Short summary
Short summary
As leaching is a major pathway of nitrogen and phosphorus loss in forest soils, we investigated several potential drivers in two contrasting beech forests. The composition of leachates, obtained by zero-tension lysimeters, varied by season, and climatic extremes influenced the magnitude of leaching. Effects of nitrogen and phosphorus fertilization varied with soil nutrient status and sorption properties, and leaching from the low-nutrient soil was more sensitive to environmental factors.
Zuzana Frkova, Chiara Pistocchi, Yuliya Vystavna, Katerina Capkova, Jiri Dolezal, and Federica Tamburini
SOIL, 8, 1–15, https://doi.org/10.5194/soil-8-1-2022, https://doi.org/10.5194/soil-8-1-2022, 2022
Short summary
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.
Philipp Baumann, Juhwan Lee, Emmanuel Frossard, Laurie Paule Schönholzer, Lucien Diby, Valérie Kouamé Hgaza, Delwende Innocent Kiba, Andrew Sila, Keith Sheperd, and Johan Six
SOIL, 7, 717–731, https://doi.org/10.5194/soil-7-717-2021, https://doi.org/10.5194/soil-7-717-2021, 2021
Short summary
Short summary
This work delivers openly accessible and validated calibrations for diagnosing 26 soil properties based on mid-infrared spectroscopy. These were developed for four regions in Burkina Faso and Côte d'Ivoire, including 80 fields of smallholder farmers. The models can help to site-specifically and cost-efficiently monitor soil quality and fertility constraints to ameliorate soils and yields of yam or other staple crops in the four regions between the humid forest and the northern Guinean savanna.
Jolanda E. Reusser, René Verel, Daniel Zindel, Emmanuel Frossard, and Timothy I. McLaren
Biogeosciences, 17, 5079–5095, https://doi.org/10.5194/bg-17-5079-2020, https://doi.org/10.5194/bg-17-5079-2020, 2020
Short summary
Short summary
Inositol phosphates (IPs) are a major pool of organic P in soil. However, information on their diversity and abundance in soil is limited. We isolated IPs from soil and characterised them using solution nuclear magnetic resonance (NMR) spectroscopy. For the first time, we provide direct spectroscopic evidence for the existence of a multitude of lower-order IPs in soil extracts previously not detected with NMR. Our findings will help provide new insight into the cycling of IPs in ecosystems.
Julian Helfenstein, Chiara Pistocchi, Astrid Oberson, Federica Tamburini, Daniel S. Goll, and Emmanuel Frossard
Biogeosciences, 17, 441–454, https://doi.org/10.5194/bg-17-441-2020, https://doi.org/10.5194/bg-17-441-2020, 2020
Short summary
Short summary
In this article we provide estimates of mean residence times of phosphorus in inorganic soil phosphorus pools. These values improve our understanding of the dynamics of phosphorus cycling and can be used to improve global land surface models.
Catharina Simone Nisbeth, Federica Tamburini, Jacob Kidmose, Søren Jessen, and David William O'Connell
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-469, https://doi.org/10.5194/hess-2019-469, 2019
Preprint withdrawn
Short summary
Short summary
Phosphorus contamination frequently causes eutrophication of freshwater lakes. However it is often difficult to establish the origin of the contaminating phosphorus. This study aims to contribute to the development and improvement of a method for tracing phosphorus in the freshwater environment, by using the oxygen-18 isotope of orthophosphate (δ18Op). The use of a coherent and common method across research groups may enable phosphorus tracing and better management of freshwater ecosystems.
Julian Helfenstein, Jannes Jegminat, Timothy I. McLaren, and Emmanuel Frossard
Biogeosciences, 15, 105–114, https://doi.org/10.5194/bg-15-105-2018, https://doi.org/10.5194/bg-15-105-2018, 2018
Short summary
Short summary
Soil solution phosphorus (P) turnover is essential for describing the bioavailability of this important nutrient. Here, we provide a derivation of calculating soil solution P turnover using parameters obtained from isotope exchange kinetic experiments. We then calculated and analyzed soil solution P turnover for 217 soils and for 18 long-term P fertilizer field experiments worldwide. Our study thus provides important insights on P dynamics in soils.
J. Stieger, I. Bamberger, N. Buchmann, and W. Eugster
Atmos. Chem. Phys., 15, 14055–14069, https://doi.org/10.5194/acp-15-14055-2015, https://doi.org/10.5194/acp-15-14055-2015, 2015
Short summary
Short summary
At night, concentrations of methane and other trace gases in the near-surface atmosphere increase due to limited turbulent mixing and confluence of cold air from valley slopes towards the valley bottom. Here we used a tethered balloon sounding system to obtain time-height profiles of methane concentrations from which we compute methane emissions. These flux estimates serve as the first experimental validation of Swiss agricultural methane emissions at the farm scale.
C. von Sperber, F. Tamburini, B. Brunner, S. M. Bernasconi, and E. Frossard
Biogeosciences, 12, 4175–4184, https://doi.org/10.5194/bg-12-4175-2015, https://doi.org/10.5194/bg-12-4175-2015, 2015
B. P. Guillod, B. Orlowsky, D. Miralles, A. J. Teuling, P. D. Blanken, N. Buchmann, P. Ciais, M. Ek, K. L. Findell, P. Gentine, B. R. Lintner, R. L. Scott, B. Van den Hurk, and S. I. Seneviratne
Atmos. Chem. Phys., 14, 8343–8367, https://doi.org/10.5194/acp-14-8343-2014, https://doi.org/10.5194/acp-14-8343-2014, 2014
S. Vicca, M. Bahn, M. Estiarte, E. E. van Loon, R. Vargas, G. Alberti, P. Ambus, M. A. Arain, C. Beier, L. P. Bentley, W. Borken, N. Buchmann, S. L. Collins, G. de Dato, J. S. Dukes, C. Escolar, P. Fay, G. Guidolotti, P. J. Hanson, A. Kahmen, G. Kröel-Dulay, T. Ladreiter-Knauss, K. S. Larsen, E. Lellei-Kovacs, E. Lebrija-Trejos, F. T. Maestre, S. Marhan, M. Marshall, P. Meir, Y. Miao, J. Muhr, P. A. Niklaus, R. Ogaya, J. Peñuelas, C. Poll, L. E. Rustad, K. Savage, A. Schindlbacher, I. K. Schmidt, A. R. Smith, E. D. Sotta, V. Suseela, A. Tietema, N. van Gestel, O. van Straaten, S. Wan, U. Weber, and I. A. Janssens
Biogeosciences, 11, 2991–3013, https://doi.org/10.5194/bg-11-2991-2014, https://doi.org/10.5194/bg-11-2991-2014, 2014
R. V. Hiller, D. Bretscher, T. DelSontro, T. Diem, W. Eugster, R. Henneberger, S. Hobi, E. Hodson, D. Imer, M. Kreuzer, T. Künzle, L. Merbold, P. A. Niklaus, B. Rihm, A. Schellenberger, M. H. Schroth, C. J. Schubert, H. Siegrist, J. Stieger, N. Buchmann, and D. Brunner
Biogeosciences, 11, 1941–1959, https://doi.org/10.5194/bg-11-1941-2014, https://doi.org/10.5194/bg-11-1941-2014, 2014
S. Zielis, S. Etzold, R. Zweifel, W. Eugster, M. Haeni, and N. Buchmann
Biogeosciences, 11, 1627–1635, https://doi.org/10.5194/bg-11-1627-2014, https://doi.org/10.5194/bg-11-1627-2014, 2014
S. Burri, P. Sturm, U. E. Prechsl, A. Knohl, and N. Buchmann
Biogeosciences, 11, 961–975, https://doi.org/10.5194/bg-11-961-2014, https://doi.org/10.5194/bg-11-961-2014, 2014
D. Imer, L. Merbold, W. Eugster, and N. Buchmann
Biogeosciences, 10, 5931–5945, https://doi.org/10.5194/bg-10-5931-2013, https://doi.org/10.5194/bg-10-5931-2013, 2013
Related subject area
Soils and biogeochemical cycling
Cover crops improve soil structure and change organic carbon distribution in macroaggregate fractions
Soil carbon, nitrogen, and phosphorus storage in juniper–oak savanna: role of vegetation and geology
Organic matters, but inorganic matters too: column examination of elevated mercury sorption on low organic matter aquifer material using concentrations and stable isotope ratios
Contrasting potential for biological N2 fixation at three polluted central European Sphagnum peat bogs: combining the 15N2-tracer and natural-abundance isotope approaches
Soil organic carbon stocks did not change after 130 years of afforestation on a former Swiss Alpine pasture
The six rights of how and when to test for soil C saturation
Shifts in controls and abundance of particulate and mineral-associated organic matter fractions among subfield yield stability zones
Land inclination controls CO2 and N2O fluxes, but not CH4 uptake, in a temperate upland forest soil
Tropical Andosol organic carbon quality and degradability in relation to soil geochemistry as affected by land use
Elemental stoichiometry and Rock-Eval® thermal stability of organic matter in French topsoils
Oil-palm management alters the spatial distribution of amorphous silica and mobile silicon in topsoils
Semantics about soil organic carbon storage: DATA4C+, a comprehensive thesaurus and classification of management practices in agriculture and forestry
Forest liming in the face of climate change: the implications of restorative liming for soil organic carbon in mature German forests
Biotic factors dominantly determine soil inorganic carbon stock across Tibetan alpine grasslands
Effects of returning corn straw and fermented corn straw to fields on the soil organic carbon pools and humus composition
Soil nutrient contents and stoichiometry within aggregate size classes varied with tea plantation age and soil depth in southern Guangxi in China
Land use impact on carbon mineralization in well aerated soils is mainly explained by variations of particulate organic matter rather than of soil structure
Inclusion of biochar in a C dynamics model based on observations from an 8-year field experiment
Synergy between compost and cover crops in a Mediterranean row crop system leads to increased subsoil carbon storage
Phosphorus dynamics during early soil development in a cold desert: insights from oxygen isotopes in phosphate
Transformation of n-alkanes from plant to soil: a review
Heterotrophic soil respiration and carbon cycling in geochemically distinct African tropical forest soils
Soil organic carbon mobility in equatorial podzols: soil column experiments
Microbial activity responses to water stress in agricultural soils from simple and complex crop rotations
The role of geochemistry in organic carbon stabilization against microbial decomposition in tropical rainforest soils
Geogenic organic carbon in terrestrial sediments and its contribution to total soil carbon
Aluminous clay and pedogenic Fe oxides modulate aggregation and related carbon contents in soils of the humid tropics
Continental-scale controls on soil organic carbon across sub-Saharan Africa
Modelling of long-term Zn, Cu, Cd and Pb dynamics from soils fertilised with organic amendments
Stable isotope signatures of soil nitrogen on an environmental–geomorphic gradient within the Congo Basin
Iron and aluminum association with microbially processed organic matter via meso-density aggregate formation across soils: organo-metallic glue hypothesis
Land-use perturbations in ley grassland decouple the degradation of ancient soil organic matter from the storage of newly derived carbon inputs
Switch of fungal to bacterial degradation in natural, drained and rewetted oligotrophic peatlands reflected in δ15N and fatty acid composition
Catchment export of base cations: improved mineral dissolution kinetics influence the role of water transit time
Boreal-forest soil chemistry drives soil organic carbon bioreactivity along a 314-year fire chronosequence
Ramped thermal analysis for isolating biologically meaningful soil organic matter fractions with distinct residence times
Variations in soil chemical and physical properties explain basin-wide Amazon forest soil carbon concentrations
Lithology- and climate-controlled soil aggregate-size distribution and organic carbon stability in the Peruvian Andes
Evaluating the effects of soil erosion and productivity decline on soil carbon dynamics using a model-based approach
Base cations in the soil bank: non-exchangeable pools may sustain centuries of net loss to forestry and leaching
Short-range-order minerals as powerful factors explaining deep soil organic carbon stock distribution: the case of a coffee agroforestry plantation on Andosols in Costa Rica
A new look at an old concept: using 15N2O isotopomers to understand the relationship between soil moisture and N2O production pathways
Assessing the impact of acid rain and forest harvest intensity with the HD-MINTEQ model – soil chemistry of three Swedish conifer sites from 1880 to 2080
Dynamic modelling of weathering rates – the benefit over steady-state modelling
Aluminium and base cation chemistry in dynamic acidification models – need for a reappraisal?
Challenges of soil carbon sequestration in the NENA region
Continental soil drivers of ammonium and nitrate in Australia
Comment on “Soil organic stocks are systematically overestimated by misuse of the parameters bulk density and rock fragment content” by Poeplau et al. (2017)
Hot regions of labile and stable soil organic carbon in Germany – Spatial variability and driving factors
Potential short-term losses of N2O and N2 from high concentrations of biogas digestate in arable soils
Norman Gentsch, Florin Laura Riechers, Jens Boy, Dörte Schweneker, Ulf Feuerstein, Diana Heuermann, and Georg Guggenberger
SOIL, 10, 139–150, https://doi.org/10.5194/soil-10-139-2024, https://doi.org/10.5194/soil-10-139-2024, 2024
Short summary
Short summary
Cover crops have substantial impacts on soil properties, but so far it is not clear how long a legacy effect of cover cropping will remain in the soil. We found that cover crops attenuate negative effects on soil structure that come from soil cultivation. The combination of plants with different litter qualities and rhizodeposits in biodiverse cover crop mixtures can improve the positive effects of cover cropping on soil structure amelioration.
Che-Jen Hsiao, Pedro A. M. Leite, Ayumi Hyodo, and Thomas W. Boutton
SOIL, 10, 93–108, https://doi.org/10.5194/soil-10-93-2024, https://doi.org/10.5194/soil-10-93-2024, 2024
Short summary
Short summary
Tree cover has increased in grasslands worldwide, with juniper and oak trees expanding in the southern Great Plains, USA. Here, we examine how these changes interact with geology to affect soil C, N, and P storage. Soil concentrations of these elements were significantly higher under trees than grasslands but increased more under trees growing on Edwards soils. Our results suggest that geology and vegetation change should be considered when predicting soil storage in dryland ecosystems globally.
David S. McLagan, Carina Esser, Lorenz Schwab, Jan G. Wiederhold, Jan-Helge Richard, and Harald Biester
SOIL, 10, 77–92, https://doi.org/10.5194/soil-10-77-2024, https://doi.org/10.5194/soil-10-77-2024, 2024
Short summary
Short summary
Sorption of mercury in soils, aquifer materials, and sediments is primarily linked to organic matter. Using column experiments, mercury concentration, speciation, and stable isotope analyses, we show that large quantities of mercury in soil water and groundwater can be sorbed to inorganic minerals; sorption to the solid phase favours lighter isotopes. Data provide important insights on the transport and fate of mercury in soil–groundwater systems and particularly in low-organic-matter systems.
Marketa Stepanova, Martin Novak, Bohuslava Cejkova, Ivana Jackova, Frantisek Buzek, Frantisek Veselovsky, Jan Curik, Eva Prechova, Arnost Komarek, and Leona Bohdalkova
SOIL, 9, 623–640, https://doi.org/10.5194/soil-9-623-2023, https://doi.org/10.5194/soil-9-623-2023, 2023
Short summary
Short summary
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.
Tatjana C. Speckert, Jeannine Suremann, Konstantin Gavazov, Maria J. Santos, Frank Hagedorn, and Guido L. B. Wiesenberg
SOIL, 9, 609–621, https://doi.org/10.5194/soil-9-609-2023, https://doi.org/10.5194/soil-9-609-2023, 2023
Short summary
Short summary
Soil organic carbon (SOC) is key player in the global carbon cycle. Afforestation on pastures potentially alters organic matter input and SOC sequestration. We investigated the effects of a Picea abies L. afforestation sequence (0 to 130 years) on a former subalpine pasture on SOC stocks and dynamics. We found no difference in the SOC stock after 130 years of afforestation and thus no additional SOC sequestration. SOC composition was altered due to a modified SOC input following afforestation.
Johan Six, Sebastian Doetterl, Moritz Laub, Claude Raoul Müller, and Marijn Van de Broek
EGUsphere, https://doi.org/10.5194/egusphere-2023-2221, https://doi.org/10.5194/egusphere-2023-2221, 2023
Short summary
Short summary
The sequestration of carbon (C) in soils is seen as a potential mitigation strategy. However, more than 2 decades ago the concept of soil C saturation, which puts a limit to how much C can be stabilized in a soil, emerged. Recently, this concept has been challenged in some studies. Here, we argue that if one pays attention to six fundamental principles when testing for soil C saturation, that the concept is robust and there is effectively a maximum to how much C soil minerals can stabilize.
Sam J. Leuthold, Jocelyn M. Lavallee, Bruno Basso, William F. Brinton, and M. Francesca Cotrufo
EGUsphere, https://doi.org/10.5194/egusphere-2023-2327, https://doi.org/10.5194/egusphere-2023-2327, 2023
Short summary
Short summary
We examined physical soil organic matter fractions to understand their relationship to temporal variability in crop yield at the field scale. We found that interactions between crop productivity, topography, and climate led to variability in soil organic matter stocks among different yield stability zones. Our results imply linkages between soil organic matter and yield stability may be scale-dependent, and that particulate organic matter may be an indicator of unstable areas within croplands.
Lauren M. Gillespie, Nathalie Y. Triches, Diego Abalos, Peter Finke, Sophie Zechmeister-Boltenstern, Stephan Glatzel, and Eugenio Díaz-Pinés
SOIL, 9, 517–531, https://doi.org/10.5194/soil-9-517-2023, https://doi.org/10.5194/soil-9-517-2023, 2023
Short summary
Short summary
Forest soil is potentially an important source or sink of greenhouse gases (CO2, N2O, and CH4), but this is affected by soil conditions. We studied how land inclination and soil/litter properties influence the flux of these gases. CO2 and N2O were more affected by inclination than CH4; all were affected by soil/litter properties. This study underlines the importance of inclination and soil/litter properties in predicting greenhouse gas fluxes from forest soil and potential source–sink balance.
Sastrika Anindita, Peter Finke, and Steven Sleutel
SOIL, 9, 443–459, https://doi.org/10.5194/soil-9-443-2023, https://doi.org/10.5194/soil-9-443-2023, 2023
Short summary
Short summary
This study investigated how land use, through its impact on soil geochemistry, might indirectly control soil organic carbon (SOC) content in tropical volcanic soils in Indonesia. We analyzed SOC fractions, substrate-specific mineralization, and net priming of SOC. Our results indicated that the enhanced formation of aluminum (hydr)oxides promoted aggregation and physical occlusion of OC, which is consistent with the lesser degradability of SOC in agricultural soils.
Amicie A. Delahaie, Pierre Barré, François Baudin, Dominique Arrouays, Antonio Bispo, Line Boulonne, Claire Chenu, Claudy Jolivet, Manuel P. Martin, Céline Ratié, Nicolas P. A. Saby, Florence Savignac, and Lauric Cécillon
SOIL, 9, 209–229, https://doi.org/10.5194/soil-9-209-2023, https://doi.org/10.5194/soil-9-209-2023, 2023
Short summary
Short summary
We characterized organic matter in French soils by analysing samples from the French RMQS network using Rock-Eval thermal analysis. We found that thermal analysis is appropriate to characterize large set of samples (ca. 2000) and provides interpretation references for Rock-Eval parameter values. This shows that organic matter in managed soils is on average more oxidized and more thermally stable and that some Rock-Eval parameters are good proxies for organic matter biogeochemical stability.
Britta Greenshields, Barbara von der Lühe, Harold J. Hughes, Christian Stiegler, Suria Tarigan, Aiyen Tjoa, and Daniela Sauer
SOIL, 9, 169–188, https://doi.org/10.5194/soil-9-169-2023, https://doi.org/10.5194/soil-9-169-2023, 2023
Short summary
Short summary
Silicon (Si) research could provide complementary measures in sustainably cultivating oil-palm monocultures. Our study shows that current oil-palm management practices and topsoil erosion on oil-palm plantations in Indonesia have caused a spatial distribution of essential Si pools in soil. A lack of well-balanced Si levels in topsoil could negatively affect crop yield and soil fertility for future replanting at the same plantation site. Potential measures are suggested to maintain Si cycling.
Kenji Fujisaki, Tiphaine Chevallier, Antonio Bispo, Jean-Baptiste Laurent, François Thevenin, Lydie Chapuis-Lardy, Rémi Cardinael, Christine Le Bas, Vincent Freycon, Fabrice Bénédet, Vincent Blanfort, Michel Brossard, Marie Tella, and Julien Demenois
SOIL, 9, 89–100, https://doi.org/10.5194/soil-9-89-2023, https://doi.org/10.5194/soil-9-89-2023, 2023
Short summary
Short summary
This paper presents a first comprehensive thesaurus for management practices driving soil organic carbon (SOC) storage. So far, a comprehensive thesaurus of management practices in agriculture and forestry has been lacking. It will help to merge datasets, a promising way to evaluate the impacts of management practices in agriculture and forestry on SOC. Identifying the drivers of SOC stock changes is of utmost importance to contribute to global challenges (climate change, food security).
Oliver van Straaten, Larissa Kulp, Guntars O. Martinson, Dan Paul Zederer, and Ulrike Talkner
SOIL, 9, 39–54, https://doi.org/10.5194/soil-9-39-2023, https://doi.org/10.5194/soil-9-39-2023, 2023
Short summary
Short summary
Across northern Europe, millions of hectares of forest have been limed to counteract soil acidification and restore forest ecosystems. In this study, we investigated how restorative liming affects the forest soil organic carbon (SOC) stocks and correspondingly ecosystem greenhouse gas fluxes. We found that the magnitude and direction of SOC stock changes hinge on the inherent site characteristics, namely, forest type, soil texture, initial soil pH, and initial soil SOC stocks (before liming).
Junxiao Pan, Jinsong Wang, Dashuan Tian, Ruiyang Zhang, Yang Li, Lei Song, Jiaming Yang, Chunxue Wei, and Shuli Niu
SOIL, 8, 687–698, https://doi.org/10.5194/soil-8-687-2022, https://doi.org/10.5194/soil-8-687-2022, 2022
Short summary
Short summary
We found that climatic, edaphic, plant and microbial variables jointly affect soil inorganic carbon (SIC) stock in Tibetan grasslands, and biotic factors have a larger contribution than abiotic factors to the variation in SIC stock. The effects of microbial and plant variables on SIC stock weakened with soil depth, while the effects of edaphic variables strengthened. The contrasting responses and drivers of SIC stock highlight differential mechanisms underlying SIC preservation with soil depth.
Yifeng Zhang, Sen Dou, Batande Sinovuyo Ndzelu, Rui Ma, Dandan Zhang, Xiaowei Zhang, Shufen Ye, and Hongrui Wang
SOIL, 8, 605–619, https://doi.org/10.5194/soil-8-605-2022, https://doi.org/10.5194/soil-8-605-2022, 2022
Short summary
Short summary
How to effectively convert corn straw into humic substances and return them to the soil in a relatively stable form is a concerning topic. Through a 360 d field experiment under equal carbon (C) mass, we found that return of the fermented corn straw treated with Trichoderma reesei to the field is more valuable and conducive to increasing easily oxidizable organic C, humus C content, and carbon pool management index than the direct application of corn straw.
Ling Mao, Shaoming Ye, and Shengqiang Wang
SOIL, 8, 487–505, https://doi.org/10.5194/soil-8-487-2022, https://doi.org/10.5194/soil-8-487-2022, 2022
Short summary
Short summary
Soil ecological stoichiometry offers a tool to explore the distribution, cycling, limitation, and balance of chemical elements. This study improved the understanding of soil organic carbon and nutrient dynamics in tea plantation ecosystems and also provided supplementary information for soil ecological stoichiometry in global terrestrial ecosystems.
Steffen Schlüter, Tim Roussety, Lena Rohe, Vusal Guliyev, Evgenia Blagodatskaya, and Thomas Reitz
SOIL, 8, 253–267, https://doi.org/10.5194/soil-8-253-2022, https://doi.org/10.5194/soil-8-253-2022, 2022
Short summary
Short summary
We combined microstructure analysis via X-ray CT with carbon mineralization analysis via respirometry of intact soil cores from different land uses. We found that the amount of particulate organic matter (POM) exerted a dominant control on carbon mineralization in well-aerated topsoils, whereas soil moisture and macroporosity did not play role. This is because carbon mineralization mainly occurs in microbial hotspots around degrading POM, where it is decoupled from conditions of the bulk soil.
Roberta Pulcher, Enrico Balugani, Maurizio Ventura, Nicolas Greggio, and Diego Marazza
SOIL, 8, 199–211, https://doi.org/10.5194/soil-8-199-2022, https://doi.org/10.5194/soil-8-199-2022, 2022
Short summary
Short summary
Biochar, a solid product from the thermal conversion of biomass, can be used as a climate change mitigation strategy, since it can sequester carbon from the atmosphere and store it in the soil. The aim of this study is to assess the potential of biochar as a mitigation strategy in the long term, by modelling the results obtained from an 8-year field experiment. As far as we know, this is the first time that a model for biochar degradation has been validated with long-term field data.
Daniel Rath, Nathaniel Bogie, Leonardo Deiss, Sanjai J. Parikh, Daoyuan Wang, Samantha Ying, Nicole Tautges, Asmeret Asefaw Berhe, Teamrat A. Ghezzehei, and Kate M. Scow
SOIL, 8, 59–83, https://doi.org/10.5194/soil-8-59-2022, https://doi.org/10.5194/soil-8-59-2022, 2022
Short summary
Short summary
Storing C in subsoils can help mitigate climate change, but this requires a better understanding of subsoil C dynamics. We investigated changes in subsoil C storage under a combination of compost, cover crops (WCC), and mineral fertilizer and found that systems with compost + WCC had ~19 Mg/ha more C after 25 years. This increase was attributed to increased transport of soluble C and nutrients via WCC root pores and demonstrates the potential for subsoil C storage in tilled agricultural systems.
Zuzana Frkova, Chiara Pistocchi, Yuliya Vystavna, Katerina Capkova, Jiri Dolezal, and Federica Tamburini
SOIL, 8, 1–15, https://doi.org/10.5194/soil-8-1-2022, https://doi.org/10.5194/soil-8-1-2022, 2022
Short summary
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.
Carrie L. Thomas, Boris Jansen, E. Emiel van Loon, and Guido L. B. Wiesenberg
SOIL, 7, 785–809, https://doi.org/10.5194/soil-7-785-2021, https://doi.org/10.5194/soil-7-785-2021, 2021
Short summary
Short summary
Plant organs, such as leaves, contain a variety of chemicals that are eventually deposited into soil and can be useful for studying organic carbon cycling. We performed a systematic review of available data of one type of plant-derived chemical, n-alkanes, to determine patterns of degradation or preservation from the source plant to the soil. We found that while there was degradation in the amount of n-alkanes from plant to soil, some aspects of the chemical signature were preserved.
Benjamin Bukombe, Peter Fiener, Alison M. Hoyt, Laurent K. Kidinda, and Sebastian Doetterl
SOIL, 7, 639–659, https://doi.org/10.5194/soil-7-639-2021, https://doi.org/10.5194/soil-7-639-2021, 2021
Short summary
Short summary
Through a laboratory incubation experiment, we investigated the spatial patterns of specific maximum heterotrophic respiration in tropical African mountain forest soils developed from contrasting parent material along slope gradients. We found distinct differences in soil respiration between soil depths and geochemical regions related to soil fertility and the chemistry of the soil solution. The topographic origin of our samples was not a major determinant of the observed rates of respiration.
Patricia Merdy, Yves Lucas, Bruno Coulomb, Adolpho J. Melfi, and Célia R. Montes
SOIL, 7, 585–594, https://doi.org/10.5194/soil-7-585-2021, https://doi.org/10.5194/soil-7-585-2021, 2021
Short summary
Short summary
Transfer of organic C from topsoil to deeper horizons and the water table is little documented, especially in equatorial environments, despite high primary productivity in the evergreen forest. Using column experiments with podzol soil and a percolating solution sampled in an Amazonian podzol area, we show how the C-rich Bh horizon plays a role in natural organic matter transfer and Si, Fe and Al mobility after a kaolinitic layer transition, thus giving insight to the genesis of tropical podzol.
Jörg Schnecker, D. Boone Meeden, Francisco Calderon, Michel Cavigelli, R. Michael Lehman, Lisa K. Tiemann, and A. Stuart Grandy
SOIL, 7, 547–561, https://doi.org/10.5194/soil-7-547-2021, https://doi.org/10.5194/soil-7-547-2021, 2021
Short summary
Short summary
Drought and flooding challenge agricultural systems and their management globally. Here we investigated the response of soils from long-term agricultural field sites with simple and diverse crop rotations to either drought or flooding. We found that irrespective of crop rotation complexity, soil and microbial properties were more resistant to flooding than to drought and highly resilient to drought and flooding during single or repeated stress pulses.
Mario Reichenbach, Peter Fiener, Gina Garland, Marco Griepentrog, Johan Six, and Sebastian Doetterl
SOIL, 7, 453–475, https://doi.org/10.5194/soil-7-453-2021, https://doi.org/10.5194/soil-7-453-2021, 2021
Short summary
Short summary
In deeply weathered tropical rainforest soils of Africa, we found that patterns of soil organic carbon stocks differ between soils developed from geochemically contrasting parent material due to differences in the abundance of organo-mineral complexes, the presence/absence of chemical stabilization mechanisms of carbon with minerals and the presence of fossil organic carbon from sedimentary rocks. Physical stabilization mechanisms by aggregation provide additional protection of soil carbon.
Fabian Kalks, Gabriel Noren, Carsten W. Mueller, Mirjam Helfrich, Janet Rethemeyer, and Axel Don
SOIL, 7, 347–362, https://doi.org/10.5194/soil-7-347-2021, https://doi.org/10.5194/soil-7-347-2021, 2021
Short summary
Short summary
Sedimentary rocks contain organic carbon that may end up as soil carbon. However, this source of soil carbon is overlooked and has not been quantified sufficiently. We analysed 10 m long sediment cores with three different sedimentary rocks. All sediments contain considerable amounts of geogenic carbon contributing 3 %–12 % to the total soil carbon below 30 cm depth. The low 14C content of geogenic carbon can result in underestimations of soil carbon turnover derived from 14C data.
Maximilian Kirsten, Robert Mikutta, Didas N. Kimaro, Karl-Heinz Feger, and Karsten Kalbitz
SOIL, 7, 363–375, https://doi.org/10.5194/soil-7-363-2021, https://doi.org/10.5194/soil-7-363-2021, 2021
Short summary
Short summary
Mineralogical combinations of aluminous clay and pedogenic Fe oxides revealed significant effects on soil structure and related organic carbon (OC) storage.
The mineralogical combination resulting in the largest aggregate stability does not better preserve OC during conversion of forests into croplands.
Structural changes in the direction of smaller mean weight diameters do not cancel out the stabilizing effect of soil minerals.
Sophie F. von Fromm, Alison M. Hoyt, Markus Lange, Gifty E. Acquah, Ermias Aynekulu, Asmeret Asefaw Berhe, Stephan M. Haefele, Steve P. McGrath, Keith D. Shepherd, Andrew M. Sila, Johan Six, Erick K. Towett, Susan E. Trumbore, Tor-G. Vågen, Elvis Weullow, Leigh A. Winowiecki, and Sebastian Doetterl
SOIL, 7, 305–332, https://doi.org/10.5194/soil-7-305-2021, https://doi.org/10.5194/soil-7-305-2021, 2021
Short summary
Short summary
We investigated various soil and climate properties that influence soil organic carbon (SOC) concentrations in sub-Saharan Africa. Our findings indicate that climate and geochemistry are equally important for explaining SOC variations. The key SOC-controlling factors are broadly similar to those for temperate regions, despite differences in soil development history between the two regions.
Claudia Cagnarini, Stephen Lofts, Luigi Paolo D'Acqui, Jochen Mayer, Roman Grüter, Susan Tandy, Rainer Schulin, Benjamin Costerousse, Simone Orlandini, and Giancarlo Renella
SOIL, 7, 107–123, https://doi.org/10.5194/soil-7-107-2021, https://doi.org/10.5194/soil-7-107-2021, 2021
Short summary
Short summary
Application of organic amendments, although considered a sustainable form of soil fertilisation, may cause an accumulation of trace elements (TEs) in the topsoil. In this research, we analysed the concentration of zinc, copper, lead and cadmium in a > 60-year experiment in Switzerland and showed that the dynamic model IDMM adequately predicted the historical TE concentrations in plots amended with farmyard manure, sewage sludge and compost and produced reasonable concentration trends up to 2100.
Simon Baumgartner, Marijn Bauters, Matti Barthel, Travis W. Drake, Landry C. Ntaboba, Basile M. Bazirake, Johan Six, Pascal Boeckx, and Kristof Van Oost
SOIL, 7, 83–94, https://doi.org/10.5194/soil-7-83-2021, https://doi.org/10.5194/soil-7-83-2021, 2021
Short summary
Short summary
We compared stable isotope signatures of soil profiles in different forest ecosystems within the Congo Basin to assess ecosystem-level differences in N cycling, and we examined the local effect of topography on the isotopic signature of soil N. Soil δ15N profiles indicated that the N cycling in in the montane forest is more closed, whereas the lowland forest and Miombo woodland experienced a more open N cycle. Topography only alters soil δ15N values in forests with high erosional forces.
Rota Wagai, Masako Kajiura, and Maki Asano
SOIL, 6, 597–627, https://doi.org/10.5194/soil-6-597-2020, https://doi.org/10.5194/soil-6-597-2020, 2020
Short summary
Short summary
Global significance of metals (extractable Fe and Al phases) to control organic matter (OM) in recognized. Next key questions include the identification of their localization and mechanism behind OM–metal relationships. Across 23 soils of contrasting mineralogy, Fe and Al phases were mainly associated with microbially processed OM as meso-density microaggregates. OM- and metal-rich nanocomposites with a narrow OM : metal ratio likely acted as binding agents. A new conceptual model was proposed.
Marco Panettieri, Denis Courtier-Murias, Cornelia Rumpel, Marie-France Dignac, Gonzalo Almendros, and Abad Chabbi
SOIL, 6, 435–451, https://doi.org/10.5194/soil-6-435-2020, https://doi.org/10.5194/soil-6-435-2020, 2020
Short summary
Short summary
In the context of global change, soil has been identified as a potential C sink, depending on land-use strategies. This work is devoted to identifying the processes affecting labile soil C pools resulting from changes in land use. We show that the land-use change in ley grassland provoked a decoupling of the storage and degradation processes after the grassland phase. Overall, the study enables us to develop a sufficient understanding of fine-scale C dynamics to refine soil C prediction models.
Miriam Groß-Schmölders, Pascal von Sengbusch, Jan Paul Krüger, Kristy Klein, Axel Birkholz, Jens Leifeld, and Christine Alewell
SOIL, 6, 299–313, https://doi.org/10.5194/soil-6-299-2020, https://doi.org/10.5194/soil-6-299-2020, 2020
Short summary
Short summary
Degradation turns peatlands into a source of CO2. There is no cost- or time-efficient method available for indicating peatland hydrology or the success of restoration. We found that 15N values have a clear link to microbial communities and degradation. We identified trends in natural, drained and rewetted conditions and concluded that 15N depth profiles can act as a reliable and efficient tool for obtaining information on current hydrology, restoration success and drainage history.
Martin Erlandsson Lampa, Harald U. Sverdrup, Kevin H. Bishop, Salim Belyazid, Ali Ameli, and Stephan J. Köhler
SOIL, 6, 231–244, https://doi.org/10.5194/soil-6-231-2020, https://doi.org/10.5194/soil-6-231-2020, 2020
Short summary
Short summary
In this study, we demonstrate how new equations describing base cation release from mineral weathering can reproduce patterns in observations from stream and soil water. This is a major step towards modeling base cation cycling on the catchment scale, which would be valuable for defining the highest sustainable rates of forest harvest and levels of acidifying deposition.
Benjamin Andrieux, David Paré, Julien Beguin, Pierre Grondin, and Yves Bergeron
SOIL, 6, 195–213, https://doi.org/10.5194/soil-6-195-2020, https://doi.org/10.5194/soil-6-195-2020, 2020
Short summary
Short summary
Our study aimed to disentangle the contribution of several drivers to explaining the proportion of soil carbon that can be released to CO2 through microbial respiration. We found that boreal-forest soil chemistry is an important driver of the amount of carbon that microbes can process. Our results emphasize the need to include the effects of soil chemistry into models of carbon cycling to better anticipate the role played by boreal-forest soils in carbon-cycle–climate feedbacks.
Jonathan Sanderman and A. Stuart Grandy
SOIL, 6, 131–144, https://doi.org/10.5194/soil-6-131-2020, https://doi.org/10.5194/soil-6-131-2020, 2020
Short summary
Short summary
Soils contain one of the largest and most dynamic pools of carbon on Earth, yet scientists still struggle to understand the reactivity and fate of soil organic matter upon disturbance. In this study, we found that with increasing thermal stability, the turnover time of organic matter increased from decades to centuries with a concurrent shift in chemical composition. In this proof-of-concept study, we found that ramped thermal analyses can provide new insights for understanding soil carbon.
Carlos Alberto Quesada, Claudia Paz, Erick Oblitas Mendoza, Oliver Lawrence Phillips, Gustavo Saiz, and Jon Lloyd
SOIL, 6, 53–88, https://doi.org/10.5194/soil-6-53-2020, https://doi.org/10.5194/soil-6-53-2020, 2020
Short summary
Short summary
Amazon soils hold as much carbon (C) as is contained in the vegetation. In this work we sampled soils across 8 different Amazonian countries to try to understand which soil properties control current Amazonian soil C concentrations. We confirm previous knowledge that highly developed soils hold C through clay content interactions but also show a previously unreported mechanism of soil C stabilization in the younger Amazonian soil types which hold C through aluminium organic matter interactions.
Songyu Yang, Boris Jansen, Samira Absalah, Rutger L. van Hall, Karsten Kalbitz, and Erik L. H. Cammeraat
SOIL, 6, 1–15, https://doi.org/10.5194/soil-6-1-2020, https://doi.org/10.5194/soil-6-1-2020, 2020
Short summary
Short summary
Soils store large carbon and are important for global warming. We do not know what factors are important for soil carbon storage in the alpine Andes or how they work. We studied how rainfall affects soil carbon storage related to soil structure. We found soil structure is not important, but soil carbon storage and stability controlled by rainfall is dependent on rocks under the soils. The results indicate that we should pay attention to the rocks when we study soil carbon storage in the Andes.
Samuel Bouchoms, Zhengang Wang, Veerle Vanacker, and Kristof Van Oost
SOIL, 5, 367–382, https://doi.org/10.5194/soil-5-367-2019, https://doi.org/10.5194/soil-5-367-2019, 2019
Short summary
Short summary
Soil erosion has detrimental effects on soil fertility which can reduce carbon inputs coming from crops to soils. Our study integrated this effect into a model linking soil organic carbon (SOC) dynamics to erosion and crop productivity. When compared to observations, the inclusion of productivity improved SOC loss predictions. Over centuries, ignoring crop productivity evolution in models could result in underestimating SOC loss and overestimating C exchanged with the atmosphere.
Nicholas P. Rosenstock, Johan Stendahl, Gregory van der Heijden, Lars Lundin, Eric McGivney, Kevin Bishop, and Stefan Löfgren
SOIL, 5, 351–366, https://doi.org/10.5194/soil-5-351-2019, https://doi.org/10.5194/soil-5-351-2019, 2019
Short summary
Short summary
Biofuel harvests from forests involve large removals of available nutrients, necessitating accurate measurements of soil nutrient stocks. We found that dilute hydrochloric acid extractions from soils released far more Ca, Na, and K than classical salt–extracted exchangeable nutrient pools. The size of these acid–extractable pools may indicate that forest ecosystems could sustain greater biomass extractions of Ca, Mg, and K than are predicted from salt–extracted exchangeable base cation pools.
Tiphaine Chevallier, Kenji Fujisaki, Olivier Roupsard, Florian Guidat, Rintaro Kinoshita, Elias de Melo Viginio Filho, Peter Lehner, and Alain Albrecht
SOIL, 5, 315–332, https://doi.org/10.5194/soil-5-315-2019, https://doi.org/10.5194/soil-5-315-2019, 2019
Short summary
Short summary
Soil organic carbon (SOC) is the largest terrestrial C stock. Andosols of volcanic areas hold particularly large stocks (e.g. from 24 to 72 kgC m−2 in the upper 2 m of soil) as determined via MIR spectrometry at our Costa Rican study site: a 1 km2 basin covered by coffee agroforestry. Andic soil properties explained this high variability, which did not correlate with stocks in the upper 20 cm of soil. Topography and pedogenesis are needed to understand the SOC stocks at landscape scales.
Katelyn A. Congreves, Trang Phan, and Richard E. Farrell
SOIL, 5, 265–274, https://doi.org/10.5194/soil-5-265-2019, https://doi.org/10.5194/soil-5-265-2019, 2019
Short summary
Short summary
There are surprising grey areas in the precise quantification of pathways that produce nitrous oxide, a potent greenhouse gas, as influenced by soil moisture. Here, we take a new look at a classic study but use isotopomers as a powerful tool to determine the source pathways of nitrous oxide as regulated by soil moisture. Our results support earlier research, but we contribute scientific advancements by providing models that enable quantifying source partitioning rather than just inferencing.
Eric McGivney, Jon Petter Gustafsson, Salim Belyazid, Therese Zetterberg, and Stefan Löfgren
SOIL, 5, 63–77, https://doi.org/10.5194/soil-5-63-2019, https://doi.org/10.5194/soil-5-63-2019, 2019
Short summary
Short summary
Forest management may lead to long-term soil acidification due to the removal of base cations during harvest. By means of the HD-MINTEQ model, we compared the acidification effects of harvesting with the effects of historical acid rain at three forested sites in Sweden. The effects of harvesting on pH were predicted to be much smaller than those resulting from acid deposition during the 20th century. There were only very small changes in predicted weathering rates due to acid rain or harvest.
Veronika Kronnäs, Cecilia Akselsson, and Salim Belyazid
SOIL, 5, 33–47, https://doi.org/10.5194/soil-5-33-2019, https://doi.org/10.5194/soil-5-33-2019, 2019
Short summary
Short summary
Weathering rates in forest soils are important for sustainable forestry but cannot be measured. In this paper, we have modelled weathering with the commonly used PROFILE model as well as with the dynamic model ForSAFE, better suited to a changing climate with changing human activities but never before tested for weathering calculations. We show that ForSAFE gives comparable weathering rates to PROFILE and that it shows the variation in weathering with time and works well for scenario modelling.
Jon Petter Gustafsson, Salim Belyazid, Eric McGivney, and Stefan Löfgren
SOIL, 4, 237–250, https://doi.org/10.5194/soil-4-237-2018, https://doi.org/10.5194/soil-4-237-2018, 2018
Short summary
Short summary
This paper investigates how different dynamic soil chemistry models describe the processes governing aluminium and base cations in acid soil waters. We find that traditional cation-exchange equations, which are still used in many models, diverge from state-of-the-art complexation submodels such as WHAM, SHM, and NICA-Donnan when large fluctuations in pH or ionic strength occur. In conclusion, the complexation models provide a better basis for the modelling of chemical dynamics in acid soils.
Talal Darwish, Thérèse Atallah, and Ali Fadel
SOIL, 4, 225–235, https://doi.org/10.5194/soil-4-225-2018, https://doi.org/10.5194/soil-4-225-2018, 2018
Short summary
Short summary
This paper is part of the GSP-ITPS effort to produce a global SOC map and update information on C stocks using old and new soil information to assess the potential for enhanced C sequestration in dry land areas of the NENA region. We used the DSMW from FAO-UNESCO (2007), focusing on organic and inorganic content in 0.3 m of topsoil and 0.7 m of subsoil, to discuss the human factors affecting the accumulation of organic C and the fate of inorganic C.
Juhwan Lee, Gina M. Garland, and Raphael A. Viscarra Rossel
SOIL, 4, 213–224, https://doi.org/10.5194/soil-4-213-2018, https://doi.org/10.5194/soil-4-213-2018, 2018
Short summary
Short summary
Soil nitrogen (N) is an essential element for plant growth, but its plant-available forms are subject to loss from the environment by leaching and gaseous emissions. Still, factors controlling soil mineral N concentrations at large spatial scales are not well understood. We determined and discussed primary soil controls over the concentrations of NH4+ and NO3− at the continental scale of Australia while considering specific dominant land use patterns on a regional basis.
Eleanor Ursula Hobley, Brian Murphy, and Aaron Simmons
SOIL, 4, 169–171, https://doi.org/10.5194/soil-4-169-2018, https://doi.org/10.5194/soil-4-169-2018, 2018
Short summary
Short summary
This research evaluates equations to calculate soil organic carbon (SOC) stocks. Although various equations exist for SOC stock calculations, we recommend using the simplest equation with THE lowest associated errors. Adjusting SOC stock calculations for rock content is essential. Using the mass proportion of rocks to do so minimizes error.
Cora Vos, Angélica Jaconi, Anna Jacobs, and Axel Don
SOIL, 4, 153–167, https://doi.org/10.5194/soil-4-153-2018, https://doi.org/10.5194/soil-4-153-2018, 2018
Short summary
Short summary
Soil organic carbon sequestration can be facilitated by agricultural management, but its influence is not the same on all soil carbon pools. We assessed how soil organic carbon is distributed among C pools in Germany, identified factors influencing this distribution and identified regions with high vulnerability to C losses. Explanatory variables were soil texture, C / N ratio, soil C content and pH. For some regions, the drivers were linked to the land-use history as heathlands or peatlands.
Sebastian Rainer Fiedler, Jürgen Augustin, Nicole Wrage-Mönnig, Gerald Jurasinski, Bertram Gusovius, and Stephan Glatzel
SOIL, 3, 161–176, https://doi.org/10.5194/soil-3-161-2017, https://doi.org/10.5194/soil-3-161-2017, 2017
Short summary
Short summary
Injection of biogas digestates (BDs) is suspected to increase losses of N2O and thus to counterbalance prevented NH3 emissions. We determined N2O and N2 losses after mixing high concentrations of BD into two soils by an incubation under an artificial helium–oxygen atmosphere. Emissions did not increase with the application rate of BD, probably due to an inhibitory effect of the high NH4+ content in BD on nitrification. However, cumulated gaseous N losses may effectively offset NH3 reductions.
Cited articles
Ågren, G. I.: Stoichiometry and nutrition of plant growth in natural
communities, Ann. Rev. Ecol. Evol. Syst., 39, 153–70, 2008.
Bellenger, J.-P., Wichard, T., Xu, Y., and Kraepiel, A. M. L.: Essential
metals for nitrogen fixation in a free-living N2-fixing bacterium:
chelation, homeostasis and high use efficiency, Environ. Microbiol., 13,
1395–1411, 2011.
Bonzi, M.: Evaluation et déterminisme du bilan de l'azote en sols
cultivés du centre Burkina Faso: Etude par traçage isotopique
15N au cours d'essais en station et en milieu paysan. Thèse de
Doctorat Unique en Sciences Agronomique, INPL/ENSAIA, Nancy, France, 2002.
Bosshard, C.: Nitrogen dynamics in organic and conventional cropping
systems, PhD dissertation, ETH No. 17329, Swiss Federal Institute of
Technology ETH, Zurich, Switzerland, 2007.
Bosshard, C., Frossard, E., Dubois, D., Mäder, P., Manolov, I., and
Oberson, A.: Incorporation of 15N-labeled amendments into physically
separated soil organic matter fractions, Soil Sci. Soc. Am. J., 72, 949-959,
2008.
Bowman, R. A. and Moir, J. O.: Basic EDTA as an extractant for soil organic
phosphorus, Soil Sci. Soc. Am. J., 57, 1516–1518, 1993.
Bünemann, E. K., Heenan, D. P., Marschner, P., and McNeill, A. M.:
Long-term effects of crop rotation, stubble management and tillage on soil
phosphorus dynamics, Aust. J. Soil Res., 44, 611–618, 2006.
Bünemann, E. K., Smernik, R. J., Doolette, A. L., Marschner, P., Stonor,
R., Wakelin, S. A., and McNeill, A. M.: Forms of phosphorus in bacteria and
fungi isolated from two Australian soils, Soil Biol. Biochem., 40,
1908–1915, 2008a.
Bünemann, E. K., Marschner, P., Smernik, R. J., Conyers, M., and McNeill,
A. M.: Soil organic phosphorus and microbial community composition as
affected by 26 years of different management strategies, Biol. Fert.
Soils, 44, 717–726, 2008b.
Bünemann, E. K., Prusisz, B., and Ehlers, K.: Characterization of
phosphorus forms in soil microorganisms, in: Phosphorus in action –
Biological processes in soil phosphorus cycling, edited by: Bünemann, E. K.,
Oberson, A., and Frossard, E., Soil Biology Vol. 26, Springer, Heidelberg,
37–57, 2011.
Chan, K. Y. and Heenan, D. P.: Effects of lupin on soil properties and wheat
production, Aust. J. Agr. Res., 44, 1971–1984, 1993.
Chan, K. Y., Roberts, W. P., and Heenan, D. P.: Organic carbon and associated
soil properties of a Red Earth after 10 years of rotation under different
stubble and tillage practices, Aust. J. Soil Res., 30, 71–83, 1992.
Chen, X., Daniell, T. J., Neilson, R., O'Flaherty, V., and Griffiths B. S.:
Microbial and microfaunal communities in phosphorus limited, grazed
grassland change composition but maintain homeostatic nutrient
stoichiometry, Soil Biol. Biochem. 75, 94–101, 2014.
Cleveland, C. C. and Liptzin, D.: C : N : P stoichiometry in soil: is there a
“Redfield ratio” for the microbial biomass? Biogeochemistry, 85, 235–252,
2007.
Cotrufo, M. F., Wallenstein, M. D., Boot, C. M., Denef, K., and Paul, E.:
The microbial efficiency-matrix stabilization (MEMS) framework integrates
plant litter decomposition with soil organic matter stabilization: do labile
plant inputs form stable soil organic matter?, Glob. Change Biol., 19,
988–995, 2013.
Dutartre, P., Bartoli, F., Andreux, F., Portal, J. M., and Ange, A.:
Influence of content and nature of organic matter on the structure of some
sandy soils from West Africa, Geoderma, 56, 459–478, 1993.
Elser, J. J., Fagan, W. F., Kerkhoff, A. J., Swenson, N. G., and Enquist, B.
J.: Biological stoichiometry of plant production: metabolism, scaling and
ecological response to global change, New Phytol., 186, 593–608, 2010.
Esperschütz, J., Gattinger, A., Mäder, P., Schloter, M., and
Fliessbach, A.: Response of soil microbial biomass and community structures
to conventional and organic farming systems under identical crop rotations,
FEMS Microbiol. Ecol., 61, 26–37, 2007.
Fanin, N., Fromin, N., Buatois, B., and Hättenschwiler, S.: An
experimental test of the hypothesis of non-homeostatic consumer
stoichiometry in a plant litter microbe system, Ecol. Lett., 16, 764–772,
2013.
FAO, ISRIC, ISSS: World reference base for soil resources, FAO, Rome, 1998.
Fernández-Martínez, M., Vicca, S., Janssens, I. A., Sardans, J.,
Luyssaert, S., Campioli, M., Chapin III, F. S., Ciais, P., Malhi, Y.,
Obersteiner, M., Papale, D., Piao, S. L., Reichstein, M., Rodà, F., and
Peñuelas, J.: Nutrient availability as the key regulator of global
forest carbon balance, Nat. Clim. Chang., 4, 471–476, 2014.
Flisch, R., Sinaj, S., Charles, R., and Richner, W.: GRUDAF, Grundlagen
für die Düngung im Acker- und Futterbau, Agrarforschung, 16, 1–100,
2009.
Frossard, E., Condron, L. M., Oberson, A., Sinaj, S., and Fardeau, J. C.:
Processes governing phosphorus availability in temperate soils, J. Environ.
Qual., 29, 15–23, 2000.
Frostegård, Å. and Bååth, E.: The use of phospholipid fatty
acid analysis to estimate bacterial and fungal biomass in soil, Biol. Fert. Soils, 22, 59–65, 1996.
Gressel, N., McColl, J. G., Preston, C. M., Newman, R. H., and Powers, R.
F.: Linkages between phosphorus transformations and carbon decomposition in
a forest soil, Biogeochemistry, 33, 97–123, 1996.
Griffiths, B. S., Spilles, A., and Bonkowski, M.: C:N:P stoichiometry and
nutrient limitation of the soil microbial biomass in a grazed grassland site
under experimental P limitation or excess, Ecol. Process., 1,
https://doi.org/10.1186/2192-1709-1-6,
2012.
Güsewell, S.: N : P ratios in terrestrial plants: variation and functional
significance, New Phytol., 164, 243–266, 2004.
Hanson, P. J., Edwards, N. T., Garten, C. T., and Andrews, J. A.: Separating
root and soil microbial contributions to soil respiration: A review of
methods and observations, Biogeochemistry, 48, 115–146, 2000.
Harrison, A. F.: Soil organic phosphorus. A review of world literature, CAB
international, Oxon, UK, 1987.
Hartman, W. H. and Richardson, C. J.: Differential nutrient limitation of
soil microbial biomass and metabolic quotients (qCO2): Is there a
biological stoichiometry of soil microbes? PLoS ONE, 8, e57127,
https://doi.org/10.1371/journal.pone.0057127,
2013.
He, Z. L., Wu, J., O'Donnell, A. G., and Syers, J. K.: Seasonal responses in
microbial biomass carbon, phosphorus and sulphur in soils under pasture,
Biol. Fert. Soils, 24, 421–428, 1997.
Heenan, D. P. and Chan, K. Y.: The long-term effects of rotation, tillage
and stubble management on soil mineral nitrogen supply to wheat, Aust. J.
Soil Res., 30, 977–988, 1992.
Heenan, D. P. and Taylor, A. C.: Soil pH decline in relation to rotation,
tillage, stubble retention and nitrogen fertilizer in SE Australia, Soil Use
Manage., 11, 4–9, 1995.
Heenan, D. P., Taylor, A. C., Cullis, B. R., and Lill, W. J.: Long-term
effects of rotation, tillage and stubble management on wheat production in
southern NSW, Aust. J. Agric. Res., 45, 93-117, 1994.
Heenan, D. P., McGhie, W. J., Thomson, F. M., and Chan, K. Y.: Decline in
soil organic carbon and total nitrogen in relation to tillage, stubble
management, and rotation, Aust. J. Exp. Agr., 35, 877–884, 1995.
Heenan, D. P., Taylor, A. C., Chan, K. Y., McGhie, W. J., Collins, D., and
Lill, W. J.: The impact of long-term rotation, tillage and stubble
management on lupin (Lupinus angustifolius) productivity, Field Crop Res., 67, 11–23, 2000.
Heenan, D. P., Chan, K. Y., and Knight, P. G.: Long-term impact of rotation,
tillage and stubble management on the loss of soil organic carbon and
nitrogen from a Chromic Luvisol, Soil Tillage Res., 76, 59–68, 2004.
Hessen, D. O., Elser, J. J., Sterner, R. W., and Urabe, J.: Ecological
stoichiometry: An elementary approach using basic principles, Limnol.
Oceanogr., 58, 2219–2236, 2013.
Heuck, C., Weig, A., and Spohn, M.: Soil microbial biomass C : N : P
stoichiometry and microbial use of organic phosphorus, Soil Biol. Biochem.,
85, 119–129, 2015.
Hien, E.: Dynamique du carbone dans un Acrisol ferrique du Centre Ouest
Burkina: Influence des pratiques culturales sur le stock et la qualité
de la matière organique, Thèse de doctorat, Ecole Nationale
Supérieure Agronomique de Montpellier, Montpellier, France, 2004.
Kalbitz, K., Solinger, S., Park, J. H., Michalzik, B., and Matzner, E.:
Controls on the dynamics of dissolved organic matter in soils: A review,
Soil Sci., 165, 277–304, 2000.
Keller, A. and Schulin, R.: Modelling heavy metal and phosphorus balances
for farming systems, Nutr. Cycl. Agroecosys., 66, 271–284, 2003.
Keller, M., Oberson, A., Annaheim, K. E., Tamburini, F., Mäder, P.,
Mayer, J., Frossard, E., and Bünemann, E. K.: Phosphorus forms and
enzymatic hydrolysability of organic phosphorus in soils after 30 years of
organic and conventional farming, J. Plant Nutr. Soil Sc., 175, 385–393,
2012.
Kertesz, M. A. and Frossard, E.: Biological cycling of inorganic nutrients
and metals in soils and role in soil biogeochemistry, in:
Soil Microbiology, Ecology and Biochemistry, edited by: Paul, E. A., 4th Edn., Elsevier,
471–503, 2015.
Kiba, D. I.: Diversité des modes de gestion de la fertilité des sols
et de leurs effets sur la qualité des sols et la production de culture
en zones urbaine, périurbaine, et rurale au Burkina Faso, Thèse de
doctorat, Institut du développement rural, université polytechnique
de Bobo Dioulasso, Bobo Dioulasso, Burkina Faso, 2012.
Kirkby, C. A., Kirkegaard, J. A., Richardson, A. E., Wade, L. J., Blanchard,
C., and Batten, G.: Stable soil organic matter: A comparison of C : N : P:S
ratios in Australian and other world soils, Geoderma, 163, 197–208, 2011.
Kirkby, C. A., Richardson, A. E., Wade, L. J., Batten, G. D., Blanchard, C.,
and Kirkegaard, J. A.: Carbon-nutrient stoichiometry to increase soil carbon
sequestration, Soil Biol. Biochem., 60, 77–86, 2013.
Kirkby, C. A., Richardson, A. E., Wade, L. J., Passioura, J. B., Batten, G.
D., Blanchard, C., and Kirkegaard, J. A.: Nutrient availability limits
carbon sequestration in arable soils, Soil Biol. Biochem., 68, 402–409,
2014.
Leifeld, J., Reiser, R., and Oberholzer, H.-R.: Consequences of conventional
versus organic farming on soil carbon: Results from a 27-year field
experiment, Agron. J., 101, 1204–1218, 2009.
Lesschen, J. P., Stoorvogel, J. J., Smaling, E. M. A., Heuvelink, G. B. M.,
and Veldkamp, A.: A spatially explicit methodology to quantify soil nutrient
balances and their uncertainties at the national level, Nutr. Cycl.
Agroecosyst., 78, 111–131, 2007.
Loladze, I. and Elser, J. J.: The origins of the Redfield
nitrogen-to-phosphorus ratio are in a homoeostatic protein-to-rRNA ratio,
Ecol. Lett., 14, 244–250, 2011.
Lompo, F.: Effets induits des modes de gestion de la fertilité sur les
états du phosphore et la solubilisation des phosphates naturels dans
deux sols acides du Burkina Faso, thèse doctorat d'Etat, Université
de Cocody, Abidjan, Côte d'Ivoire, 2009.
Mäder, P., Fliessbach, A., Dubois, D., Gunst, L., Jossi, W., Widmer, F.,
Oberson, A., Frossard, E., Oehl, F., Wiemken, A., Gattinger, A., and Niggli,
U.: The DOK experiment (Switzerland), in: Long-term field experiments in
organic farming, edited by: Raupp, J., Pekrun, C., Oltmanns, M., and
Köpke, U., Verlag Dr. Köster, Berlin, 41–58, 2006.
Makino, W., Cotner, J. B., Sterner, R. W., and Elser, J. J.: Are bacteria
more like plants or animals? Growth rate and resource dependence of
bacterial C:N:P stoichiometry, Funct. Ecol., 17, 121–130, 2003.
McGill, W. B. and Cole, C. V.: Comparative aspects of cycling of organic C,
N, S and P through soil organic matter, Geoderma, 26, 267-286, 1981.
Miltner, A., Bombach, P., Schmidt-Brücken, B., and Kästner, M.: SOM
genesis: microbial biomass as a significant source, Biogeochemistry, 111,
41–55, 2012.
Mooshammer, M., Wanek, W., Zechmeister-Boltenstern, S., and Richter, A.:
Stoichiometric imbalances between terrestrial decomposer communities and
their resources: mechanisms and implications of microbial adaptations to
their resources, Front. Microbiol., 5, https://doi.org/10.3389/fmicb.2014.00022, 2014.
Mouginot, C., Kawamura, R., Matulich, K. L., Berlemont, R., Allison, S. D.,
Amend, A. S., and Martiny, A. C.: Elemental stoichiometry of Fungi and
Bacteria strains from grassland leaf litter, Soil Biol. Biochem., 76,
278–285, 2014.
Mulder, C., Ahrestani, F. S., Bahn, M., Bohan, D. A., Bonkowski, M.,
Griffiths, B. S., Guicharnaud, R. A., Kattge, J., Krogh, P. H., Lavorel, S.,
Lewis, O. T., Mancinelli, G., Naeem, S., Peñuelas, J., Poorter, H.,
Reich, P. B., Rossi, L., Rusch, G. M., Sardans, J., and Wright, I. J.:
Connecting the green and brown worlds: allometric and stoichiometric
predictability of above- and below-ground networks, Adv. Ecol. Res., 49,
69–175, 2013.
Nesper, M., Bünemann, E. K., Fonte, S. J., Rao, I. M., Velásquez, J.
E., Ramirez, B., Hegglin, D., Frossard, E., and Oberson, A.: Pasture
degradation decreases organic P content of tropical soils due to soil
structural decline, Geoderma, 257–258, 123–133, 2015.
Oberson, A., Frossard, E., Bühlmann, C., Mayer, J., Mäder, P., and
Lüscher, A.: Nitrogen fixation and transfer in grass-clover leys under
organic and conventional cropping systems, Plant Soil, 371, 237-255, 2013.
Oehl, F., Oberson, A., Tagmann, H. U., Besson, J. M., Dubois, D., Mäder,
P., Roth, H.-R., and Frossard, E.: Phosphorus budget and phosphorus
availability in soils under organic and conventional farming, Nutr. Cycl.
Agroecosyst., 62, 25–35, 2002.
Oenema, O., Kros, H., and de Vries, W.: Approaches and uncertainties in
nutrient budgets: implications for nutrient management and environmental
policies, Eur. J. Agron., 20, 3–16, 2003.
Ognalaga, M., Frossard, E., and Thomas, F.: Glucose-1-phosphate and
myo-inositol hexaphosphate adsorption mechanisms on goethite, Soil Sci. Soc.
Am. J., 58, 332–337, 1994.
Parton, W. J., Stewart, J. W. B., and Cole, C. V.: Dynamics of C, N, P and S
in grassland soils – a model, Biogeochemistry, 5, 109–131, 1988.
Parton, W. J., Del Grosso, S. J., Plante, A. F., Adair, E. C., and Lutz,
S. M.: Modeling the dynamics of soil organic matter and nutrient cycling, in:
Soil Microbiology, Ecology and Biochemistry, edited by: Paul, E. A., 4th
Edn., 505–537, 2015.
Pieri, C.: Fertilité des terres de savanes, Bilan de trente ans de
recherche et de développement agricoles au sud du Sahara, Ministère
de la coopération et du Développement, et CIRAD-IRAT, Paris, France,
1989.
Redfield, A. C.: The biological control of chemical factors in the
environment, Am. Sci., 46, 205–221, 1958.
Richardson, A. E., Kirkby, C. A., Banerjee, S., and Kirkegaard, J. A.: The
inorganic nutrient cost of building soil carbon, Carbon Manag., 5, 265–268,
2014.
Saunders, W. M. H. and Williams, E. G.: Observations on the determination
of total organic phosphorus in soils, J. Soil Sci., 6, 254–267, 1955.
Schmidt, M. W. I., Torn, M. S., Abiven, S., Dittmar, T., Guggenberger, G.,
Janssens, I. A., Kleber, M., Kögel-Knabner, I., Lehmann, J., Manning, D.
A. C., Nannipieri, P., Rasse, D. P., Weiner, S., and Trumbore, S. E.:
Persistence of soil organic matter as an ecosystem property, Nature, 478,
49–56, 2011.
Sedogo, M. P.: Evolution des sols ferrugineux lessivés sous culture:
incidence des modes de gestion sur la fertilité, Thèse de Doct.
D'Etat, FAST, Université Nationale de Côte d'Ivoire, Côte
d'Ivoire, 1993.
Siegrist, S., Schaub, D., Pfiffner, L., and Mäder, P.: Does organic
agriculture reduce soil erodibility? The results of a long-term field study
on loess in Switzerland, Agr. Ecosyst. Environ., 69, 253–264, 1998.
Sinaj, S., Frossard, E., and Fardeau, J. C.: Isotopically exchangeable
phosphate in size fractionated and unfractionated soils, Soil Sci. Soc. Am.
J., 61, 1413–1417, 1997.
Six, J., Bossuyt, H., Degryze, S., and Denef, K.: A history of research on
the link between (micro)aggregates, soil biota, and soil organic matter
dynamics, Soil Tillage Res., 79, 7–31, 2004.
Six, J., Frey, S. D., Thiet, R. K., and Batten, K. M.: Bacterial and fungal
contributions to carbon sequestration in agroecosystems, Soil Sci. Soc. Am.
J., 70, 555–569, 2006.
Spiess, E., Prasuhn, V., and Stauffer, W.: Influence of organic and mineral
fertilizers on nutrient leaching, Agrarforschung Schweiz, 2, 376–381, 2011.
Sterner, R. W. and Elser, J. J.: Ecological Stoichiometry: The biology of
elements from molecules to the biosphere, Princeton, NJ, Princeton
University Press, USA, 2002.
Stewart, J. W. B. and Tiessen, H.: Dynamics of soil organic phosphorus,
Biogeochemistry, 4, 41–60, 1987.
Traoré, O. Y. A., Kiba, D. I., Arnold, M. C., Fliessbach, A.,
Oberholzer, H., Nacro, H. B., Lompo, F., Oberson, A., Frossard, E., and
Bünemann, E. K.: Fertilization practices alter microbial nutrient
limitations in a Ferric Acrisol, Biol. Fert. Soils, 52, 177–189, https://doi.org/10.1007/s00374-015-1061-9,
2016.
Trivedi, P., Anderson, I. C., and Singh, B. K.: Microbial modulators of soil
carbon storage: integrating genomic and metabolic knowledge for global
prediction, Trends Microbiol., 21, 641–651, 2013.
Van Groenigen, K. J., Six, J., Hungate, B. A., de Graaff, M. A., van
Breemen, N., and van Kessel, C.: Element interactions limit soil carbon
storage, Proc. Natl. Acad. Sci. USA, 103, 6571–6574, 2006.
Vanlauwe, B., Bationo, A., Chianu, J., Giller, K. E., Merckx, R., Mokwunye,
U., Ohi-okpehai, O., Pypers, P., Tabo, R., Shepherd, K. D., Smaling, E. M.
A., Woomer, P. L., and Sanginga, N.: Integrated soil fertility management.
Operational definition and consequences for implementation and
dissemination, Outlook Agr., 39, 17–24, 2010.
Van Mooy, B. A. S., Rocap, G., Fredricks, H. F., Evans, C. T., and Devol, A.
H.: Sulfolipids dramatically decrease phosphorus demand by picocyanobacteria
in oligotrophic marine environments, Proc. Natl. Acad. Sci. USA, 6, 8607—8612, 2006.
Vitousek, P. M., Naylor, R., Crews, T., David, M. B., Drinkwater, L. E.,
Holland, E., Johnes, P. J., Katzenberger, J., Martinelli, L. A., Matson, P.
A., Nziguheba, G., Ojima, D., Palm, C. A., Robertson, G. P., Sanchez, P. A.,
Townsend, A. R., and Zhang, F. S.: Nutrient imbalances in agricultural
development, Science, 324, 1519–1520, 2009.
Von Lützow, M., Kögel-Knaber, I., Ekschmitt, K., Matzner, E.,
Guggenberger, G., Marschner, B., and Flessa, H. Stabilization of organic
matter in temperate soils: mechanisms and their relevance under different
soil conditions – a review, Eur. J. Soil Sci., 57, 426–445, 2006.
Vrede, K., Heldal, M., Norland, S., and Bratbak, G.: Elemental composition
(C, N, P) and celle volume of exponentially growing and nutrient-limited
bacterioplankton, Appl. Environ. Microbiol., 68, 2965–2971, 2002.
Wang, X. M., Liu, F., Tan, W. F., Li, W., Feng, X. H., and Sparks, D. L.:
Characteristics of phosphate adsorption-desorption onto ferrihydrite:
comparison with well-crystalline Fe (hydr)oxides, Soil Sci., 178, 1–11,
2013.
Woodward, G., Gessner, M. O., Giller, P. S., Gulis, V., Hladyz, S., Lecerf,
A., Malmqvist, B., McKie, B. G., Tiegs, S. D., Cariss, H., Dobson, M.,
Elosegi, A., Ferreira, V., Graca, M. A. S., Fleituch, T., Lacoursiere, J.
O., Nistorescu, M., Pozo, J., Risnoveanu, G., Schindler, M., Vadineanu, A.,
Vought, L. B. M., and Chauvet, E.: Continental-scale effects of nutrient
pollution on stream ecosystem functioning, Science, 336, 1438–1440,
2012.
Xu, X., Thornton, P. E., and Post, W. M.: A global analysis of soil
microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems,
Global Ecol. Biogeogr., 22, 737–749, 2013.
Zhang, G. S., Chan, K. Y., Oates, A., Heenan, D. P., and Huang, G. B.:
Relationship between soil structure and runoff/soil loss after 24 years of
conservation tillage, Soil Till. Res., 92, 122–128, 2007.
Zida, Z., Ouédraogo, E., Mando, A., and Stroosnijder, L.: Termite and
earthworm abundance and taxonomic richness under long-term conservation soil
management in Saria, Burkina Faso, West Africa, Appl. Soil Ecol., 51, 122–129, 2011.
Zougmoré, R., Mando, A., Stroosnijder, L., and Guillobez, S.: Nitrogen
flows and balances as affected by water and nutrient management in a sorghum
cropping system of semiarid Burkina Faso, Field Crop Res., 90, 235–244,
2004.
