Articles | Volume 15, issue 9
https://doi.org/10.5194/bg-15-2743-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-2743-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Massive carbon addition to an organic-rich Andosol increased the subsoil but not the topsoil carbon stock
Antonia Zieger
CORRESPONDING AUTHOR
Chair of Soil Science, Institute of Ecology, Technische
Universität Berlin, Ernst-Reuter-Platz 1, 10587 Berlin, Germany
Klaus Kaiser
Soil Science and Soil Protection, Martin Luther University
Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120 Halle (Saale), Germany
Pedro Ríos Guayasamín
Laboratorio de Ecología Tropical Natural y Aplicada,
Universidad Estatal Amazónica, Campus Principal Km 2.1/2 via a Napo (Paso
Lateral) Puyo, Pastaza, Ecuador
Martin Kaupenjohann
Chair of Soil Science, Institute of Ecology, Technische
Universität Berlin, Ernst-Reuter-Platz 1, 10587 Berlin, Germany
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Cited
16 citations as recorded by crossref.
- Legacy Effects of Sorption Determine the Formation Efficiency of Mineral-Associated Soil Organic Matter S. Chen et al. 10.1021/acs.est.1c06880
- Conversion of forest to cinnamon plantation depletes soil carbon stocks in the top metre of the tropical highlands of Kerinci Regency, Jambi Province, Indonesia D. Antony et al. 10.1111/sum.12974
- Deep-C storage: Biological, chemical and physical strategies to enhance carbon stocks in agricultural subsoils E. Button et al. 10.1016/j.soilbio.2022.108697
- Biochar effects on NTFP-enriched secondary forest growth and soil properties in Amazonian Ecuador P. Ríos Guayasamín et al. 10.1016/j.jenvman.2023.119068
- Stable oxic-anoxic transitional interface is beneficial to retard soil carbon loss in drained peatland L. Liu et al. 10.1016/j.soilbio.2023.109024
- Soil carbon stocks of regenerating Icelandic native birch woodlands: Effects of space and time S. Sanchez et al. 10.1016/j.scitotenv.2024.178063
- Comparing amorphous silica, short-range-ordered silicates and silicic acid species by FTIR R. Ellerbrock et al. 10.1038/s41598-022-15882-4
- Aggregate stability of south Chilean volcanic ash soils – A combined XPS, contact angle, and surface charge analysis J. Bachmann et al. 10.1016/j.geoderma.2019.114022
- Microscale spatial distribution and soil organic matter persistence in top and subsoil T. Inagaki et al. 10.1016/j.soilbio.2022.108921
- Pemanfaatan Bioarang pada Beragam Cekaman Air untuk Ketersediaan Fosforus Guna Meningkatkan Produktivitas Kedelai Anjasmoro (Glycine max L. Merrill.) A. Prasetya et al. 10.18343/jipi.29.1.99
- What do relationships between extractable metals and soil organic carbon concentrations mean? S. Hall & A. Thompson 10.1002/saj2.20343
- 15-year fertilization increased soil organic carbon stock even in systems reputed to be saturated like permanent grassland on andosols L. Edouard Rambaut et al. 10.1016/j.geoderma.2022.116025
- Effects of Glucose Addition on Dynamics of Organic Carbon Fractions and cbbL-Containing Bacteria in Wetlands Q. Cao et al. 10.3390/app122010239
- .No-tillage intercropping with a robotic mower: advancing a high productivity, low-carbon and energy-efficient organic farming system1 Q. Huang et al. 10.1016/j.energy.2025.135851
- Impacts of Landscape Evolution on Heterotrophic Carbon Loss in Intensively Managed Landscapes Q. Yan & P. Kumar 10.3389/frwa.2021.666278
- Three‐Dimensional Modeling of the Coevolution of Landscape and Soil Organic Carbon Q. Yan et al. 10.1029/2018WR023634
14 citations as recorded by crossref.
- Legacy Effects of Sorption Determine the Formation Efficiency of Mineral-Associated Soil Organic Matter S. Chen et al. 10.1021/acs.est.1c06880
- Conversion of forest to cinnamon plantation depletes soil carbon stocks in the top metre of the tropical highlands of Kerinci Regency, Jambi Province, Indonesia D. Antony et al. 10.1111/sum.12974
- Deep-C storage: Biological, chemical and physical strategies to enhance carbon stocks in agricultural subsoils E. Button et al. 10.1016/j.soilbio.2022.108697
- Biochar effects on NTFP-enriched secondary forest growth and soil properties in Amazonian Ecuador P. Ríos Guayasamín et al. 10.1016/j.jenvman.2023.119068
- Stable oxic-anoxic transitional interface is beneficial to retard soil carbon loss in drained peatland L. Liu et al. 10.1016/j.soilbio.2023.109024
- Soil carbon stocks of regenerating Icelandic native birch woodlands: Effects of space and time S. Sanchez et al. 10.1016/j.scitotenv.2024.178063
- Comparing amorphous silica, short-range-ordered silicates and silicic acid species by FTIR R. Ellerbrock et al. 10.1038/s41598-022-15882-4
- Aggregate stability of south Chilean volcanic ash soils – A combined XPS, contact angle, and surface charge analysis J. Bachmann et al. 10.1016/j.geoderma.2019.114022
- Microscale spatial distribution and soil organic matter persistence in top and subsoil T. Inagaki et al. 10.1016/j.soilbio.2022.108921
- Pemanfaatan Bioarang pada Beragam Cekaman Air untuk Ketersediaan Fosforus Guna Meningkatkan Produktivitas Kedelai Anjasmoro (Glycine max L. Merrill.) A. Prasetya et al. 10.18343/jipi.29.1.99
- What do relationships between extractable metals and soil organic carbon concentrations mean? S. Hall & A. Thompson 10.1002/saj2.20343
- 15-year fertilization increased soil organic carbon stock even in systems reputed to be saturated like permanent grassland on andosols L. Edouard Rambaut et al. 10.1016/j.geoderma.2022.116025
- Effects of Glucose Addition on Dynamics of Organic Carbon Fractions and cbbL-Containing Bacteria in Wetlands Q. Cao et al. 10.3390/app122010239
- .No-tillage intercropping with a robotic mower: advancing a high productivity, low-carbon and energy-efficient organic farming system1 Q. Huang et al. 10.1016/j.energy.2025.135851
Discussed (final revised paper)
Latest update: 02 Apr 2025
Short summary
We tested a current theory, which proposes an upper limit for organic carbon (OC) stocks independent of increasing carbon input for a soil with already large OC stocks. The soil received a large additional carbon input as sawdust. In response, only the OC stock in 25–50 cm depth increased significantly. We assume, that due to saturation in 0–25 cm, added OC migrates downwards and becomes retained in 25–50 cm. This indicates the possibility to sustainably increase already large OC stocks further.
We tested a current theory, which proposes an upper limit for organic carbon (OC) stocks...
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