Articles | Volume 16, issue 24
https://doi.org/10.5194/bg-16-4783-2019
© 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/bg-16-4783-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Reviews and syntheses
| 
17 Dec 2019
Reviews and syntheses |
| 17 Dec 2019
| 17 Dec 2019
Reviews and syntheses: Agropedogenesis – humankind as the sixth soil-forming factor and attractors of agricultural soil degradation
Department of Soil Science of Temperate Ecosystems, Georg-August-Universität Göttingen, Büsgenweg 2, 37077 Göttingen, Germany
Department of Agricultural Soil Science, Georg-August-Universität Göttingen, Büsgenweg 2, 37077 Göttingen, Germany
Kazem Zamanian
CORRESPONDING AUTHOR
Department of Soil Science of Temperate Ecosystems, Georg-August-Universität Göttingen, Büsgenweg 2, 37077 Göttingen, Germany
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Peter Mueller, Lisa M. Schile-Beers, Thomas J. Mozdzer, Gail L. Chmura, Thomas Dinter, Yakov Kuzyakov, Alma V. de Groot, Peter Esselink, Christian Smit, Andrea D'Alpaos, Carles Ibáñez, Magdalena Lazarus, Urs Neumeier, Beverly J. Johnson, Andrew H. Baldwin, Stephanie A. Yarwood, Diana I. Montemayor, Zaichao Yang, Jihua Wu, Kai Jensen, and Stefanie Nolte
Biogeosciences, 15, 3189–3202, https://doi.org/10.5194/bg-15-3189-2018, https://doi.org/10.5194/bg-15-3189-2018, 2018
Jie Chen, Guoliang Xiao, Yakov Kuzyakov, G. Darrel Jenerette, Ying Ma, Wei Liu, Zhengfeng Wang, and Weijun Shen
Biogeosciences, 14, 2513–2525, https://doi.org/10.5194/bg-14-2513-2017, https://doi.org/10.5194/bg-14-2513-2017, 2017
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We conducted a field manipulation experiment by redistributing 67 % of dry-season rainfall into the wet season while keeping the annual rainfall unchanged in a subtropical forest. Soil net nitrification and N mineralization rates were decreased by 13–20 % in the dry season and increased by 50 % with an accelerated NO3 leaching in the wet season. Functional microbial gene abundance and microbial biomass were the main factors affecting the N-process responses to the rainfall seasonality changes.
This article is included in the Encyclopedia of Geosciences
Anna Gunina, Michaela Dippold, Bruno Glaser, and Yakov Kuzyakov
Biogeosciences, 14, 271–283, https://doi.org/10.5194/bg-14-271-2017, https://doi.org/10.5194/bg-14-271-2017, 2017
Johannes Krohn, Ivana Lozanovska, Yakov Kuzyakov, and Maxim Dorodnikov
Biogeosciences Discuss., https://doi.org/10.5194/bg-2016-162, https://doi.org/10.5194/bg-2016-162, 2016
Revised manuscript not accepted
W. Babel, T. Biermann, H. Coners, E. Falge, E. Seeber, J. Ingrisch, P.-M. Schleuß, T. Gerken, J. Leonbacher, T. Leipold, S. Willinghöfer, K. Schützenmeister, O. Shibistova, L. Becker, S. Hafner, S. Spielvogel, X. Li, X. Xu, Y. Sun, L. Zhang, Y. Yang, Y. Ma, K. Wesche, H.-F. Graf, C. Leuschner, G. Guggenberger, Y. Kuzyakov, G. Miehe, and T. Foken
Biogeosciences, 11, 6633–6656, https://doi.org/10.5194/bg-11-6633-2014, https://doi.org/10.5194/bg-11-6633-2014, 2014
Peter Mueller, Lisa M. Schile-Beers, Thomas J. Mozdzer, Gail L. Chmura, Thomas Dinter, Yakov Kuzyakov, Alma V. de Groot, Peter Esselink, Christian Smit, Andrea D'Alpaos, Carles Ibáñez, Magdalena Lazarus, Urs Neumeier, Beverly J. Johnson, Andrew H. Baldwin, Stephanie A. Yarwood, Diana I. Montemayor, Zaichao Yang, Jihua Wu, Kai Jensen, and Stefanie Nolte
Biogeosciences, 15, 3189–3202, https://doi.org/10.5194/bg-15-3189-2018, https://doi.org/10.5194/bg-15-3189-2018, 2018
Jie Chen, Guoliang Xiao, Yakov Kuzyakov, G. Darrel Jenerette, Ying Ma, Wei Liu, Zhengfeng Wang, and Weijun Shen
Biogeosciences, 14, 2513–2525, https://doi.org/10.5194/bg-14-2513-2017, https://doi.org/10.5194/bg-14-2513-2017, 2017
Short summary
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We conducted a field manipulation experiment by redistributing 67 % of dry-season rainfall into the wet season while keeping the annual rainfall unchanged in a subtropical forest. Soil net nitrification and N mineralization rates were decreased by 13–20 % in the dry season and increased by 50 % with an accelerated NO3 leaching in the wet season. Functional microbial gene abundance and microbial biomass were the main factors affecting the N-process responses to the rainfall seasonality changes.
This article is included in the Encyclopedia of Geosciences
Anna Gunina, Michaela Dippold, Bruno Glaser, and Yakov Kuzyakov
Biogeosciences, 14, 271–283, https://doi.org/10.5194/bg-14-271-2017, https://doi.org/10.5194/bg-14-271-2017, 2017
Johannes Krohn, Ivana Lozanovska, Yakov Kuzyakov, and Maxim Dorodnikov
Biogeosciences Discuss., https://doi.org/10.5194/bg-2016-162, https://doi.org/10.5194/bg-2016-162, 2016
Revised manuscript not accepted
W. Babel, T. Biermann, H. Coners, E. Falge, E. Seeber, J. Ingrisch, P.-M. Schleuß, T. Gerken, J. Leonbacher, T. Leipold, S. Willinghöfer, K. Schützenmeister, O. Shibistova, L. Becker, S. Hafner, S. Spielvogel, X. Li, X. Xu, Y. Sun, L. Zhang, Y. Yang, Y. Ma, K. Wesche, H.-F. Graf, C. Leuschner, G. Guggenberger, Y. Kuzyakov, G. Miehe, and T. Foken
Biogeosciences, 11, 6633–6656, https://doi.org/10.5194/bg-11-6633-2014, https://doi.org/10.5194/bg-11-6633-2014, 2014
Related subject area
Biogeochemistry: Soils
Vegetation patterns associated with nutrient availability and supply in high-elevation tropical Andean ecosystems
Technical note: An open-source, low-cost system for continuous monitoring of low nitrate concentrations in soil and open water
Long-term fertilization increases soil but not plant or microbial N in a Chihuahuan Desert grassland
Factors controlling spatiotemporal variability of soil carbon accumulation and stock estimates in a tidal salt marsh
Moisture and temperature effects on the radiocarbon signature of respired carbon dioxide to assess stability of soil carbon in the Tibetan Plateau
Technical Note: A validated correction method to quantify organic and inorganic carbon in soils using Rock-Eval® thermal analysis
Non-mycorrhizal root-associated fungi increase soil C stocks and stability via diverse mechanisms
Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change in chemical structure
Diverse organic carbon dynamics captured by radiocarbon analysis of distinct compound classes in a grassland soil
Soil priming effects and involved microbial community along salt gradients
Adjustments to the Rock-Eval® thermal analysis for soil organic and inorganic carbon quantification
Ecosystem-specific patterns and drivers of global reactive iron mineral-associated organic carbon
Dark septate endophytic fungi associated with pioneer grass inhabiting volcanic deposits and their functions in promoting plant growth
Global patterns and drivers of phosphorus fractions in natural soils
Reviews and syntheses: Iron – a driver of nitrogen bioavailability in soils?
The Effects of Land Use on Soil Carbon Stocks in the UK
How well does ramped thermal oxidation quantify the age distribution of soil carbon? Assessing thermal stability of physically and chemically fractionated soil organic matter
Differential temperature sensitivity of intracellular metabolic processes and extracellular soil enzyme activities
Mapping soil organic carbon fractions for Australia, their stocks, and uncertainty
Technical note: The recovery rate of free particulate organic matter from soil samples is strongly affected by the method of density fractionation
Deforestation for agriculture leads to soil warming and enhanced litter decomposition in subarctic soils
Temperature sensitivity of soil organic carbon respiration along a forested elevation gradient in the Rwenzori Mountains, Uganda
The influence of elevated CO2 and soil depth on rhizosphere activity and nutrient availability in a mature Eucalyptus woodland
The paradox of assessing greenhouse gases from soils for nature-based solutions
Management-induced changes in soil organic carbon on global croplands
Pore network modeling as a new tool for determining gas diffusivity in peat
Temperature sensitivity of dark CO2 fixation in temperate forest soils
Effects of precipitation seasonality, irrigation, vegetation cycle and soil type on enhanced weathering – modeling of cropland case studies across four sites
Stable isotope profiles of soil organic carbon in forested and grassland landscapes in the Lake Alaotra basin (Madagascar): insights in past vegetation changes
Reviews and syntheses: The promise of big diverse soil data, moving current practices towards future potential
Dynamics of rare earth elements and associated major and trace elements during Douglas-fir (Pseudotsuga menziesii) and European beech (Fagus sylvatica L.) litter degradation
To what extent can soil moisture and soil Cu contamination stresses affect nitrous species emissions? Estimation through calibration of a nitrification–denitrification model
Carbon, nitrogen, and phosphorus stoichiometry of organic matter in Swedish forest soils and its relationship with climate, tree species, and soil texture
Soil geochemistry as a driver of soil organic matter composition: insights from a soil chronosequence
Leaching of inorganic and organic phosphorus and nitrogen in contrasting beech forest soils – seasonal patterns and effects of fertilization
Age and chemistry of dissolved organic carbon reveal enhanced leaching of ancient labile carbon at the permafrost thaw zone
Soil organic carbon stabilization mechanisms and temperature sensitivity in old terraced soils
Effect of organic carbon addition on paddy soil organic carbon decomposition under different irrigation regimes
Soil profile connectivity can impact microbial substrate use, affecting how soil CO2 effluxes are controlled by temperature
Additional carbon inputs to reach a 4 per 1000 objective in Europe: feasibility and projected impacts of climate change based on Century simulations of long-term arable experiments
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Representing methane emissions from wet tropical forest soils using microbial functional groups constrained by soil diffusivity
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Geochemical zones and environmental gradients for soils from the central Transantarctic Mountains, Antarctica
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Denitrification in soil as a function of oxygen availability at the microscale
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Armando Molina, Veerle Vanacker, Oliver Chadwick, Santiago Zhiminaicela, Marife Corre, and Edzo Veldkamp
Biogeosciences, 21, 3075–3091, https://doi.org/10.5194/bg-21-3075-2024, https://doi.org/10.5194/bg-21-3075-2024, 2024
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The tropical Andes contains unique landscapes where forest patches are surrounded by tussock grasses and cushion-forming plants. The aboveground vegetation composition informs us about belowground nutrient availability: patterns in plant-available nutrients resulted from strong biocycling of cations and removal of soil nutrients by plant uptake or leaching. Future changes in vegetation distribution will affect soil water and solute fluxes and the aquatic ecology of Andean rivers and lakes.
This article is included in the Encyclopedia of Geosciences
Sahiti Bulusu, Cristina Prieto García, Helen E. Dahlke, and Elad Levintal
Biogeosciences, 21, 3007–3013, https://doi.org/10.5194/bg-21-3007-2024, https://doi.org/10.5194/bg-21-3007-2024, 2024
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Do-it-yourself hardware is a new way to improve measurement resolution. We present a low-cost, automated system for field measurements of low nitrate concentrations in soil porewater and open water bodies. All data hardware components cost USD 1100, which is much cheaper than other available commercial solutions. We provide the complete building guide to reduce technical barriers, which we hope will allow easier reproducibility and set up new soil and environmental monitoring applications.
This article is included in the Encyclopedia of Geosciences
Violeta Mendoza-Martinez, Scott L. Collins, and Jennie R. McLaren
Biogeosciences, 21, 2655–2667, https://doi.org/10.5194/bg-21-2655-2024, https://doi.org/10.5194/bg-21-2655-2024, 2024
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We examine the impacts of multi-decadal nitrogen additions on a dryland ecosystem N budget, including the soil, microbial, and plant N pools. After 26 years, there appears to be little impact on the soil microbial or plant community and only minimal increases in N pools within the soil. While perhaps encouraging from a conservation standpoint, we calculate that greater than 95 % of the nitrogen added to the system is not retained and is instead either lost deeper in the soil or emitted as gas.
This article is included in the Encyclopedia of Geosciences
Sean Fettrow, Andrew Wozniak, Holly A. Michael, and Angelia L. Seyfferth
Biogeosciences, 21, 2367–2384, https://doi.org/10.5194/bg-21-2367-2024, https://doi.org/10.5194/bg-21-2367-2024, 2024
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Salt marshes play a big role in global carbon (C) storage, and C stock estimates are used to predict future changes. However, spatial and temporal gradients in C burial rates over the landscape exist due to variations in water inundation, dominant plant species and stage of growth, and tidal action. We quantified soil C concentrations in soil cores across time and space beside several porewater biogeochemical variables and discussed the controls on variability in soil C in salt marsh ecosystems.
This article is included in the Encyclopedia of Geosciences
Andrés Tangarife-Escobar, Georg Guggenberger, Xiaojuan Feng, Guohua Dai, Carolina Urbina-Malo, Mina Azizi-Rad, and Carlos A. Sierra
Biogeosciences, 21, 1277–1299, https://doi.org/10.5194/bg-21-1277-2024, https://doi.org/10.5194/bg-21-1277-2024, 2024
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Soil organic matter stability depends on future temperature and precipitation scenarios. We used radiocarbon (14C) data and model predictions to understand how the transit time of carbon varies under environmental change in grasslands and peatlands. Soil moisture affected the Δ14C of peatlands, while temperature did not have any influence. Our models show the correspondence between Δ14C and transit time and could allow understanding future interactions between terrestrial and atmospheric carbon
This article is included in the Encyclopedia of Geosciences
Marija Stojanova, Pierre Arbelet, François Baudin, Nicolas Bouton, Giovanni Caria, Lorenza Pacini, Nicolas Proix, Edouard Quibel, Achille Thin, and Pierre Barré
EGUsphere, https://doi.org/10.5194/egusphere-2024-578, https://doi.org/10.5194/egusphere-2024-578, 2024
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Because of its importance for climate regulation and soil health, many studies are focusing on carbon dynamics in soils. However, quantifying organic and inorganic carbon remains an issue in carbonated soils. In this technical note, we propose a validated correction method to quantify organic and inorganic carbon in soils using Rock-Eval® thermal analysis. With this correction, Rock-Eval® method has the potential to become the standard method for quantifying carbon in carbonate soils.
This article is included in the Encyclopedia of Geosciences
Emiko K. Stuart, Laura Castañeda-Gómez, Wolfram Buss, Jeff R. Powell, and Yolima Carrillo
Biogeosciences, 21, 1037–1059, https://doi.org/10.5194/bg-21-1037-2024, https://doi.org/10.5194/bg-21-1037-2024, 2024
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We inoculated wheat plants with various types of fungi whose impacts on soil carbon are poorly understood. After several months of growth, we examined both their impacts on soil carbon and the underlying mechanisms using multiple methods. Overall the fungi benefitted the storage of carbon in soil, mainly by improving the stability of pre-existing carbon, but several pathways were involved. This study demonstrates their importance for soil carbon storage and, therefore, climate change mitigation.
This article is included in the Encyclopedia of Geosciences
Huimin Sun, Michael W. I. Schmidt, Jintao Li, Jinquan Li, Xiang Liu, Nicholas O. E. Ofiti, Shurong Zhou, and Ming Nie
Biogeosciences, 21, 575–589, https://doi.org/10.5194/bg-21-575-2024, https://doi.org/10.5194/bg-21-575-2024, 2024
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A soil organic carbon (SOC) molecular structure suggested that the easily decomposable and stabilized SOC is similarly affected after 9-year warming and N treatments despite large changes in SOC stocks. Given the long residence time of some SOC, the similar loss of all measurable chemical forms of SOC under global change treatments could have important climate consequences.
This article is included in the Encyclopedia of Geosciences
Katherine E. Grant, Marisa N. Repasch, Kari M. Finstad, Julia D. Kerr, Maxwell A. T. Marple, Christopher J. Larson, Taylor A. B. Broek, Jennifer Pett-Ridge, and Karis J. McFarlane
EGUsphere, https://doi.org/10.5194/egusphere-2023-3125, https://doi.org/10.5194/egusphere-2023-3125, 2024
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Soils store organic carbon composed of different compounds from plants and microbes that stays in the soils for different lengths of time. To understand this process, we measure the time each carbon fraction is in a grassland soil profile. Our results show that the length of time each individual soil fraction is in our soil changes. Our approach allows a detailed look at the different components in soils. This study can help improve our understanding of soil dynamics.
This article is included in the Encyclopedia of Geosciences
Haoli Zhang, Doudou Chang, Zhifeng Zhu, Chunmei Meng, and Kaiyong Wang
Biogeosciences, 21, 1–11, https://doi.org/10.5194/bg-21-1-2024, https://doi.org/10.5194/bg-21-1-2024, 2024
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Soil salinity mediates microorganisms and soil processes like soil organic carbon (SOC) cycling. We observed that negative priming effects at the early stages might be due to the preferential utilization of cottonseed meal. The positive priming that followed decreased with the increase in salinity.
This article is included in the Encyclopedia of Geosciences
Joséphine Hazera, David Sebag, Isabelle Kowalewski, Eric Verrecchia, Herman Ravelojaona, and Tiphaine Chevallier
Biogeosciences, 20, 5229–5242, https://doi.org/10.5194/bg-20-5229-2023, https://doi.org/10.5194/bg-20-5229-2023, 2023
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This study adapts the Rock-Eval® protocol to quantify soil organic carbon (SOC) and soil inorganic carbon (SIC) on a non-pretreated soil aliquot. The standard protocol properly estimates SOC contents once the TOC parameter is corrected. However, it cannot complete the thermal breakdown of SIC amounts > 4 mg, leading to an underestimation of high SIC contents by the MinC parameter, even after correcting for this. Thus, the final oxidation isotherm is extended to 7 min to quantify any SIC amount.
This article is included in the Encyclopedia of Geosciences
Bo Zhao, Amin Dou, Zhiwei Zhang, Zhenyu Chen, Wenbo Sun, Yanli Feng, Xiaojuan Wang, and Qiang Wang
Biogeosciences, 20, 4761–4774, https://doi.org/10.5194/bg-20-4761-2023, https://doi.org/10.5194/bg-20-4761-2023, 2023
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This study provided a comprehensive analysis of the spatial variability and determinants of Fe-bound organic carbon (Fe-OC) among terrestrial, wetland, and marine ecosystems and its governing factors globally. We illustrated that reactive Fe was not only an important sequestration mechanism for OC in terrestrial ecosystems but also an effective “rusty sink” of OC preservation in wetland and marine ecosystems, i.e., a key factor for long-term OC storage in global ecosystems.
This article is included in the Encyclopedia of Geosciences
Han Sun, Tomoyasu Nishizawa, Hiroyuki Ohta, and Kazuhiko Narisawa
Biogeosciences, 20, 4737–4749, https://doi.org/10.5194/bg-20-4737-2023, https://doi.org/10.5194/bg-20-4737-2023, 2023
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In this research, we assessed the diversity and function of the dark septate endophytic (DSE) fungi community associated with Miscanthus condensatus root in volcanic ecosystems. Both metabarcoding and isolation were adopted in this study. We further validated effects on plant growth by inoculation of some core DSE isolates. This study helps improve our understanding of the role of Miscanthus condensatus-associated DSE fungi during the restoration of post-volcanic ecosystems.
This article is included in the Encyclopedia of Geosciences
Xianjin He, Laurent Augusto, Daniel S. Goll, Bruno Ringeval, Ying-Ping Wang, Julian Helfenstein, Yuanyuan Huang, and Enqing Hou
Biogeosciences, 20, 4147–4163, https://doi.org/10.5194/bg-20-4147-2023, https://doi.org/10.5194/bg-20-4147-2023, 2023
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We identified total soil P concentration as the most important predictor of all soil P pool concentrations, except for primary mineral P concentration, which is primarily controlled by soil pH and only secondarily by total soil P concentration. We predicted soil P pools’ distributions in natural systems, which can inform assessments of the role of natural P availability for ecosystem productivity, climate change mitigation, and the functioning of the Earth system.
This article is included in the Encyclopedia of Geosciences
Imane Slimani, Xia Zhu-Barker, Patricia Lazicki, and William Horwath
Biogeosciences, 20, 3873–3894, https://doi.org/10.5194/bg-20-3873-2023, https://doi.org/10.5194/bg-20-3873-2023, 2023
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There is a strong link between nitrogen availability and iron minerals in soils. These minerals have multiple outcomes for nitrogen availability depending on soil conditions and properties. For example, iron can limit microbial degradation of nitrogen in aerated soils but has opposing outcomes in non-aerated soils. This paper focuses on the multiple ways iron can affect nitrogen bioavailability in soils.
This article is included in the Encyclopedia of Geosciences
Peter Levy, Laura Bentley, Bridget Emmett, Angus Garbutt, Aidan Keith, Inma Lebron, and David Robinson
EGUsphere, https://doi.org/10.5194/egusphere-2023-1681, https://doi.org/10.5194/egusphere-2023-1681, 2023
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We collated a large data set (15790 soil cores) on soil carbon stock in different land uses. Soil carbon stocks were highest in woodlands and lowest in croplands. The variability in the effects were large. This has important implications for agri-environment schemes, seeking to sequester carbon in the soil by altering land use, because the effect of a given intervention is very hard to verify.
This article is included in the Encyclopedia of Geosciences
Shane W. Stoner, Marion Schrumpf, Alison Hoyt, Carlos A. Sierra, Sebastian Doetterl, Valier Galy, and Susan Trumbore
Biogeosciences, 20, 3151–3163, https://doi.org/10.5194/bg-20-3151-2023, https://doi.org/10.5194/bg-20-3151-2023, 2023
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Soils store more carbon (C) than any other terrestrial C reservoir, but the processes that control how much C stays in soil, and for how long, are very complex. Here, we used a recent method that involves heating soil in the lab to measure the range of C ages in soil. We found that most C in soil is decades to centuries old, while some stays for much shorter times (days to months), and some is thousands of years old. Such detail helps us to estimate how soil C may react to changing climate.
This article is included in the Encyclopedia of Geosciences
Adetunji Alex Adekanmbi, Laurence Dale, Liz Shaw, and Tom Sizmur
Biogeosciences, 20, 2207–2219, https://doi.org/10.5194/bg-20-2207-2023, https://doi.org/10.5194/bg-20-2207-2023, 2023
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The decomposition of soil organic matter and flux of carbon dioxide are expected to increase as temperatures rise. However, soil organic matter decomposition is a two-step process whereby large molecules are first broken down outside microbial cells and then respired within microbial cells. We show here that these two steps are not equally sensitive to increases in soil temperature and that global warming may cause a shift in the rate-limiting step from outside to inside the microbial cell.
This article is included in the Encyclopedia of Geosciences
Mercedes Román Dobarco, Alexandre M. J-C. Wadoux, Brendan Malone, Budiman Minasny, Alex B. McBratney, and Ross Searle
Biogeosciences, 20, 1559–1586, https://doi.org/10.5194/bg-20-1559-2023, https://doi.org/10.5194/bg-20-1559-2023, 2023
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Soil organic carbon (SOC) is of a heterogeneous nature and varies in chemistry, stabilisation mechanisms, and persistence in soil. In this study we mapped the stocks of SOC fractions with different characteristics and turnover rates (presumably PyOC >= MAOC > POC) across Australia, combining spectroscopy and digital soil mapping. The SOC stocks (0–30 cm) were estimated as 13 Pg MAOC, 2 Pg POC, and 5 Pg PyOC.
This article is included in the Encyclopedia of Geosciences
Frederick Büks
Biogeosciences, 20, 1529–1535, https://doi.org/10.5194/bg-20-1529-2023, https://doi.org/10.5194/bg-20-1529-2023, 2023
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Ultrasonication with density fractionation of soils is a commonly used method to separate soil organic matter pools, which is, e.g., important to calculate carbon turnover in landscapes. It is shown that the approach that merges soil and dense solution without mixing has a low recovery rate and causes co-extraction of parts of the retained labile pool along with the intermediate pool. An alternative method with high recovery rates and no cross-contamination was recommended.
This article is included in the Encyclopedia of Geosciences
Tino Peplau, Christopher Poeplau, Edward Gregorich, and Julia Schroeder
Biogeosciences, 20, 1063–1074, https://doi.org/10.5194/bg-20-1063-2023, https://doi.org/10.5194/bg-20-1063-2023, 2023
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We buried tea bags and temperature loggers in a paired-plot design in soils under forest and agricultural land and retrieved them after 2 years to quantify the effect of land-use change on soil temperature and litter decomposition in subarctic agricultural systems. We could show that agricultural soils were on average 2 °C warmer than forests and that litter decomposition was enhanced. The results imply that deforestation amplifies effects of climate change on soil organic matter dynamics.
This article is included in the Encyclopedia of Geosciences
Joseph Okello, Marijn Bauters, Hans Verbeeck, Samuel Bodé, John Kasenene, Astrid Françoys, Till Engelhardt, Klaus Butterbach-Bahl, Ralf Kiese, and Pascal Boeckx
Biogeosciences, 20, 719–735, https://doi.org/10.5194/bg-20-719-2023, https://doi.org/10.5194/bg-20-719-2023, 2023
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The increase in global and regional temperatures has the potential to drive accelerated soil organic carbon losses in tropical forests. We simulated climate warming by translocating intact soil cores from higher to lower elevations. The results revealed increasing temperature sensitivity and decreasing losses of soil organic carbon with increasing elevation. Our results suggest that climate warming may trigger enhanced losses of soil organic carbon from tropical montane forests.
This article is included in the Encyclopedia of Geosciences
Johanna Pihlblad, Louise C. Andresen, Catriona A. Macdonald, David S. Ellsworth, and Yolima Carrillo
Biogeosciences, 20, 505–521, https://doi.org/10.5194/bg-20-505-2023, https://doi.org/10.5194/bg-20-505-2023, 2023
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Elevated CO2 in the atmosphere increases forest biomass productivity when growth is not limited by soil nutrients. This study explores how mature trees stimulate soil availability of nitrogen and phosphorus with free-air carbon dioxide enrichment after 5 years of fumigation. We found that both nutrient availability and processes feeding available pools increased in the rhizosphere, and phosphorus increased at depth. This appears to not be by decomposition but by faster recycling of nutrients.
This article is included in the Encyclopedia of Geosciences
Rodrigo Vargas and Van Huong Le
Biogeosciences, 20, 15–26, https://doi.org/10.5194/bg-20-15-2023, https://doi.org/10.5194/bg-20-15-2023, 2023
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Quantifying the role of soils in nature-based solutions requires accurate estimates of soil greenhouse gas (GHG) fluxes. We suggest that multiple GHG fluxes should not be simultaneously measured at a few fixed time intervals, but an optimized sampling approach can reduce bias and uncertainty. Our results have implications for assessing GHG fluxes from soils and a better understanding of the role of soils in nature-based solutions.
This article is included in the Encyclopedia of Geosciences
Kristine Karstens, Benjamin Leon Bodirsky, Jan Philipp Dietrich, Marta Dondini, Jens Heinke, Matthias Kuhnert, Christoph Müller, Susanne Rolinski, Pete Smith, Isabelle Weindl, Hermann Lotze-Campen, and Alexander Popp
Biogeosciences, 19, 5125–5149, https://doi.org/10.5194/bg-19-5125-2022, https://doi.org/10.5194/bg-19-5125-2022, 2022
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Soil organic carbon (SOC) has been depleted by anthropogenic land cover change and agricultural management. While SOC models often simulate detailed biochemical processes, the management decisions are still little investigated at the global scale. We estimate that soils have lost around 26 GtC relative to a counterfactual natural state in 1975. Yet, since 1975, SOC has been increasing again by 4 GtC due to a higher productivity, recycling of crop residues and manure, and no-tillage practices.
This article is included in the Encyclopedia of Geosciences
Petri Kiuru, Marjo Palviainen, Arianna Marchionne, Tiia Grönholm, Maarit Raivonen, Lukas Kohl, and Annamari Laurén
Biogeosciences, 19, 5041–5058, https://doi.org/10.5194/bg-19-5041-2022, https://doi.org/10.5194/bg-19-5041-2022, 2022
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Peatlands are large carbon stocks. Emissions of carbon dioxide and methane from peatlands may increase due to changes in management and climate. We studied the variation in the gas diffusivity of peat with depth using pore network simulations and laboratory experiments. Gas diffusivity was found to be lower in deeper peat with smaller pores and lower pore connectivity. However, gas diffusivity was not extremely low in wet conditions, which may reflect the distinctive structure of peat.
This article is included in the Encyclopedia of Geosciences
Rachael Akinyede, Martin Taubert, Marion Schrumpf, Susan Trumbore, and Kirsten Küsel
Biogeosciences, 19, 4011–4028, https://doi.org/10.5194/bg-19-4011-2022, https://doi.org/10.5194/bg-19-4011-2022, 2022
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Soils will likely become warmer in the future, and this can increase the release of carbon dioxide (CO2) into the atmosphere. As microbes can take up soil CO2 and prevent further escape into the atmosphere, this study compares the rate of uptake and release of CO2 at two different temperatures. With warming, the rate of CO2 uptake increases less than the rate of release, indicating that the capacity to modulate soil CO2 release into the atmosphere will decrease under future warming.
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Giuseppe Cipolla, Salvatore Calabrese, Amilcare Porporato, and Leonardo V. Noto
Biogeosciences, 19, 3877–3896, https://doi.org/10.5194/bg-19-3877-2022, https://doi.org/10.5194/bg-19-3877-2022, 2022
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Enhanced weathering (EW) is a promising strategy for carbon sequestration. Since models may help to characterize field EW, the present work applies a hydro-biogeochemical model to four case studies characterized by different rainfall seasonality, vegetation and soil type. Rainfall seasonality strongly affects EW dynamics, but low carbon sequestration suggests that an in-depth analysis at the global scale is required to see if EW may be effective to mitigate climate change.
This article is included in the Encyclopedia of Geosciences
Vao Fenotiana Razanamahandry, Marjolein Dewaele, Gerard Govers, Liesa Brosens, Benjamin Campforts, Liesbet Jacobs, Tantely Razafimbelo, Tovonarivo Rafolisy, and Steven Bouillon
Biogeosciences, 19, 3825–3841, https://doi.org/10.5194/bg-19-3825-2022, https://doi.org/10.5194/bg-19-3825-2022, 2022
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In order to shed light on possible past vegetation shifts in the Central Highlands of Madagascar, we measured stable isotope ratios of organic carbon in soil profiles along both forested and grassland hillslope transects in the Lake Alaotra region. Our results show that the landscape of this region was more forested in the past: soils in the C4-dominated grasslands contained a substantial fraction of C3-derived carbon, increasing with depth.
This article is included in the Encyclopedia of Geosciences
Katherine E. O. Todd-Brown, Rose Z. Abramoff, Jeffrey Beem-Miller, Hava K. Blair, Stevan Earl, Kristen J. Frederick, Daniel R. Fuka, Mario Guevara Santamaria, Jennifer W. Harden, Katherine Heckman, Lillian J. Heran, James R. Holmquist, Alison M. Hoyt, David H. Klinges, David S. LeBauer, Avni Malhotra, Shelby C. McClelland, Lucas E. Nave, Katherine S. Rocci, Sean M. Schaeffer, Shane Stoner, Natasja van Gestel, Sophie F. von Fromm, and Marisa L. Younger
Biogeosciences, 19, 3505–3522, https://doi.org/10.5194/bg-19-3505-2022, https://doi.org/10.5194/bg-19-3505-2022, 2022
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Research data are becoming increasingly available online with tantalizing possibilities for reanalysis. However harmonizing data from different sources remains challenging. Using the soils community as an example, we walked through the various strategies that researchers currently use to integrate datasets for reanalysis. We find that manual data transcription is still extremely common and that there is a critical need for community-supported informatics tools like vocabularies and ontologies.
This article is included in the Encyclopedia of Geosciences
Alessandro Montemagno, Christophe Hissler, Victor Bense, Adriaan J. Teuling, Johanna Ziebel, and Laurent Pfister
Biogeosciences, 19, 3111–3129, https://doi.org/10.5194/bg-19-3111-2022, https://doi.org/10.5194/bg-19-3111-2022, 2022
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We investigated the biogeochemical processes that dominate the release and retention of elements (nutrients and potentially toxic elements) during litter degradation. Our results show that toxic elements are retained in the litter, while nutrients are released in solution during the first stages of degradation. This seems linked to the capability of trees to distribute the elements between degradation-resistant and non-degradation-resistant compounds of leaves according to their chemical nature.
This article is included in the Encyclopedia of Geosciences
Laura Sereni, Bertrand Guenet, Charlotte Blasi, Olivier Crouzet, Jean-Christophe Lata, and Isabelle Lamy
Biogeosciences, 19, 2953–2968, https://doi.org/10.5194/bg-19-2953-2022, https://doi.org/10.5194/bg-19-2953-2022, 2022
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This study focused on the modellisation of two important drivers of soil greenhouse gas emissions: soil contamination and soil moisture change. The aim was to include a Cu function in the soil biogeochemical model DNDC for different soil moisture conditions and then to estimate variation in N2O, NO2 or NOx emissions. Our results show a larger effect of Cu on N2 and N2O emissions than on the other nitrogen species and a higher effect for the soils incubated under constant constant moisture.
This article is included in the Encyclopedia of Geosciences
Marie Spohn and Johan Stendahl
Biogeosciences, 19, 2171–2186, https://doi.org/10.5194/bg-19-2171-2022, https://doi.org/10.5194/bg-19-2171-2022, 2022
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We explored the ratios of carbon (C), nitrogen (N), and phosphorus (P) of organic matter in Swedish forest soils. The N : P ratio of the organic layer was most strongly related to the mean annual temperature, while the C : N ratios of the organic layer and mineral soil were strongly related to tree species even in the subsoil. The organic P concentration in the mineral soil was strongly affected by soil texture, which diminished the effect of tree species on the C to organic P (C : OP) ratio.
This article is included in the Encyclopedia of Geosciences
Moritz Mainka, Laura Summerauer, Daniel Wasner, Gina Garland, Marco Griepentrog, Asmeret Asefaw Berhe, and Sebastian Doetterl
Biogeosciences, 19, 1675–1689, https://doi.org/10.5194/bg-19-1675-2022, https://doi.org/10.5194/bg-19-1675-2022, 2022
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The largest share of terrestrial carbon is stored in soils, making them highly relevant as regards global change. Yet, the mechanisms governing soil carbon stabilization are not well understood. The present study contributes to a better understanding of these processes. We show that qualitative changes in soil organic matter (SOM) co-vary with alterations of the soil matrix following soil weathering. Hence, the type of SOM that is stabilized in soils might change as soils develop.
This article is included in the Encyclopedia of Geosciences
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
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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.
This article is included in the Encyclopedia of Geosciences
Karis J. McFarlane, Heather M. Throckmorton, Jeffrey M. Heikoop, Brent D. Newman, Alexandra L. Hedgpeth, Marisa N. Repasch, Thomas P. Guilderson, and Cathy J. Wilson
Biogeosciences, 19, 1211–1223, https://doi.org/10.5194/bg-19-1211-2022, https://doi.org/10.5194/bg-19-1211-2022, 2022
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Planetary warming is increasing seasonal thaw of permafrost, making this extensive old carbon stock vulnerable. In northern Alaska, we found more and older dissolved organic carbon in small drainages later in summer as more permafrost was exposed by deepening thaw. Younger and older carbon did not differ in chemical indicators related to biological lability suggesting this carbon can cycle through aquatic systems and contribute to greenhouse gas emissions as warming increases permafrost thaw.
This article is included in the Encyclopedia of Geosciences
Pengzhi Zhao, Daniel Joseph Fallu, Sara Cucchiaro, Paolo Tarolli, Clive Waddington, David Cockcroft, Lisa Snape, Andreas Lang, Sebastian Doetterl, Antony G. Brown, and Kristof Van Oost
Biogeosciences, 18, 6301–6312, https://doi.org/10.5194/bg-18-6301-2021, https://doi.org/10.5194/bg-18-6301-2021, 2021
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We investigate the factors controlling the soil organic carbon (SOC) stability and temperature sensitivity of abandoned prehistoric agricultural terrace soils. Results suggest that the burial of former topsoil due to terracing provided an SOC stabilization mechanism. Both the soil C : N ratio and SOC mineral protection regulate soil SOC temperature sensitivity. However, which mechanism predominantly controls SOC temperature sensitivity depends on the age of the buried terrace soils.
This article is included in the Encyclopedia of Geosciences
Heleen Deroo, Masuda Akter, Samuel Bodé, Orly Mendoza, Haichao Li, Pascal Boeckx, and Steven Sleutel
Biogeosciences, 18, 5035–5051, https://doi.org/10.5194/bg-18-5035-2021, https://doi.org/10.5194/bg-18-5035-2021, 2021
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We assessed if and how incorporation of exogenous organic carbon (OC) such as straw could affect decomposition of native soil organic carbon (SOC) under different irrigation regimes. Addition of exogenous OC promoted dissolution of native SOC, partly because of increased Fe reduction, leading to more net release of Fe-bound SOC. Yet, there was no proportionate priming of SOC-derived DOC mineralisation. Water-saving irrigation can retard both priming of SOC dissolution and mineralisation.
This article is included in the Encyclopedia of Geosciences
Frances A. Podrebarac, Sharon A. Billings, Kate A. Edwards, Jérôme Laganière, Matthew J. Norwood, and Susan E. Ziegler
Biogeosciences, 18, 4755–4772, https://doi.org/10.5194/bg-18-4755-2021, https://doi.org/10.5194/bg-18-4755-2021, 2021
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Soil respiration is a large and temperature-responsive flux in the global carbon cycle. We found increases in microbial use of easy to degrade substrates enhanced the temperature response of respiration in soils layered as they are in situ. This enhanced response is consistent with soil composition differences in warm relative to cold climate forests. These results highlight the importance of the intact nature of soils rarely studied in regulating responses of CO2 fluxes to changing temperature.
This article is included in the Encyclopedia of Geosciences
Elisa Bruni, Bertrand Guenet, Yuanyuan Huang, Hugues Clivot, Iñigo Virto, Roberta Farina, Thomas Kätterer, Philippe Ciais, Manuel Martin, and Claire Chenu
Biogeosciences, 18, 3981–4004, https://doi.org/10.5194/bg-18-3981-2021, https://doi.org/10.5194/bg-18-3981-2021, 2021
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Increasing soil organic carbon (SOC) stocks is beneficial for climate change mitigation and food security. One way to enhance SOC stocks is to increase carbon input to the soil. We estimate the amount of carbon input required to reach a 4 % annual increase in SOC stocks in 14 long-term agricultural experiments around Europe. We found that annual carbon input should increase by 43 % under current temperature conditions, by 54 % for a 1 °C warming scenario and by 120 % for a 5 °C warming scenario.
This article is included in the Encyclopedia of Geosciences
Rainer Brumme, Bernd Ahrends, Joachim Block, Christoph Schulz, Henning Meesenburg, Uwe Klinck, Markus Wagner, and Partap K. Khanna
Biogeosciences, 18, 3763–3779, https://doi.org/10.5194/bg-18-3763-2021, https://doi.org/10.5194/bg-18-3763-2021, 2021
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In order to study the fate of litter nitrogen in forest soils, we combined a leaf litterfall exchange experiment using 15N-labeled leaf litter with long-term element budgets at seven European beech sites in Germany. It appears that fructification intensity, which has increased in recent decades, has a distinct impact on N retention in forest soils. Despite reduced nitrogen deposition, about 6 and 10 kg ha−1 of nitrogen were retained annually in the soils and in the forest stands, respectively.
This article is included in the Encyclopedia of Geosciences
Lorenz Gfeller, Andrea Weber, Isabelle Worms, Vera I. Slaveykova, and Adrien Mestrot
Biogeosciences, 18, 3445–3465, https://doi.org/10.5194/bg-18-3445-2021, https://doi.org/10.5194/bg-18-3445-2021, 2021
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Our incubation experiment shows that flooding of polluted floodplain soils may induce pulses of both mercury (Hg) and methylmercury to the soil solution and threaten downstream ecosystems. We demonstrate that mobilization of Hg bound to manganese oxides is a relevant process in organic-matter-poor soils. Addition of organic amendments accelerates this mobilization but also facilitates the formation of nanoparticulate Hg and the subsequent fixation of Hg from soil solution to the soil.
This article is included in the Encyclopedia of Geosciences
Yao Zhang, Jocelyn M. Lavallee, Andy D. Robertson, Rebecca Even, Stephen M. Ogle, Keith Paustian, and M. Francesca Cotrufo
Biogeosciences, 18, 3147–3171, https://doi.org/10.5194/bg-18-3147-2021, https://doi.org/10.5194/bg-18-3147-2021, 2021
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Soil organic matter (SOM) is essential for the health of soils, and the accumulation of SOM helps removal of CO2 from the atmosphere. Here we present the result of the continued development of a mathematical model that simulates SOM and its measurable fractions. In this study, we simulated several grassland sites in the US, and the model generally captured the carbon and nitrogen amounts in SOM and their distribution between the measurable fractions throughout the entire soil profile.
This article is included in the Encyclopedia of Geosciences
Zhongkui Luo, Raphael A. Viscarra-Rossel, and Tian Qian
Biogeosciences, 18, 2063–2073, https://doi.org/10.5194/bg-18-2063-2021, https://doi.org/10.5194/bg-18-2063-2021, 2021
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Using the data from 141 584 whole-soil profiles across the globe, we disentangled the relative importance of biotic, climatic and edaphic variables in controlling global SOC stocks. The results suggested that soil properties and climate contributed similarly to the explained global variance of SOC in four sequential soil layers down to 2 m. However, the most important individual controls are consistently soil-related, challenging current climate-driven framework of SOC dynamics.
This article is included in the Encyclopedia of Geosciences
Debjani Sihi, Xiaofeng Xu, Mónica Salazar Ortiz, Christine S. O'Connell, Whendee L. Silver, Carla López-Lloreda, Julia M. Brenner, Ryan K. Quinn, Jana R. Phillips, Brent D. Newman, and Melanie A. Mayes
Biogeosciences, 18, 1769–1786, https://doi.org/10.5194/bg-18-1769-2021, https://doi.org/10.5194/bg-18-1769-2021, 2021
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Humid tropical soils are important sources and sinks of methane. We used model simulation to understand how different kinds of microbes and observed soil moisture and oxygen dynamics contribute to production and consumption of methane along a wet tropical hillslope during normal and drought conditions. Drought alters the diffusion of oxygen and microbial substrates into and out of soil microsites, resulting in enhanced methane release from the entire hillslope during drought recovery.
This article is included in the Encyclopedia of Geosciences
Mathieu Chassé, Suzanne Lutfalla, Lauric Cécillon, François Baudin, Samuel Abiven, Claire Chenu, and Pierre Barré
Biogeosciences, 18, 1703–1718, https://doi.org/10.5194/bg-18-1703-2021, https://doi.org/10.5194/bg-18-1703-2021, 2021
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Evolution of organic carbon content in soils could be a major driver of atmospheric greenhouse gas concentrations over the next century. Understanding factors controlling carbon persistence in soil is a challenge. Our study of unique long-term bare-fallow samples, depleted in labile organic carbon, helps improve the separation, evaluation and characterization of carbon pools with distinct residence time in soils and gives insight into the mechanisms explaining soil organic carbon persistence.
This article is included in the Encyclopedia of Geosciences
Melisa A. Diaz, Christopher B. Gardner, Susan A. Welch, W. Andrew Jackson, Byron J. Adams, Diana H. Wall, Ian D. Hogg, Noah Fierer, and W. Berry Lyons
Biogeosciences, 18, 1629–1644, https://doi.org/10.5194/bg-18-1629-2021, https://doi.org/10.5194/bg-18-1629-2021, 2021
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Water-soluble salt and nutrient concentrations of soils collected along the Shackleton Glacier, Antarctica, show distinct geochemical gradients related to latitude, longitude, elevation, soil moisture, and distance from coast and glacier. Machine learning algorithms were used to estimate geochemical gradients for the region given the relationship with geography. Geography and surface exposure age drive salt and nutrient abundances, influencing invertebrate habitat suitability and biogeography.
This article is included in the Encyclopedia of Geosciences
Marion Schrumpf, Klaus Kaiser, Allegra Mayer, Günter Hempel, and Susan Trumbore
Biogeosciences, 18, 1241–1257, https://doi.org/10.5194/bg-18-1241-2021, https://doi.org/10.5194/bg-18-1241-2021, 2021
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A large amount of organic carbon (OC) in soil is protected against decay by bonding to minerals. We studied the release of mineral-bonded OC by NaF–NaOH extraction and H2O2 oxidation. Unexpectedly, extraction and oxidation removed mineral-bonded OC at roughly constant portions and of similar age distributions, irrespective of mineral composition, land use, and soil depth. The results suggest uniform modes of interactions between OC and minerals across soils in quasi-steady state with inputs.
This article is included in the Encyclopedia of Geosciences
Lena Rohe, Bernd Apelt, Hans-Jörg Vogel, Reinhard Well, Gi-Mick Wu, and Steffen Schlüter
Biogeosciences, 18, 1185–1201, https://doi.org/10.5194/bg-18-1185-2021, https://doi.org/10.5194/bg-18-1185-2021, 2021
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Total denitrification, i.e. N2O and (N2O + N2) fluxes, of repacked soil cores were analysed for different combinations of soils and water contents. Prediction accuracy of (N2O + N2) fluxes was highest with combined proxies for oxygen demand (CO2 flux) and oxygen supply (anaerobic soil volume fraction). Knowledge of denitrification completeness (product ratio) improved N2O predictions. Substitutions with cheaper proxies (soil organic matter, empirical diffusivity) reduced prediction accuracy.
This article is included in the Encyclopedia of Geosciences
Severin-Luca Bellè, Asmeret Asefaw Berhe, Frank Hagedorn, Cristina Santin, Marcus Schiedung, Ilja van Meerveld, and Samuel Abiven
Biogeosciences, 18, 1105–1126, https://doi.org/10.5194/bg-18-1105-2021, https://doi.org/10.5194/bg-18-1105-2021, 2021
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Controls of pyrogenic carbon (PyC) redistribution under rainfall are largely unknown. However, PyC mobility can be substantial after initial rain in post-fire landscapes. We conducted a controlled simulation experiment on plots where PyC was applied on the soil surface. We identified redistribution of PyC by runoff and splash and vertical movement in the soil depending on soil texture and PyC characteristics (material and size). PyC also induced changes in exports of native soil organic carbon.
This article is included in the Encyclopedia of Geosciences
Cited articles
Afshar, E., Yarnia, M., Bagherzadeh, A., Mirshekari, B., and Haghighi, R. S.:
The Effect of Crops Cultivation on Soil Erosion Indices Based on Impelero
Model in Northeast Iran, Appl. Ecol. Environ. Res., 16, 855–866,
https://doi.org/10.15666/aeer/1601_855866, 2018.
Alletto, L. and Coquet, Y.: Temporal and spatial variability of soil bulk
density and near-saturated hydraulic conductivity under two contrasted
tillage management systems, Geoderma, 152, 85–94,
https://doi.org/10.1016/j.geoderma.2009.05.023, 2009.
Amundson, R. and Jenny, H.: The Place of Humans in the State Factor Theory
of Ecosystems and Their Soils, Soil Sci., 151, 99–109, 1991.
Andrews, S. S., Karlen, D. L., and Mitchell, J. P.: A comparison of soil
quality indexing methods for vegetable production systems in Northern
California, Agric. Ecosyst. Environ., 90, 25–45,
https://doi.org/10.1016/S0167-8809(01)00174-8, 2002.
Andrews, S. S., Flora, C. B., Mitchell, J. P., and Karlen, D. L.: Growers'
perceptions and acceptance of soil quality indices, Geoderma, 114,
187–213, https://doi.org/10.1016/S0016-7061(03)00041-7, 2003.
Arekhi, S., Niazi, Y., and Kalteh, A. M.: Soil erosion and sediment yield
modeling using RS and GIS techniques: a case study, Iran, Arab. J. Geosci.,
5, 285–296, https://doi.org/10.1007/s12517-010-0220-4, 2012.
Askari, M. S. and Holden, N. M.: Quantitative soil quality indexing of
temperate arable management systems, Soil Tillage Res., 150,
57–67, https://doi.org/10.1016/j.still.2015.01.010, 2015.
Ayoubi, S., Mokhtari Karchegani, P., Mosaddeghi, M. R., and Honarjoo, N.:
Soil aggregation and organic carbon as affected by topography and land use
change in western Iran, Soil Tillage Res., 121, 18–26,
https://doi.org/10.1016/j.still.2012.01.011, 2012.
Bidwell, O. W. and Hole, F. D.: Man as a factor of soil formation, Soil
Sci., 99, 65–72, 1965.
Boix-Fayos, C., Calvo-Cases, A., Imeson, A. C., and Soriano-Soto, M. D.:
Influence of soil properties on the aggregation of some Mediterranean soils
and the use of aggregate size and stability as land degradation indicators,
Catena, 44, 47–67, https://doi.org/10.1016/S0341-8162(00)00176-4, 2001.
Bosch-Serra, A. D., Padro, R., Boixadera-Bosch, R. R., Orobitg, J., and
Yaguee, M. R.: Tillage and slurry over-fertilization affect oribatid mite
communities in a semiarid Mediterranean environment, Appl. Soil Ecol., 84,
124–139, https://doi.org/10.1016/j.apsoil.2014.06.010, 2014.
Breland, T. A. and Eltun, R.: Soil microbial biomass and mineralization of
carbon and nitrogen in ecological, integrated and conventional forage and
arable cropping systems, Biol. Fertil. Soils, 30, 193–201,
https://doi.org/10.1007/s003740050608, 1999.
Bryant, R. B. and Galbraith, J. M.: Incorporating Anthropogenic Processes in
Soil Classification, in: Soil Classification: A Global Desk Reference, edited
by: Eswaran, H., Ahrens, R., Rice, T. J., and Stewart, B. A., CRC Press, Boca
Raton, FL, 2003.
Bünemann, E. K., Bongiorno, G., Bai, Z., Creamer, R. E., De Deyn, G., de
Goede, R., Fleskens, L., Geissen, V., Kuyper, T. W., Mäder, P.,
Pulleman, M., Sukkel, W., van Groenigen, J. W., and Brussaard, L.: Soil
quality – A critical review, Soil Biol. Biochem., 120, 105–125,
https://doi.org/10.1016/j.soilbio.2018.01.030, 2018.
Burghardt, W., Heintz, D., and Hocke, N.: Soil Fertility Characteristics and
Organic Carbon Stock in Soils of Vegetable Gardens Compared with Surrounding
Arable Land at the Center of the Urban and Industrial Area of Ruhr, Germany,
Eurasian Soil Sci., 51, 1067–1079, https://doi.org/10.1134/S106422931809003X, 2018.
Cannell, R. Q. and Hawes, J. D.: Trends in tillage practices in relation to
sustainable crop production with special reference to temperate climates,
Soil Tillage Res., 30, 245–282, https://doi.org/10.1016/0167-1987(94)90007-8, 1994.
Carducci, C. E., Zinn, Y. L., Rossoni, D. F., Heck, R. J., and Oliveira, G.
C.: Visual analysis and X-ray computed tomography for assessing the spatial
variability of soil structure in a cultivated Oxisol, Soil Tillage Res.,
173, 15–23, https://doi.org/10.1016/j.still.2016.03.006, 2017.
Carozza, J.-M., Galop, D., Metailie, J.-P., Vanniere, B., Bossuet, G.,
Monna, F., Lopez-Saez, J. A., Arnauld, M.-C., Breuil, V., Forne, M., and
Lemonnier, E.: Landuse and soil degradation in the southern Maya lowlands,
from Pre-Classic to Post-Classic times: The case of La Joyanca (Petén,
Guatemala), Geodin. Acta, 20, 195–207, https://doi.org/10.3166/ga.20.195-207, 2007.
Celik, I.: Land-use effects on organic matter and physical properties of
soil in a southern Mediterranean highland of Turkey, Soil Tillage Res.,
83, 270–277, https://doi.org/10.1016/j.still.2004.08.001, 2005.
Chadwick, O. A. and Chorover, J.: The chemistry of pedogenic thresholds,
Geoderma, 100, 321–353, https://doi.org/10.1016/S0016-7061(01)00027-1, 2001.
Chen, L.-M., Zhang, G.-L., and Effland, W. R.: Soil Characteristic Response
Times and Pedogenic Thresholds during the 1000-Year Evolution of a Paddy
Soil Chronosequence, Soil Sci. Soc. Am. J., 75, 1807–1820,
https://doi.org/10.2136/sssaj2011.0006, 2011.
Cheng, Y.-Q., Yang, L.-Z., Cao, Z.-H., Ci, E., and Yin, S.: Chronosequential
changes of selected pedogenic properties in paddy soils as compared with
non-paddy soils, Geoderma, 151, 31–41,
https://doi.org/10.1016/j.geoderma.2009.03.016, 2009.
Chertov, O. G. and Komarov, A. S.: SOMM: A model of soil organic matter
dynamics, Ecol. Model., 94, 177–189,
https://doi.org/10.1016/S0304-3800(96)00017-8, 1997.
Dalal, R. and Mayer, J. R.: Long term trends in fertility of soils under
continuous cultivation and cereal cropping in southern Queensland. II. Total
organic carbon and its rate of loss from the soil profile, Aust. J. Soil
Res., 24, 281–292, https://doi.org/10.1071/SR9860281, 1986a.
Dalal, R. and Mayer, R.: Long-term trends in fertility of soils under
continuous cultivation and cereal cropping in southern Queensland. IV. Loss
of organic carbon for different density functions, Aust. J. Soil Res., 24, 281–292, https://doi.org/10.1071/SR9860301, 1986b.
Dalal, R. C. and Mayer, R. J.: Long term trends in fertility of soils under
continuous cultivation and cereal cropping in southern Queensland .V. Rate
of loss of total nitrogen from the soil profile and changes in carbon?:
nitrogen ratios, Aust. J. Soil Res., 24, 493–504, https://doi.org/10.1071/sr9860493, 1986c.
Davidson, E. A., Samanta, S., Caramori, S. S., and Savage, K.: The Dual
Arrhenius and Michaelis-Menten kinetics model for decomposition of soil
organic matter at hourly to seasonal time scales, Glob. Change Biol., 18,
371–384, https://doi.org/10.1111/j.1365-2486.2011.02546.x, 2012.
Dazzi, C. and Monteleone, S.: Anthropogenic processes in the evolution of a
soil chronosequence on marly-limestone substrata in an Italian Mediterranean
environment, Geoderma, 141, 201–209, https://doi.org/10.1016/j.geoderma.2007.05.016,
2007.
Dehaan, R. L. and Taylor, G. R.: Field-derived spectra of salinized soils
and vegetation as indicators of irrigation-induced soil salinization, Remote
Sens. Environ., 80, 406–417, https://doi.org/10.1016/S0034-4257(01)00321-2, 2002.
Del Grosso, S., Ojima, D., Parton, W., Mosier, A., Peterson, G., and Schimel,
D.: Simulated effects of dryland cropping intensification on soil organic
matter and greenhouse gas exchanges using the DAYCENT ecosystem model,
Environ. Pollut., 116, S75–S83, https://doi.org/10.1016/S0269-7491(01)00260-3, 2002.
DeLong, C., Cruse, R., and Wiener, J.: The Soil Degradation Paradox:
Compromising Our Resources When We Need Them the Most, Sustainability, 7,
866–879, https://doi.org/10.3390/su7010866, 2015.
Denef, K., Stewart, C. E., Brenner, J., and Paustian, K.: Does long-term
center-pivot irrigation increase soil carbon stocks in semi-arid
agro-ecosystems?, Geoderma, 145, 121–129,
https://doi.org/10.1016/j.geoderma.2008.03.002, 2008.
Diamond, J.: Evolution, consequences and future of plant and animal
domestication, Nature, 418, 700–707, https://doi.org/10.1038/nature01019, 2002.
Dick, R. P., Sandor, J. A., and Eash, N. S.: Soil enzyme activities after
1500 years of terrace agriculture in the Colca Valley, Peru, Agric. Ecosyst.
Environ., 50, 123–131, https://doi.org/10.1016/0167-8809(94)90131-7, 1994.
Diedhiou, A. G., Dupouey, J.-L., Buée, M., Dambrine, E., Laüt, L.,
and Garbaye, J.: Response of ectomycorrhizal communities to past Roman
occupation in an oak forest, Soil Biol. Biochem., 41, 2206–2213,
https://doi.org/10.1016/j.soilbio.2009.08.005, 2009.
Dokuchaev, V.: Russian Chernozem, Saint Petersburg, 1883.
Dudal, R.: The sixth factor of soil formation, available at:
https://www.researchgate.net/publication/228669778_The_sixth_factor_of_soil_formation (last access: 5 October 2018),
2004.
Ebrahimzadeh, S., Motagh, M., Mahboub, V., and Harijani, F. M.: An improved
RUSLE/SDR model for the evaluation of soil erosion, Environ. Earth Sci.,
77, 454, https://doi.org/10.1007/s12665-018-7635-8, 2018.
Eleftheriadis, A., Lafuente, F., and Turrión, M.-B.: Effect of land use,
time since deforestation and management on organic C and N in soil textural
fractions, Soil Tillage Res., 183, 1–7, https://doi.org/10.1016/j.still.2018.05.012,
2018.
Ellis, S. and Newsome, D.: Chalkland soil formation and erosion on the
Yorkshire Wolds, northern England, Geoderma, 48, 59–72,
https://doi.org/10.1016/0016-7061(91)90006-F, 1991.
Emdad, M. R., Raine, S. R., Smith, R. J., and Fardad, H.: Effect of water
quality on soil structure and infiltration under furrow irrigation, Irrig.
Sci., 23, 55–60, https://doi.org/10.1007/s00271-004-0093-y, 2004.
Fageria, N. K.: Role of Soil Organic Matter in Maintaining Sustainability of
Cropping Systems, Commun. Soil Sci. Plant Anal., 43, 2063–2113,
https://doi.org/10.1080/00103624.2012.697234, 2012.
FAO: World Food and Agriculture: Statistical Pocketbook, FAO, Rome, 2018.
Finke, P. A.: Modeling the genesis of luvisols as a function of topographic
position in loess parent material, Quat. Int., 265, 3–17,
https://doi.org/10.1016/j.quaint.2011.10.016, 2012.
Finke, P. A. and Hutson, J. L.: Modelling soil genesis in calcareous loess,
Geoderma, 145, 462–479, https://doi.org/10.1016/j.geoderma.2008.01.017, 2008.
Flynn, D. F. B., Gogol-Prokurat, M., Nogeire, T., Molinari, N., Richers, B.
T., Lin, B. B., Simpson, N., Mayfield, M. M., and DeClerck, F.: Loss of
functional diversity under land use intensification across multiple taxa,
Ecol. Lett., 12, 22–33, https://doi.org/10.1111/j.1461-0248.2008.01255.x, 2009.
Francis, G. S. and Knight, T. L.: Long-term effects of conventional and
no-tillage on selected soil properties and crop yields in Canterbury, New
Zealand, Soil Tillage Res., 26, 193–210,
https://doi.org/10.1016/0167-1987(93)90044-P, 1993.
Gerasimov, I.: The System of Basic Genetic Concepts That Should Be Included
in Modern Dokuchayevian Soil Science, Sov. Geogr., 25, 1–14, 1984.
Gerasimov, I. P. and Fridland, V.: Historical role and current problems of
genetical soil science of Dokuchaev, Pochvovedenie, 4, 5–10, 1984.
Gharahi Ghehi, N., Nemes, A., Verdoodt, A., Van Ranst, E., Cornelis, W., and
Boeckx, P.: Nonparametric techniques for predicting soil bulk density of
tropical rainforest topsoils in Rwanda, Soil Sci. Soc. Am. J., 76,
1172–1183, https://doi.org/10.2136/sssaj2011.0330, 2012.
Glaser, B., Haumaier, L., Guggenberger, G., and Zech, W.: The “Terra Preta”
phenomenon: a model for sustainable agriculture in the humid tropics,
Naturwissenschaften, 88, 37–41, https://doi.org/10.1007/s001140000193, 2001.
Glinka, K. D.: Dokuchaiev's ideas in the development of pedology and cognate
sciences, The Academy, Leningrad, 1927.
Govers, G., Vandaele, K., Desmet, P., Poesen, J., and Bunte, K.: The Role of
Tillage in Soil Redistribution on Hillslopes, Eur. J. Soil Sci., 45,
469–478, https://doi.org/10.1111/j.1365-2389.1994.tb00532.x, 1994.
Grant, R. F.: Changes in soil organic matter under different tillage and
rotation: Mathematical modeling in ecosys, Soil Sci. Soc. Am. J., 61,
1159–1175, https://doi.org/10.2136/sssaj1997.03615995006100040023x, 1997.
Guillaume, T., Holtkamp, A. M., Damris, M., Brummer, B., and Kuzyakov, Y.:
Soil degradation in oil palm and rubber plantations under land resource
scarcity, Agric. Ecosyst. Environ., 232, 110–118,
https://doi.org/10.1016/j.agee.2016.07.002, 2016a.
Guillaume, T., Maranguit, D., Murtilaksono, K., and Kuzyakov, Y.: Sensitivity
and resistance of soil fertility indicators to land-use changes: New concept
and examples from conversion of Indonesian rainforest to plantations, Ecol.
Indic., 67, 49–57, https://doi.org/10.1016/j.ecolind.2016.02.039, 2016b.
Haas, H. J., Evans, C. E., and Miles, E. F.: Nitrogen and Carbon Changes in
Great Plains Soils as Influenced by Cropping and Soil Treatments, U.S.
Department of Agriculture, Washington D.C., 1957.
Hall, S. J., Trujillo, J., Nakase, D., Strawhacker, C., Kruse-Peeples, M.,
Schaafsma, H., and Briggs, J.: Legacies of Prehistoric Agricultural Practices
Within Plant and Soil Properties Across an Arid Ecosystem, Ecosystems,
16, 1273–1293, https://doi.org/10.1007/s10021-013-9681-0, 2013.
Hartemink, A. E.: Assessing Soil Fertility Decline in the Tropics Using Soil
Chemical Data, Advances in Agronomy, 89, 179–225, 2006.
Hartemink, A. E. and Bridges, E. M.: The influence of parent material on
soil fertility degradation in the coastal plain of Tanzania, Land Degrad.
Dev., 6, 215–221, https://doi.org/10.1002/ldr.3400060403, 1995.
Henrot, J. and Robertson, G. P.: Vegetation removal in two soils of the
humid tropics: Effect on microbial biomass, Soil Biol. Biochem., 26,
111–116, https://doi.org/10.1016/0038-0717(94)90202-X, 1994.
Hernanz, J. L., Peixoto, H., Cerisola, C., and Sanchez-Giron, V.: An
empirical model to predict soil bulk density profiles in field conditions
using penetration resistance, moisture content and soil depth, J.
Terramechanics, 37, 167–184, https://doi.org/10.1016/S0022-4898(99)00020-8, 2000.
Holthusen, D., Brandt, A. A., Reichert, J. M., and Horn, R.: Soil porosity,
permeability and static and dynamic strength parameters under native
forest/grassland compared to no-tillage cropping, Soil Tillage Res., 177,
113–124, https://doi.org/10.1016/j.still.2017.12.003, 2018.
Homburg, J. A. and Sandor, J. A.: Anthropogenic effects on soil quality of
ancient agricultural systems of the American Southwest, Catena, 85,
144–154, https://doi.org/10.1016/j.catena.2010.08.005, 2011.
Homburg, J. A., Sandor, J. A., and Norton, J. B.: Anthropogenic influences on
Zuni agricultural soils, Geoarchaeology Int. J., 20, 661–693,
https://doi.org/10.1002/gea.20076, 2005.
Horn, R. and Fleige, H.: Risk assessment of subsoil compaction for arable
soils in Northwest Germany at farm scale, Soil Tillage Res., 102,
201–208, https://doi.org/10.1016/j.still.2008.07.015, 2009.
Howard, J.: Anthropogenic Soils, Springer International Publishing, available at: https://www.springer.com/de/book/9783319543307 (last access: 22 April 2019), 2017.
Jalabert, S. S. M., Martin, M. P., Renaud, J.-P., Boulonne, L., Jolivet, C.,
Montanarella, L., and Arrouays, D.: Estimating forest soil bulk density using
boosted regression modelling, Soil Use Manag., 26, 516–528,
https://doi.org/10.1111/j.1475-2743.2010.00305.x, 2010.
Jalali, M. and Ranjbar, F.: Effects of sodic water on soil sodicity and
nutrient leaching in poultry and sheep manure amended soils, Geoderma,
153, 194–204, https://doi.org/10.1016/j.geoderma.2009.08.004, 2009.
Jangid, K., Williams, M. A., Franzluebbers, A. J., Schmidt, T. M., Coleman,
D. C., and Whitman, W. B.: Land-use history has a stronger impact on soil
microbial community composition than aboveground vegetation and soil
properties, Soil Biol. Biochem., 43, 2184–2193,
https://doi.org/10.1016/j.soilbio.2011.06.022, 2011.
Jenny, H.: Factors of soil formation: a system of quantitative pedology,
McGraw-Hill, New York, 1941.
KA-5: Bodenkundliche Kartieranleitung, 5th ed., Schweizerbart'sche, E.,
Stuttgart, 2005.
Kalinina, O., Chertov, O., Dolgikh, A. V., Goryachkin, S. V., Lyuri, D. I.,
Vormstein, S., and Giani, L.: Self-restoration of post-agrogenic
Albeluvisols: Soil development, carbon stocks and dynamics of carbon pools,
Geoderma, 207–208, 221–233, https://doi.org/10.1016/j.geoderma.2013.05.019, 2013.
Kalinina, O., Cherkinsky, A., Chertov, O., Goryachkin, S., Kurganova, I.,
Lopes de Gerenyu, V., Lyuri, D., Kuzyakov, Y., and Giani, L.:
Post-agricultural restoration: Implications for dynamics of soil organic
matter pools, Catena, 181, 104096, https://doi.org/10.1016/j.catena.2019.104096, 2019.
Karathanasis, A. D. and Wells, K. L.: A Comparison of Mineral Weathering
Trends Between Two Management Systems on a Catena of Loess-Derived Soils,
Soil Sci. Soc. Am. J., 53, 582–588,
https://doi.org/10.2136/sssaj1989.03615995005300020047x, 1989.
KDPR: Klassifikazia i Diagnostika Pochv Rossii (Classification and
Diagnostics of Soil of Russia), edited by: Shishov, L. L., Lebedeva, I. I., Gerasimova, M.
I., and Tonkongov, V. D., Smolensk: Oikumena, available
at: http://infosoil.ru/index.php?pageID=clas04mode (last access: 10 September 2018), 2004.
Keyvanshokouhi, S., Cornu, S., Samouelian, A., and Finke, P.: Evaluating
SoilGen2 as a tool for projecting soil evolution induced by global change,
Sci. Total Environ., 571, 110–123, https://doi.org/10.1016/j.scitotenv.2016.07.119,
2016.
Khormali, F., Ajami, M., Ayoubi, S., Srinivasarao, C., and Wani, S. P.: Role
of deforestation and hillslope position on soil quality attributes of
loess-derived soils in Golestan province, Iran, Agric. Ecosyst. Environ.,
134, 178–189, https://doi.org/10.1016/j.agee.2009.06.017, 2009.
Kölbl, A., Schad, P., Jahn, R., Amelung, W., Bannert, A., Cao, Z. H.,
Fiedler, S., Kalbitz, K., Lehndorff, E., Müller-Niggemann, C., Schloter,
M., Schwark, L., Vogelsang, V., Wissing, L., and Kögel-Knabner, I.:
Accelerated soil formation due to paddy management on marshlands (Zhejiang
Province, China), Geoderma, 228–229, 67–89,
https://doi.org/10.1016/j.geoderma.2013.09.005, 2014.
Kozlovskii, F. I.: The Modeling of Agropedogenesis in Plowed Soils on Mantle
Loams, Eurasian Soil Sci. CC Pochvovedenie, 32, 710–720, 1999.
Kozlovskii, F. I. and Goryachkin, S. V.: Soil as a mirror of landscape and the concept on informational structure of soil cover, Eur. Soil Sci., 29, 255–263, 1996.
Kurganova, I., Merino, A., Lopes de Gerenyu, V., Barros, N., Kalinina, O.,
Giani, L., and Kuzyakov, Y.: Mechanisms of carbon sequestration and
stabilization by restoration of arable soils after abandonment: A
chronosequence study on Phaeozems and Chernozems, Geoderma, 354, 113882,
https://doi.org/10.1016/j.geoderma.2019.113882, 2019.
Lal, R.: Long-term tillage and maize monoculture effects on a tropical
Alfisol in western Nigeria. I. Crop yield and soil physical properties, Soil
Tillage Res., 42, 145–160, https://doi.org/10.1016/S0167-1987(97)00006-8, 1997.
Lal, R.: Soil degradation by erosion, Land Degrad. Dev., 12, 519–539,
https://doi.org/10.1002/ldr.472, 2001.
Lal, R.: Climate change, soil carbon dynamics and global food security, in:
Climate change and global food security, edited by: Lal, R., Stewart, B. A.,
Uphoff, N., and Hansen, D. O., 113–143, CRC Press, Taylor & Francis, Boca Raton, FL,
2005.
Lal, R.: Enhancing crop yields in the developing countries through
restoration of the soil organic carbon pool in agricultural lands, Land
Degrad. Dev., 17, 197–209, https://doi.org/10.1002/ldr.696, 2006.
Lal, R.: Soils and sustainable agriculture. A review, Agron. Sustain. Dev.,
28, 57–64, https://doi.org/10.1051/agro:2007025, 2008.
Lal, R.: Soil degradation as a reason for inadequate human nutrition, Food
Secur., 1, 45–57, https://doi.org/10.1007/s12571-009-0009-z, 2009.
Lal, R.: Restoring Soil Quality to Mitigate Soil Degradation,
Sustainability, 7, 5875–5895, https://doi.org/10.3390/su7055875, 2015.
Lemenih, M., Karltun, E., and Olsson, M.: Assessing soil chemical and
physical property responses to deforestation and subsequent cultivation in
smallholders farming system in Ethiopia, Agric. Ecosyst. Environ., 105,
373–386, https://doi.org/10.1016/j.agee.2004.01.046, 2005.
Lincoln, N., Chadwick, O., and Vitousek, P.: Indicators of soil fertility and
opportunities for precontact agriculture in Kona, Hawai'i, Ecosphere, 5,
42, https://doi.org/10.1890/ES13-00328.1, 2014.
Lipiec, J., Horn, R., Pietrusiewicz, J., and Siczek, A.: Effects of soil
compaction on root elongation and anatomy of different cereal plant species,
Soil Tillage Res., 121, 74–81, https://doi.org/10.1016/j.still.2012.01.013, 2012.
Lisetskii, F., Stolba, V., Ergina, E., Rodionova, M., and Terekhin, E.:
Post-agrogenic evolution of soils in ancient Greek land use areas in the
Herakleian Peninsula, southwestern Crimea, The Holocene, 23, 504-514,
https://doi.org/10.1177/0959683612463098, 2013.
Lisetskii, F., Stolba, V. F., and Marininà, O.: Indicators of agricultural
soil genesis under varying conditions of land use, Steppe Crimea, Geoderma,
239–240, 304–316, https://doi.org/10.1016/j.geoderma.2014.11.006, 2015.
Liu, S. G., Bliss, N., Sundquist, E., and Huntington, T. G.: Modeling carbon
dynamics in vegetation and soil under the impact of soil erosion and
deposition, Glob. Biogeochem. Cycles, 17, 1074, https://doi.org/10.1029/2002GB002010,
2003.
Liu, X., Zhang, W., Zhang, M., Ficklin, D. L., and Wang, F.: Spatio-temporal
variations of soil nutrients influenced by an altered land tenure system in
China, Geoderma, 152, 23–34, https://doi.org/10.1016/j.geoderma.2009.05.022, 2009.
Lobe, I., Amelung, W., and Preez, C. C. D.: Losses of carbon and nitrogen
with prolonged arable cropping from sandy soils of the South African
Highveld, Eur. J. Soil Sci., 52, 93–101,
https://doi.org/10.1046/j.1365-2389.2001.t01-1-00362.x, 2001.
Lo Papa, G., Palermo, V., and Dazzi, C.: Is land-use change a cause of loss
of pedodiversity? The case of the Mazzarrone study area, Sicily,
Geomorphology, 135, 332–342, https://doi.org/10.1016/j.geomorph.2011.02.015, 2011.
Lo Papa, G., Palermo, V., and Dazzi, C.: The “genetic erosion” of the soil
ecosystem, Int. Soil Water Conserv. Res., 1, 11–18,
https://doi.org/10.1016/S2095-6339(15)30045-9, 2013.
Makovnikova, J., Siran, M., Houskova, B., Palka, B., and Jones, A.:
Comparison of different models for predicting soil bulk density. Case study
– Slovakian agricultural soils, Int. Agrophysics, 31, 491–498,
https://doi.org/10.1515/intag-2016-0079, 2017.
Matus F. and Egli M.: Mathematical–statistical problem that has a significant implication
on estimation of interval-specific rates of soil-forming processes, J. Soil Sci. Plant Nutr., in press, https://doi.org/10.1007/s42729-019-00095-y, 2019.
McBratney, A. B., Mendonça Santos, M. L., and Minasny, B.: On digital
soil mapping, Geoderma, 117, 3–52, 2003.
Meuser, H.: Anthropogenic Soils, in: Contaminated Urban Soils, edited by:
Meuser, H., pp. 121–193, Springer Netherlands, Dordrecht, 2010.
Millward, A. A. and Mersey, J. E.: Adapting the RUSLE to model soil erosion
potential in a mountainous tropical watershed, Catena, 38, 109–129,
https://doi.org/10.1016/S0341-8162(99)00067-3, 1999.
Minasny, B. and Hartemink, A. E.: Predicting soil properties in the tropics,
Earth-Sci. Rev., 106, 52–62, https://doi.org/10.1016/j.earscirev.2011.01.005, 2011.
Morgan, R. P. C., Quinton, J. N., Smith, R. E., Govers, G., Poesen, J. W.
A., Auerswald, K., Chisci, G., Torri, D., and Styczen, M. E.: The European
Soil Erosion Model (EUROSEM): A dynamic approach for predicting sediment
transport from fields and small catchments, Earth Surf. Process. Landf.,
23, 527–544, https://doi.org/10.1002/(SICI)1096-9837(199806)23:6<527::AID-ESP868>3.0.CO;2-5, 1998.
Morrison, R. J. and Gawander, J. S.: Changes in the properties of Fijian
Oxisols over 30 years of sugarcane cultivation, Soil Res., 54, 418–429,
https://doi.org/10.1071/SR15173, 2016.
Nabiollahi, K., Taghizadeh-Mehrjardi, R., Kerry, R., and Moradian, S.:
Assessment of soil quality indices for salt-affected agricultural land in
Kurdistan Province, Iran, Ecol. Indic., 83, 482–494,
https://doi.org/10.1016/j.ecolind.2017.08.001, 2017.
Nannipieri, P., Ascher, J., Ceccherini, M. T., Landi, L., Pietramellara, G.,
and Renella, G.: Microbial diversity and soil functions, Eur. J. Soil Sci.,
54, 655–670, https://doi.org/10.1046/j.1351-0754.2003.0556.x, 2003.
Nyberg, G., Bargués Tobella, A., Kinyangi, J., and Ilstedt, U.: Soil property changes over a 120-yr chronosequence from forest to agriculture in western Kenya, Hydrol. Earth Syst. Sci., 16, 2085–2094, https://doi.org/10.5194/hess-16-2085-2012, 2012.
Obour, A. K., Mikha, M. M., Holman, J. D., and Stahlman, P. W.: Changes in
soil surface chemistry after fifty years of tillage and nitrogen
fertilization, Geoderma, 308, 46–53, https://doi.org/10.1016/j.geoderma.2017.08.020,
2017.
Ovsepyan, L., Kurganova, I., de Gerenyu, V. L., and Kuzyakov, Y.: Recovery of
organic matter and microbial biomass after abandonment of degraded
agricultural soils: the influence of climate, Land Degrad. Dev., 30,
1861–1874, https://doi.org/10.1002/ldr.3387, 2019.
Pape, J. C.: Plaggen soils in the Netherlands, Geoderma, 4, 229–255,
https://doi.org/10.1016/0016-7061(70)90005-4, 1970.
Paul, E. A.: Soil Microbiology, Ecology and Biochemistry, Academic Press, London,
2014.
Paz-González, A., Vieira, S. R., and Taboada Castro, M. T.: The effect of
cultivation on the spatial variability of selected properties of an umbric
horizon, Geoderma, 97, 273–292, https://doi.org/10.1016/S0016-7061(00)00066-5, 2000.
Ponge, J.-F., Peres, G., Guernion, M., Ruiz-Camacho, N., Cortet, J., Pernin,
C., Villenave, C., Chaussod, R., Martin-Laurent, F., Bispo, A., and Cluzeau,
D.: The impact of agricultural practices on soil biota: A regional study,
Soil Biol. Biochem., 67, 271–284, https://doi.org/10.1016/j.soilbio.2013.08.026, 2013.
Pournader, M., Ahmadi, H., Feiznia, S., Karimi, H., and Peirovan, H. R.:
Spatial prediction of soil erosion susceptibility: an evaluation of the
maximum entropy model, Earth Sci. Inform., 11, 389–401,
https://doi.org/10.1007/s12145-018-0338-6, 2018.
Raiesi, F.: A minimum data set and soil quality index to quantify the effect
of land use conversion on soil quality and degradation in native rangelands
of upland arid and semiarid regions, Ecol. Indic., 75, 307–320,
https://doi.org/10.1016/j.ecolind.2016.12.049, 2017.
Raiesi, F. and Kabiri, V.: Identification of soil quality indicators for
assessing the effect of different tillage practices through a soil quality
index in a semi-arid environment, Ecol. Indic., 71, 198–207,
https://doi.org/10.1016/j.ecolind.2016.06.061, 2016.
Rasa, K. and Horn, R.: Structure and hydraulic properties of the boreal clay
soil under differently managed buffer zones, Soil Use Manag., 29,
410–418, https://doi.org/10.1111/sum.12043, 2013.
Raty, M., Horn, R., Rasa, K., Yli-Halla, M., and Pietola, L.: Compressive
behaviour of the soil in buffer zones under different management practices
in Finland, Agric. Food Sci., 19, 160–172, 2010.
Rezapour, S. and Samadi, A.: Assessment of inceptisols soil quality
following long-term cropping in a calcareous environment, Environ. Monit.
Assess., 184, 1311–1323, https://doi.org/10.1007/s10661-011-2042-6, 2012.
Richter, D. D. B., Bacon, A. R., Megan, L. M., Richardson, C. J., Andrews,
S. S., West, L., Wills, S., Billings, S., Cambardella, C. A., Cavallaro, N.,
DeMeester, J. E., Franzluebbers, A. J., Grandy, A. S., Grunwald, S., Gruver,
J., Hartshorn, A. S., Janzen, H., Kramer, M. G., Ladha, J. K., Lajtha, K.,
Liles, G. C., Markewitz, D., Megonigal, P. J., Mermut, A. R., Rasmussen, C.,
Robinson, D. A., Smith, P., Stiles, C. A., Tate, R. L., Thompson, A., Tugel,
A. J., Es, H. V., Yaalon, D., and Zobeck, T. M.: Human-soil relations are
changing rapidly: Proposals from SSSA's cross-divisional soil change working
group, Soil Sci. Soc. Am. J., 75, 2079–2084, https://doi.org/10.2136/sssaj2011.0124,
2011.
Richter, D. deB. J.: Humanity's transformation of earth's soil: pedology's new frontier, Soil Sci., 172, 957, https://doi.org/10.1097/ss.0b013e3181586bb7,
2007.
Richter, D. deB., Bacon, A. R., Brecheisen, Z., and Mobley, M. L.: Soil in the
Anthropocene, IOP Conf. Ser. Earth Environ. Sci., 25, 012010,
https://doi.org/10.1088/1755-1315/25/1/012010, 2015.
Rose, C. W., Williams, J. R., Sander, G. C., and Barry, D. A.: A Mathematical
Model of Soil Erosion and Deposition Processes: I. Theory for a Plane Land
Element 1, Soil Sci. Soc. Am. J., 47, 991–995,
https://doi.org/10.2136/sssaj1983.03615995004700050030x, 1983.
Sandor, J., Burras, C. L., and Thompson, M.: Factors of soil formation: human
impacts, in: Encyclopedia of Soils in the Environment, edited by: Hillel, D.,
pp. 520–532, Elsevier Ltd., available at:
https://www.elsevier.com/books/encyclopedia-of-soils-in-the-environment/9780123485304
(last access: 22 April 2019), 2005.
Sandor, J. A. and Homburg, J. A.: Anthropogenic Soil Change in Ancient and
Traditional Agricultural Fields in Arid to Semiarid Regions of the Americas,
J. Ethnobiol., 37, 196–217, https://doi.org/10.2993/0278-0771-37.2.196, 2017.
Sandor, J. A., Hawley, J. W., Schiowitz, R. H., and Gersper, P. L.:
Soil-geomorphic setting and change in prehistoric agricultural terraces in
the Mimbres area, New Mexico, in: Geology of the Gila Wilderness-Silver City
area: New Mexico Geological Society Fifty-ninth Annual Field Conference,
23–25 October 2008, pp. 167–176, New Mexico Geological Society, Socorro,
NM, 2008.
Sedov, S., Solleiro-Rebolledo, E., Fedick, S. L., Gama-Castro, J.,
Palacios-Mayorga, S., and Vallejo Gómez, E.: Soil genesis in relation to
landscape evolution and ancient sustainable land use in the northeastern
Yucatan Peninsula, Mexico, Atti Della Soc. Toscana Sci. Nat. Mem. Ser. A,
112, 115–126, 2007.
Severiano, E. da C., de Oliveira, G. C., Dias Junior, M. de S., Curi, N., de
Pinho Costa, K. A., and Carducci, C. E.: Preconsolidation pressure, soil
water retention characteristics, and texture of Latosols in the Brazilian
Cerrado, Soil Res., 51, 193–202, https://doi.org/10.1071/SR12366, 2013.
Seybold, C. A., Mausbach, M. J., Karlen, D. L., and Rogers, H. H.:
Quantification of soil quality, in: Soil Processes and the Carbon Cycle,
edited by: Lal, R., Kimble, J. M., Follett, R. F., and Stewart, B. A., CRC Press,
Boca Raton, FL, 1997.
Shiri, J., Keshavarzi, A., Kisi, O., Karimi, S., and Iturraran-Viveros, U.:
Modeling soil bulk density through a complete data scanning procedure:
Heuristic alternatives, J. Hydrol., 549, 592–602,
https://doi.org/10.1016/j.jhydrol.2017.04.035, 2017.
Shpedt, A. A., Trubnikov, Y. N., and Zharinova, N. Y.: Agrogenic degradation
of soils in Krasnoyarsk forest-steppe, Eurasian Soil Sci., 50,
1209–1216, https://doi.org/10.1134/S106422931710012X, 2017.
Simonson, R. W.: Outline of a Generalized Theory of Soil Genesis 1, Soil
Sci. Soc. Am. J., 23, 152–156,
https://doi.org/10.2136/sssaj1959.03615995002300020021x, 1959.
Smith, P., Smith, J. U., Powlson, D. S., McGill, W. B., Arah, J. R. M.,
Chertov, O. G., Coleman, K., Franko, U., Frolking, S., Jenkinson, D. S.,
Jensen, L. S., Kelly, R. H., Klein-Gunnewiek, H., Komarov, A. S., Li, C.,
Molina, J. A. E., Mueller, T., Parton, W. J., Thornley, J. H. M., and
Whitmore, A. P.: A comparison of the performance of nine soil organic matter
models using datasets from seven long-term experiments, Geoderma, 81,
153–225, https://doi.org/10.1016/S0016-7061(97)00087-6, 1997.
Taalab, K. P., Corstanje, R., Creamer, R., and Whelan, M. J.: Modelling soil bulk density at the landscape scale and its contributions to C stock uncertainty, Biogeosciences, 10, 4691–4704, https://doi.org/10.5194/bg-10-4691-2013, 2013.
Targulian, V. O. and Goryachkin, S. V.: Soil memory: Tapes of record, carriers, hierarchie and diversity, Revista Mexicana de Ciencias Geológicas, 21, 1–8, 2004.
Tiessen, H., Cuevas, E., and Chacon, P.: The role of soil organic matter in
sustaining soil fertility, Nature, 371, 783–785,
https://doi.org/10.1038/371783a0, 1994.
Tranter, G., Minasny, B., Mcbratney, A. B., Murphy, B., Mckenzie, N. J.,
Grundy, M., and Brough, D.: Building and testing conceptual and empirical
models for predicting soil bulk density, Soil Use Manag., 23, 437–443,
https://doi.org/10.1111/j.1475-2743.2007.00092.x, 2007.
Trost, B., Ellmer, F., Baumecker, M., Meyer-Aurich, A., Prochnow, A., and
Drastig, K.: Effects of irrigation and nitrogen fertilizer on yield, carbon
inputs from above ground harvest residues and soil organic carbon contents
of a sandy soil in Germany, Soil Use Manag., 30, 209–218,
https://doi.org/10.1111/sum.12123, 2014.
Tugel, A. J., Herrick, J. E., Brown, J. R., Mausbach, M. J., Puckett, W., and
Hipple, K.: Soil Change, Soil Survey, and Natural Resources Decision Making,
Soil Sci. Soc. Am. J., 69, 738–747, https://doi.org/10.2136/sssaj2004.0163, 2005.
Velde, B. and Peck, T.: Clay mineral changes in the Morrow experimental plots, University of Illinois, Clays Clay Miner., 50, 364–370, 2002.
Wei, G., Zhou, Z., Guo, Y., Dong, Y., Dang, H., Wang, Y., and Ma, J.:
Long-Term Effects of Tillage on Soil Aggregates and the Distribution of Soil
Organic Carbon, Total Nitrogen, and Other Nutrients in Aggregates on the
Semi-Arid Loess Plateau, China, Arid Land Res. Manag., 28, 291–310,
https://doi.org/10.1080/15324982.2013.845803, 2014.
Weiss, H., Courty, M., Wetterstrom, W., Guichard, F., Senior, L., Meadow, R.,
and Curnow, A.: The Genesis and Collapse of 3rd Millennium North
Mesopotamian Civilization, Science, 261, 995–1004,
https://doi.org/10.1126/science.261.5124.995, 1993.
WRB: World reference base for soil resources 2014: International soil
classification system for naming soils and creating legends for soil maps –
Update 2015, Food & Agriculture Org., Rome, Italy, 2014.
Yaalon, D. H. and Yaron, B.: Framework for man-made soil changes – an
outline of metapedogenesis, Soil Sci., 102, 272–277, 1966.
Zakharov, S. A.: A Course of Soil Science, Gosizdat, Moscow, 1927.
Zamanian, K. and Kuzyakov, Y.: Contribution of soil inorganic carbon to
atmospheric CO2: More important than previously thought, Glob. Change Biol.,
25, E1–E3, https://doi.org/10.1111/gcb.14463, 2019.
Zhang, Y., Zhao, W., and Fu, L.: Soil macropore characteristics following
conversion of native desert soils to irrigated croplands in a desert-oasis
ecotone, Northwest China, Soil Tillage Res., 168, 176–186,
https://doi.org/10.1016/j.still.2017.01.004, 2017.
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Agropedogenesis, i.e. soil development under agricultural use, is the anthropogenic modification of soil and environmental factors for optimization of crop production. Maximization of only this function, crop production, leads to declines in all other soil functions and consequently promotes uniformity in soil properties around the globe. Here we developed a new scientific background for the theory of agropedogenesis and the identification of soil degradation stages.
Agropedogenesis, i.e. soil development under agricultural use, is the anthropogenic modification...
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