Articles | Volume 17, issue 20
https://doi.org/10.5194/bg-17-5025-2020
© Author(s) 2020. 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-17-5025-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
19 Oct 2020
Research article |
| 19 Oct 2020
| 19 Oct 2020
Modelling dynamic interactions between soil structure and the storage and turnover of soil organic matter
Katharina Hildegard Elisabeth Meurer
CORRESPONDING AUTHOR
Department of Soil and Environment, Swedish University of Agricultural Sciences, 750 07 Uppsala, Sweden
Claire Chenu
AgroParisTech, UMR Ecosys INRA-AgroParisTech, Université
Paris-Saclay, 78850 Thiverval-Grignon, France
Elsa Coucheney
Department of Soil and Environment, Swedish University of Agricultural Sciences, 750 07 Uppsala, Sweden
Anke Marianne Herrmann
Department of Soil and Environment, Swedish University of Agricultural Sciences, 750 07 Uppsala, Sweden
Thomas Keller
Department of Soil and Environment, Swedish University of Agricultural Sciences, 750 07 Uppsala, Sweden
Department of Agroecology and Environment, Agroscope, 8046
Zürich, Switzerland
Thomas Kätterer
Department of Ecology, Swedish University of Agricultural Sciences,
750 05 Uppsala, Sweden
David Nimblad Svensson
Department of Soil and Environment, Swedish University of Agricultural Sciences, 750 07 Uppsala, Sweden
Nicholas Jarvis
Department of Soil and Environment, Swedish University of Agricultural Sciences, 750 07 Uppsala, Sweden
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Lauric Cécillon, François Baudin, Claire Chenu, Sabine Houot, Romain Jolivet, Thomas Kätterer, Suzanne Lutfalla, Andy Macdonald, Folkert van Oort, Alain F. Plante, Florence Savignac, Laure N. Soucémarianadin, and Pierre Barré
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Lorenzo Menichetti, Thomas Kätterer, and Jens Leifeld
Biogeosciences, 13, 3003–3019, https://doi.org/10.5194/bg-13-3003-2016, https://doi.org/10.5194/bg-13-3003-2016, 2016
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C. Poeplau, H. Marstorp, K. Thored, and T. Kätterer
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Christopher Poeplau, Martin A. Bolinder, Holger Kirchmann, and Thomas Kätterer
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C. Poeplau, M. A. Bolinder, J. Eriksson, M. Lundblad, and T. Kätterer
Biogeosciences, 12, 3241–3251, https://doi.org/10.5194/bg-12-3241-2015, https://doi.org/10.5194/bg-12-3241-2015, 2015
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M. Larsbo, J. Koestel, and N. Jarvis
Hydrol. Earth Syst. Sci., 18, 5255–5269, https://doi.org/10.5194/hess-18-5255-2014, https://doi.org/10.5194/hess-18-5255-2014, 2014
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The characteristics of the macropore network determine the potential for fast transport of solutes through soil. Such characteristics computed from 3-dimensional X-ray tomography images were combined with measured solute breakthrough curves and near-saturated hydraulic conductivities. At a given flow rate, smaller macroporosities, poorer local connectivity of the macropore network and smaller near-saturated hydraulic conductivities resulted in a greater degree of preferential transport.
K. Steffens, M. Larsbo, J. Moeys, E. Kjellström, N. Jarvis, and E. Lewan
Hydrol. Earth Syst. Sci., 18, 479–491, https://doi.org/10.5194/hess-18-479-2014, https://doi.org/10.5194/hess-18-479-2014, 2014
N. Jarvis, J. Koestel, I. Messing, J. Moeys, and A. Lindahl
Hydrol. Earth Syst. Sci., 17, 5185–5195, https://doi.org/10.5194/hess-17-5185-2013, https://doi.org/10.5194/hess-17-5185-2013, 2013
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Peter Levy, Laura Bentley, Peter Danks, Bridget Emmett, Angus Garbutt, Stephen Heming, Peter Henrys, Aidan Keith, Inma Lebron, Niall McNamara, Richard Pywell, John Redhead, David Robinson, and Alexander Wickenden
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Because of its importance for climate regulation and soil health, many studies focus 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, the Rock-Eval® method has the potential to become the standard method for quantifying carbon in carbonate soils.
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.
Kyle E. Smart, Daniel O. Breecker, Christopher B. Blackwood, and Timothy M. Gallagher
EGUsphere, https://doi.org/10.5194/egusphere-2024-1757, https://doi.org/10.5194/egusphere-2024-1757, 2024
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When microbes consume carbon within soils, it is important to know how much carbon is respired and lost as carbon dioxide versus how much is used to make new biomass. We used a new approach of monitoring carbon dioxide and oxygen to track the fate of consumed carbon during a series of laboratory experiments where sugar was added to moistened soil. Our approach allowed us to estimate how much sugar was converted to dead microbial biomass, which is more likely to be preserved in soils.
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.
Henning Teickner, Edzer Pebesma, and Klaus-Holger Knorr
EGUsphere, https://doi.org/10.5194/egusphere-2024-1686, https://doi.org/10.5194/egusphere-2024-1686, 2024
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Decomposition rates for Sphagnum mosses, the main peat forming plants in northern peatlands, are often derived from litterbag experiments. Here, we estimate initial leaching losses from available Sphagnum litterbag experiments and analyze how decomposition rates are biased when initial leaching losses are ignored. Our analyses indicate that initial leaching losses range between 3 to 18 mass-% and that this may result in overestimated mass losses when extrapolated to several decades.
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.
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.
Shanshan Bai, Yifei Ge, Dongtan Yao, Yifan Wang, Jinfang Tan, Shuai Zhang, Yutao Peng, and Xiaoqian Jiang
EGUsphere, https://doi.org/10.5194/egusphere-2024-983, https://doi.org/10.5194/egusphere-2024-983, 2024
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Mineral fertilization led to increases in total P, available P, high-activity inorganic P fractions and organic P, but decreased the abundances of P cycling genes by decreasing soil pH and increasing P in bulk soil. Straw retention brought increases for organic C, total P, available P concentrations in water-extractable colloids (WECs). Abundances of phoD gene and phoD-harbouring Proteobacteria in WECs increased under straw retention, suggesting that the P mineralizing capacity increased.
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
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
Cited articles
Adams, W. A.: The effect of organic matter on the bulk and true densities of
some uncultivated podzolic soils, J. Soil Sci., 24, 10–17,
1973.
Ahrens, B., Braakhekke, M., Guggenberger, G., Schrumpf, M., and Reichstein, M.:
Contribution of sorption, DOC transport and microbial interactions to the
14C age of a soil organic carbon profile: Insights from a calibrated process
model, Soil Biol. Biochem., 88, 390–402, 2015.
Andrén, O. and Kätterer, T.: ICBM: the introductory carbon balance
model for exploration of soil carbon balances, Ecol. Appl., 7,
1226–1236, 1997.
Angst, Š., Mueller, C., Cajthaml, T., Angst, G., Lhotáková, Z.,
Bartuška, M., Špaldoňová, A., and Frouz, J.: Stabilization of
soil organic matter by earthworms is connected with physical protection
rather than with chemical changes of organic matter, Geoderma, 289, 29–35,
2017.
Arya, L. and Heitman, J.: A non-empirical method for computing pore radii and
soil water characteristics from particle-size distribution, Soil Sci.
Soc. Am. J., 79, 1537–1544, 2015.
Arya, L., Leij, F., van Genuchten, M., and Shouse, P.: Scaling parameter to
predict the soil water characteristic from particle-size distribution data,
Soil Sci. Soc. Am. J., 63, 510–519, 1999.
Assouline, S. and Or, D.: Conceptual and parametric representation of soil
hydraulic properties: a review, Vadose Zone J., 12, vzj2013.07.0121,
https://doi.org/10.2136/vzj2013.07.0121, 2013.
Balesdent, J., Chenu, C., and Balabane, M.: Relationship of soil organic matter
dynamics to physical protection and tillage, Soil Till. Res., 53,
215–230, 2000.
Barré, P., Eglin, T., Christensen, B., Ciais, P., Houot, S.,
Kätterer, T., van Oort, F., Peylin, P., Poulton, P., Romanenkov, V.,
and Chenu, C.: Quantifying and isolating stable organic carbon using long-term
bare fallow experiments, Biogeochemistry, 7, 3839–3850, 2010.
Beven, K.: A manifesto for the equifinality thesis, J. Hydrol.,
320, 18–36, 2006.
Blagodatskaya, E. and Kuzyakov, Y.: Mechanisms of real and apparent priming
effects and their dependence on soil microbial biomass and community
structure: critical review, Biol. Fert. Soils, 45, 115–131,
2008.
Boivin, P., Schäffer, B., and Sturny, W.: Quantifying the relationship
between soil organic carbon and soil physical properties using shrinkage
modelling, Eur. J. Soil Sci., 60, 265–275, 2009.
Bolinder M., Janzen, H., Gregorich, E., Angers, D., and van den Bygaart, A.: An
approach for estimating net primary productivity and annual carbon inputs to
soil for common agricultural crops in Canada, Agr. Ecosyst.
Environ., 118, 29–42, 2007.
Bradford, M.: Managing uncertainty in soil carbon feedbacks to climate
change, Nat. Clim. Change, 6, 751–758, 2016.
Bucka, F., Kölbl, A., Uteau, D., Peth, S., and Kögel-Knabner, I.:
Organic matter input determines structure development and aggregate
formation in artificial soils, Geoderma, 354, 113881, https://doi.org/10.1016/j.geoderma.2019.113881, 2019.
Chevallier, T., Blanchart, E., Albrecht, A., and Feller, C.: The physical
protection of soil organic carbon in aggregates: a mechanism of carbon
storage in a Vertisol under pasture and market gardening (Martinique, West
Indies), Agr. Ecosyst. Environ., 103, 375–387, 2004.
Cosentino, D., Chenu, C., and Le Bissonnais, Y.: Aggregate stability and
microbial community dynamics under drying-wetting cycles in a silt loam
soil, Soil Biol. Biochem., 38, 2053–2062, 2006.
Dignac, M.-F., Derrien, D., Barré, P., Barot, S., Cécillon, L.,
Chenu, C., Chevallier, T., Freschet, G., Garnier, P., Guenet, B., Hedde, M.,
Klumpp, K., Lashermes, G., Maron, P.-A., Nunan, N., Roumet, C., and
Basile-Doelsch, I.: Increasing soil carbon storage: mechanisms, effects of
agricultural practices and proxies, A review, Agron. Sustain.
Dev., 37, 1–27, https://doi.org/10.1007/s13593-017-0421-2, 2017.
Don, A., Steinberg, B., Schöning, I., Pritsch, K., Joschko, M.,
Gleixner, G., and Schulze, E.: Organic carbon sequestration in earthworm
burrows, Soil Biol. Biochem., 40, 1803–1812, 2008.
Dungait, J., Hopkins, D., Gregory, A., and Whitmore, A.: Soil organic matter
turnover is governed by accessibility not recalcitrance, Glob. Change
Biol., 18, 1781–1796, 2012.
Durner, W.: Hydraulic conductivity estimation for soils with heterogeneous
pore structure, Water Resour. Res., 30, 211–223, 1994.
Ekschmitt, K., Kandeler, E., Poll, C., Brune, A., Buscot, F., Friedrich, M.,
Gleixner, G., Hartmann, A., Kästner, M., Marhan, S., Miltner, A., Scheu,
S., and Wolters, V.: Soil-carbon preservation through habitat constraints and
biological limitations on decomposer activity, J. Soil Sci.
Plant Nutr., 171, 27–35, 2008.
Emerson, W. and McGarry, D.: Organic carbon and soil porosity, Austr.
J. Soil Res., 41, 107–118, 2003.
Falloon, P. and Smith, P.: Modelling refractory soil organic matter, Biol.
Fert. Soils, 30, 388–398, 2000.
Federer, C., Turcotte, D., and Smith, C.: The organic fraction–bulk density
relationship and the expression of nutrient content in forest soils,
Can. J. Forest Res., 23, 1026–1032, 1993.
Feeney, D., Crawford, J., Daniell, T., Hallett, P., Nunan, N., Ritz, K.,
Rivers, M., and Young, I.: Three-dimensional microorganization of the
soil-root-microbe system, Microb. Ecol., 52, 151–158, 2006.
Fies, J.-C. and Stengel, P.: Densité texturale de sols naturels I. –
Méthode de mesure, Agronomie, 1, 651–658, 1981.
Gerzabek, M., Pichlmayer, F., Kirchmann, H., and Haberhauer, G.: The response of
organic matter to manure amendments in a long-term experiment at Ultuna,
Sweden, Eur. J. Soil Sci., 48, 273–282, 1997.
Görres, J., Savin, M., and Amador, J.: Soil micropore structure and carbon
mineralization in burrows and casts of an anecic earthworm (Lumbricus terrestris), Soil Biol.
Biochem., 33, 1881–1887, 2001.
Hassink, J., Bouwman, L., Zwart, K., Bloem, J., and Brussaard, L.: Relationships
between soil texture, physical protection of organic matter, soil biota, and
C and N mineralization in grassland soils, Geoderma, 57, 105–128, 1993.
Hassink, J. and Whitmore, A.: A model of the physical protection of organic
matter in soils, Soil Sci. Soc. Am. J., 61, 131–139, 1997.
Haynes, R. and Naidu, R.: Influence of lime, fertiliser and manure applications
on soil organic matter content and soil physical conditions: a review,
Nutr. Cycl. Agr., 51, 123–137, 1998.
Henryson, K., Sundberg, C., Kätterer, T., and Hansson, P.-A.: Accounting for
long-term soil fertility effects when assessing the climate impact of crop
cultivation, Agr. Syst., 164, 185–192, 2018.
Herrmann, A. M.: Predicting nitrogen mineralization from soil organic matter
– a chimera? Doctoral Thesis, Swedish University of Agricultural Sciences,
Uppsala, Sweden, ISSN 1401-6249, ISBN 91-576-6468-4, 2003.
Herrmann, A. M. and Witter, E.: Predictors of gross N mineralization and
immobilization during decomposition of stabilized organic matter in
agricultural soil, Eur. J. Soil Sci., 59, 653–664, 2008.
Herrmann, A. M., Coucheney, E., and Nunan, N.: Isothermal microcalorimetry
provides new insight into terrestrial carbon cycling, Environ. Sci.
Technol., 48, 4344–4352, 2014.
Hudson, B.: Soil organic matter and available water capacity, J.
Soil Water Conserv., 49, 189–194, 1994.
Hyvönen, R., Ågren, G. I., and Andrén, O.: Modelling long-term carbon
and nitrogen dynamics in an arable soil receiving organic matter, Ecol.
Appl., 6, 1345–1354, 1996.
Jarvis, N. J., Forkman, J., Koestel, J., Kätterer, Larsbo, M., and Taylor,
A.: Long-term effects of grass-clover leys on the structure of a silt loam
soil in a cold climate, Agr. Ecosyst. Environ., 247,
319–328, 2017.
Johannes A., Matter, A., Schulin, R., Weisskopf, P., Baveye, P., and Boivin, P.:
Optimal organic carbon values for soil structure quality of arable soils.
Does clay content matter?, Geoderma, 302, 14–21, 2017.
Juston, J., Andrén, O., Kätterer, T., and Jansson, P.-E.: Uncertainty
analyses for calibrating a soil carbon balance model to agricultural field
trial data in Sweden and Kenya, Ecol. Modell., 221, 1880–1888, 2010.
Kätterer, T., Bolinder, M., Andrén, O., Kirchmann, H., and Menichetti,
L.: Roots contribute more to refractory soil organic matter than
above-ground crop residues, as revealed by a long-term field experiment,
Agr. Ecosyst. Environ., 141, 184–192, 2011.
Kirchmann, H. and Gerzabek, M.: Relationship between soil organic matter and
micropores in a long-term experiment at Ultuna, Sweden, J. Plant
Nutr. Soil Sci., 162, 493–498, 1999.
Kirchmann, H., Persson, J., and Carlgren, K.: The Ultuna long-term soil organic
matter experiment, 1956–1991, Department of Soil Sciences, Reports and
Dissertations 17, Swedish University of Agricultural Sciences, Uppsala,
Sweden, 1994.
Kravchenko, A. and Guber, A.: Soil pores and their contributions to soil carbon
processes, Geoderma, 287, 31–39, 2017.
Kravchenko, A., Negassa, W., Guber, A., and Rivers, M.: Protection of soil
carbon within macro-aggregates depends on intra-aggregate pore
characteristics, Sci. Rep., 5, 16261, https://doi.org/10.1038/srep16261,
2015.
Kuka, K., Franko, U., and Rühlmann, J.: Modelling the impact of pore space
distribution on carbon turnover, Ecol. Modell., 208, 295–306, 2007.
Lal, R.: Carbon management in agricultural soils, Mitigation and Adaptation
Strategies for global change, Mitig. Adapt. Strat. Gl., 12, 303–322, 2007.
Lal, R.: Intensive agriculture and the soil carbon pool, J. Crop
Improv., 27, 735–751, 2013.
Larsbo, M., Roulier, S., Stenemo, F., Kasteel, R., and Jarvis, N.: An improved
dual-permeability model of water flow and solute transport in the vadose
zone, Vadose Zone J., 4, 398–406, 2005.
Larsbo, M., Koestel, J., Kätterer, T., and Jarvis, N.: Preferential
transport in macropores is reduced by soil organic carbon, Vadose Zone
J., 15, 1–7, https://doi.org/10.2136/vzj2016.03.0021, 2016.
Lehmann J. and Kleber, M.: The contentious nature of soil organic matter,
Nature, 528, 60–68, 2015.
Libohova, Z., Seybold, C., Wysocki, D., Wills, S., Schoeneberger, P.,
Williams, C., Lindbo, D., Stott, D., and Owens, P.: Reevaluating the effects of
soil organic matter and other properties on available water-holding capacity
using the National Cooperative Soil Survey Characterization Database,
J. Soil Water Conserv., 73, 411–421, 2018.
Loveland, P. and Webb, J.: Is there a critical level of organic matter in the
agricultural soils of temperate regions: a review, Soil Till.
Res., 70, 1–18, 2003.
Luo, Z., Wang, E., and Sun, O.: Uncertain future soil carbon dynamics under
global change predicted by models constrained by total carbon measurements,
Ecol. Appl., 27, 1001–1009, 2017.
Martin, A.: Short- and long-term effects of the endogeic earthworm Millsonia
anomala (Omodeo)(Megascolecidae, Oligochaeta) of tropical savannas, on soil
organic matter, Biol. Fert. Soils, 11, 234–238, 1991.
Minasny, B. and McBratney, A.: Limited effect of organic matter on soil
available water capacity, Eur. J. Soil Sci., 69, 39–47, 2018.
Nimmo, J.: Porosity and pore size distribution. Reference module in earth
systems and environmental Sciences, Elsevier, 27 September 2013, https://doi.org/10.1016/B978-0-12-409548-9.05265-9, 2013.
Nunan, N., Leloup, J., Ruamps, L. S., Pouteau, V., and Chenu, C.: Effects of
habitat constraints on soil microbial community function, Sci.
Rep., 7, 4280, https://doi.org/10.1038/s41598-017-04485-z, 2017.
Pankhurst, C., Pierret, A., Hawke, B., and Kirby, J.: Microbiological and
chemical properties of soil associated with macropores at different depths
in a red-duplex soil in NSW Australia, Plant Soil, 238, 11–20, 2002.
Paustian, K., Parton, W., and Persson, J.: Modeling soil organic-matter in
organic-amended and nitrogen-fertilized long-term plots, Soil Sci.
Soc. Am. J., 56, 476–488, 1992.
Poeplau, C., Kätterer, T., Bolinder, M., Börjesson, G., Berti, A.,
and Lugato, E.: Low stabilization of aboveground crop residue carbon in sandy
soils of Swedish long-term experiments, Geoderma, 237/238, 246–255, 2015.
Powell, M.: The BOBYQA algorithm for bound constrained optimization without
derivatives (Report), available at: http://www.damtp.cam.ac.uk/user/na/NA_papers/NA2009_06.pdf (last access: 21 October 2019), 2009.
Pribyl, D.: A critical review of the conventional SOC to SOM conversion
factor, Geoderma 156, 75–83, 2010.
Quigley, M., Negassa, W., Guber, A., Rivers, M., and Kravchenko, A.: Influence
of pore characteristics on the fate and distribution of newly added carbon,
Front. Environ. Sci., 6, 51 pp., https://doi.org/10.3389/fenvs.2018.00051,
2018.
R Core Team: R: A language and environment for statistical computing. R
Foundation for Statistical Computing, Vienna, Austria, available at:
https://www.R-project.org/ (last access: 14 October 2020), 2018.
Rabot, E., Wiesmeier, M., Schlüter, S., and Vogel, H.-J.: Soil structure as an
indicator of soil functions: a review, Geoderma, 314, 122–137, 2018.
Rawls, W., Pachepsky, Y., Ritchie, J., Sobecki, T., and Bloodworth, H.: Effect
of soil organic carbon on soil water retention, Geoderma, 116, 61–76, 2003.
Rickson, J., Deeks, L., Graves, A., Harris, J., Kibblewhite, M., and Sakrabani,
R.: Input constraints to food production: the impact of soil degradation,
Food Secur., 7, 351–364, 2015.
Ruamps, L. S., Nunan, N., and Chenu, C.: Microbial biogeography at the soil pore
scale, Soil Biol. Biochem., 43, 280–286, 2011.
Ruehlmann, J. and Körschens, M.: Calculating the effect of soil organic
matter concentration on soil bulk density, Soil Sci. Soc. Am.
J., 73, 876–885, 2009.
Sanderman, J., Hengl, T., and Fiske, G.: Soil carbon debt of 12,000 years of
human land use, P. Natl. Acad. Sci. USA, 114, 9575–9580, 2017.
Segoli, S., De Gryze, S., Dou, F., Lee, J., Post, W., Denef, K., and Six, J.:
AggModel: a soil organic matter model with measurable pools for use in
incubation studies, Ecol. Modell., 263, 1–9, 2013.
Sierra, C., Malghani, S., and Müller, M.: Model structure and parameter
identification of soil organic matter models, Soil Biol. Biochem.,
90, 197–203, 2015.
Souza, I., Almeida, L., Jesus, G., Kleber, M., and Silva, I.: The mechanisms of
organic carbon protection and dynamics of C-saturation in Oxisols vary with
particle-size distribution, Eur. J. Soil Sci., 68, 726–739,
2017.
Stamati, F., Nikolaidis, N., Banwart, S., and Blum, W.: A coupled carbon,
aggregation, and structure turnover (CAST) model for topsoils, Geoderma,
211/212, 51–64, 2013.
Stewart, C., Paustian, K., Conant, R., Plante, A., and Six, J.: Soil carbon
saturation: concept, evidence and evaluation, Biogeochemistry, 86, 19–31,
2007.
Stewart, V. I., Adams, W. A., and Abdulla, H. H.: Quantitative pedological studies
on soils derived from Silurian mudstones, II. The relationship between stone
content and the apparent density of the fine Earth, J. Soil Sci.,
21, 242–247, 1970.
Strong, D., de Wever, H., Merckx, R., and Recous, S.: Spatial location of carbon
decomposition in the soil pore system, Eur. J. Soil Sci., 55,
739–750, 2004.
Tisdall, J. M. and Oades, J. M.: Organic matter and water stable aggregates in
soils, J. Soil Sci., 33, 141–163, 1982.
Toosi, E., Kravchenko, A., Guber, A., and Rivers, M.: Pore characteristics
regulate priming and fate of carbon from plant residue, Soil Biol.
Biochem., 113, 219–230, 2017.
Tranter, G., Minasny, B., McBratney, A., Murphy, B., McKenzie, N., Grundy,
M., and Brough, D.: Building and testing conceptual and empirical models for
predicting soil bulk density, Soil Use Manage., 23, 437–443, 2007.
van Genuchten, M.: A closed-form equation for predicting the hydraulic
conductivity of unsaturated Soils, Soil Sci. Soc. Am. J.,
44, 892–898, 1980.
Vereecken, H., Weynants, M., Javaux, M., Pachepsky, Y., Schaap, M., and van
Genuchten, M.: Using pedotransfer functions to estimate the van
Genuchten-Mualem soil hydraulic properties: a review, Vadose Zone J.,
9, 795–820, 2010.
Vogel, H.-J., Weller, U., and Schlüter, S.: Quantification of soil structure
based on Minkowski functions, Comput. Geosci., 36, 1236–1245,
2010.
Walker, A.: Openxlsx: Read, Write and Edit XLSX Files, P package version
4.1.0.1, available at: https://cran.r-project.org/web/packages/openxlsx/index.html (last access: 14 October 2020), 2019.
Wickham, H.: The Split-Allpy-Combine Strategy for Data Analysis, J.
Stat. Softw., 40, 1–29,
2011.
Wiklert, P., Andersson, S., and Weidow, B.: Studier av markprofiler i svenska
åkerjordar, En faktasammanställning. Del I. Ultunajordar, Report
132, Dept. Soil Sciences, Division of Agricultural Hydrotechnics, Swedish
University of Agricultural Sciences, 125 pp., 1983.
Witter, E.: Soil C balance in a long-term field experiment in relation to
the size of the microbial biomass, Biol. Fert. Soils, 23, 33–37, 1996.
Wösten, H., Pachepsky, Y., and Rawls, W.: Pedotransfer functions: bridging
the gap between available basic soil data and missing soil hydraulic
characteristics, J. Hydrol., 251, 123–150, 2001.
Wutzler, T. and Reichstein, M.: Priming and substrate quality interactions in soil organic matter models, Biogeosciences, 10, 2089–2103, https://doi.org/10.5194/bg-10-2089-2013, 2013.
Yoon, S. and Gimenéz, D.: Entropy characterization of soil pore systems
derived from soil-water retention curves, Soil Science, 177, 361–368, 2012.
Young, I. and Crawford, J.: Interactions and self-organization in the
soil-microbe complex, Science, 304, 1634–1637, 2004.
Young, I., Crawford, J., and Rappoldt, C.: New methods and models for
characterising structural heterogeneity of soil, Soil Till. Res.,
61, 33–45, 2001.
Yu, L., Ahrens, B., Wutzler, T., Schrumpf, M., and Zaehle, S.: Jena Soil Model (JSM v1.0; revision 1934): a microbial soil organic carbon model integrated with nitrogen and phosphorus processes, Geosci. Model Dev., 13, 783–803, https://doi.org/10.5194/gmd-13-783-2020, 2020.
Short summary
We present a simple model that describes, for the first time, the dynamic two-way interactions between soil organic matter and soil physical properties (porosity, pore size distribution, bulk density and layer thickness). The model was able to accurately reproduce the changes in soil organic carbon, soil bulk density and surface elevation observed during 63 years in a field trial, as well as soil water retention curves measured at the end of the experimental period.
We present a simple model that describes, for the first time, the dynamic two-way interactions...
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