Biological mechanisms may contribute to soil carbon saturation patterns

2021 ◽  
Author(s):  
Matthew E. Craig ◽  
Melanie A. Mayes ◽  
Benjamin N. Sulman ◽  
Anthony P. Walker
2009 ◽  
Vol 41 (2) ◽  
pp. 357-366 ◽  
Author(s):  
Catherine E. Stewart ◽  
Keith Paustian ◽  
Richard T. Conant ◽  
Alain F. Plante ◽  
Johan Six

2008 ◽  
Vol 40 (7) ◽  
pp. 1741-1750 ◽  
Author(s):  
Catherine E. Stewart ◽  
Keith Paustian ◽  
Richard T. Conant ◽  
Alain F. Plante ◽  
Johan Six

2019 ◽  
Vol 188 ◽  
pp. 53-58 ◽  
Author(s):  
Songchao Chen ◽  
Dominique Arrouays ◽  
Denis A. Angers ◽  
Manuel P. Martin ◽  
Christian Walter

2019 ◽  
Vol 171 ◽  
pp. 13-22 ◽  
Author(s):  
M. Virginia Pravia ◽  
Armen R. Kemanian ◽  
José A. Terra ◽  
Yuning Shi ◽  
Ignacio Macedo ◽  
...  

2014 ◽  
Vol 94 (3) ◽  
pp. 281-294 ◽  
Author(s):  
W. Feng ◽  
M. Xu ◽  
M. Fan ◽  
S. S. Malhi ◽  
J. J. Schoenau ◽  
...  

Feng, W., Xu, M., Fan, M., Malhi, S. S., Schoenau, J. J., Six, J. and Plante, A. F. 2014. Testing for soil carbon saturation behavior in agricultural soils receiving long-term manure amendments. Can. J. Soil Sci. 94: 281–294. Agricultural soils are typically depleted in soil organic matter compared with their undisturbed counterparts, thus reducing their fertility. Organic amendments, particularly manures, provide the opportunity to restore soil organic matter stocks, improve soil fertility and potentially sequester atmospheric carbon (C). The application of the soil C saturation theory can help identify soils with large C storage potentials. The goal of this study was to test whether soil C saturation can be observed in various soil types in agricultural ecosystems receiving long-term manure amendments. Seven long-term agricultural field experiments from China and Canada were selected for this study. Manure amendments increased C concentrations in bulk soil, particulate organic matter+sand, and silt+clay fractions in all the experiments. The increase in C concentrations of silt+clay did not fit the asymptotic regression as a function of C inputs better than the linear regression, indicating that silt+clay did not exhibit C saturation behavior. However, 44% of calculated C loading values for silt+clay were greater than the presumed maximal C loading, suggesting that this maximum may be greater than 1 mg C m−2 for many soils. The influences of soil mineral surface properties on C concentrations of silt+clay fractions were site specific. Fine soil particles did not exhibit C saturation behavior likely because current C inputs were insufficient to fill the large C saturation deficits of intensely cultivated soils, suggesting these soils may continue to act as sinks for atmospheric C.


2007 ◽  
Vol 86 (1) ◽  
pp. 19-31 ◽  
Author(s):  
Catherine E. Stewart ◽  
Keith Paustian ◽  
Richard T. Conant ◽  
Alain F. Plante ◽  
Johan Six

2017 ◽  
Author(s):  
Pierre Barré ◽  
Denis A. Angers ◽  
Isabelle Basile-Doelsch ◽  
Antonio Bispo ◽  
Lauric Cécillon ◽  
...  

Abstract. An increase in soil organic carbon stock can contribute to mitigate climate change. International negotiation mechanisms and initiatives call for countries to consider land use change and soil management to achieve atmospheric CO2 removal through storage in terrestrial systems (http://4p1000.org/). As a result, policy makers raised a specific operational question to the soil science community: how much and at which annual rate additional carbon can be stored in soils in different locations? It has been suggested that the ability of a soil to store additional organic carbon can be estimated from its carbon saturation deficit (Csat-def), which is defined as the difference between the maximum amount of carbon that can be associated to its fine (


2008 ◽  
Vol 72 (2) ◽  
pp. 379-392 ◽  
Author(s):  
Catherine E. Stewart ◽  
Alain F. Plante ◽  
Keith Paustian ◽  
Richard T. Conant ◽  
Johan Six

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