A new approach to calculate the particle density of soils considering properties of the soil organic matter and the mineral matrix

Geoderma ◽  
2006 ◽  
Vol 130 (3-4) ◽  
pp. 272-283 ◽  
Author(s):  
Jörg Rühlmann ◽  
Martin Körschens ◽  
Jan Graefe
Geoderma ◽  
2017 ◽  
Vol 286 ◽  
pp. 83-87 ◽  
Author(s):  
P. Schjønning ◽  
R.A. McBride ◽  
T. Keller ◽  
P.B. Obour

2021 ◽  
Vol 862 (1) ◽  
pp. 012030
Author(s):  
K Tsivka ◽  
A I Popov ◽  
Yu V Simonova ◽  
G Kholostov ◽  
E Sazanova ◽  
...  

2018 ◽  
Author(s):  
Suzanne Lutfalla ◽  
Pierre Barré ◽  
Sylvain Bernard ◽  
Corentin Le Guillou ◽  
Julien Alléon ◽  
...  

Abstract. The mineral matrix, particularly clay-sized minerals, protects soil organic matter (SOM) from decomposition by microorganisms. Here we report the characterization of SOM and associated minerals over decades of biodegradation, in a French long-term bare fallow (LTBF) experiment started in 1928. The amounts of carbon (C) and nitrogen (N) declined with time for six fractions (sand, coarse silt, fine silt, coarse clays, intermediate clays and fine clays). The C : N ratios of SOM associated to silt fractions remained constant whereas they significantly decreased in clays, reaching very low values in intermediate and fine clays (C : N 


Geoderma ◽  
2017 ◽  
Vol 292 ◽  
pp. 150 ◽  
Author(s):  
P. Schjønning ◽  
R.A. McBride ◽  
T. Keller ◽  
P.B. Obour

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