In the absence of significant mechanical disturbance such as under permanent no-till (NT), crop type should be a prominent factor controlling soil organic C (SOC) pools. Microbial cell residues have been shown to be influenced by plant species and are believed to contribute significantly to soil organic matter formation. We performed a study to investigate the co-accumulation of microbial cell wall residues (glucosamine, GlcN and muramic acid, MurN) and organic C (total and particle-size fractions) in the surface layer (0- to 5-cm depth) of an Oxisol after 7 yr under NT, as affected by different crop types. SOC content associated with pigeon pea [Cajanus cajan (L) Millsp.] was 20% and 18% higher than that with corn (Zea mays L) or sunflower...
Strategies for mitigating soil organic carbon (SOC) losses in intensively managed agricultural syste...
The rate of soil organic carbon (CS) loss via microbial respiration (decomposition rate k, y1), and ...
Long-term carbon (C) stabilisation in tropical and subtropical soils under no-tillage (NT) rests on ...
No-tillage (NT) and legume cover crops generally improve the quality of tropical and subtropical soi...
International audienceCrop residues are among the main inputs that allow the organic carbon (C) and ...
Quantifying residue carbon (C) incorporation into soil organic C (SOC) fractions, and underpinning m...
Decomposition of plant material influences soil aggregation dynamics in ways that are still poorly u...
Despite scant crop residue input, tillage to control weeds in vegetable systems reduces soil organic...
Substrate composition is one of the most important factors influencing the decomposition of plant re...
Vegetable production systems rely on frequent tillage to prepare beds and manage weeds, thereby acce...
International audienceSoil microorganisms play a key role in soil organic matter (SOM) dynamics, but...
Intensive agricultural management often depletes soil organic matter (SOM), the largest terrestrial ...
In no-till systems, plants play a substantial role in soil physical conditioning because physical ma...
Decomposing residues can be an important source of nutrients for plants, especially of N and P, but ...
Crop residue decomposition is mainly driven by, but also affects, soil microorganisms. However, soi...
Strategies for mitigating soil organic carbon (SOC) losses in intensively managed agricultural syste...
The rate of soil organic carbon (CS) loss via microbial respiration (decomposition rate k, y1), and ...
Long-term carbon (C) stabilisation in tropical and subtropical soils under no-tillage (NT) rests on ...
No-tillage (NT) and legume cover crops generally improve the quality of tropical and subtropical soi...
International audienceCrop residues are among the main inputs that allow the organic carbon (C) and ...
Quantifying residue carbon (C) incorporation into soil organic C (SOC) fractions, and underpinning m...
Decomposition of plant material influences soil aggregation dynamics in ways that are still poorly u...
Despite scant crop residue input, tillage to control weeds in vegetable systems reduces soil organic...
Substrate composition is one of the most important factors influencing the decomposition of plant re...
Vegetable production systems rely on frequent tillage to prepare beds and manage weeds, thereby acce...
International audienceSoil microorganisms play a key role in soil organic matter (SOM) dynamics, but...
Intensive agricultural management often depletes soil organic matter (SOM), the largest terrestrial ...
In no-till systems, plants play a substantial role in soil physical conditioning because physical ma...
Decomposing residues can be an important source of nutrients for plants, especially of N and P, but ...
Crop residue decomposition is mainly driven by, but also affects, soil microorganisms. However, soi...
Strategies for mitigating soil organic carbon (SOC) losses in intensively managed agricultural syste...
The rate of soil organic carbon (CS) loss via microbial respiration (decomposition rate k, y1), and ...
Long-term carbon (C) stabilisation in tropical and subtropical soils under no-tillage (NT) rests on ...