Abstract Understanding the distribution of soil organic carbon and nitrogen (OC(N)) content, cation exchange capacity (CEC), and specific surface area (SSA) in different soil particle sizes is crucial for studying soil fertility and properties. In this study, we investigated the distribution characteristics of the OC(N), CECand SSA in different particles of yellow–brown soil under different methods. The result revealed that as the particle size decreased, the soil OC(N), SSA and CEC content gradually increase. The content of OC and ON different soil particles ranged from 1.50–28.16 g·kg−1 to 0.18–3.78 g·kg−1, respectively, and exhibited significant differences between different particles. We observed good linear relationships between OC and...
Determining the effects of fertilization regimes on soil aggregates, carbon (C) and nitrogen (N) dis...
The distribution and storage of soil organic carbon serve as basic data for the study of soil produc...
Every soil has a limited capacity to physical-chemically protect organic matter from biodegradation ...
Non-Peer ReviewedThe capacity of a soil to store organic carbon is related to its particle size dist...
Despite the importance of phosphorus (P) as a macronutrient, the factors controlling the pool sizes ...
Many of the cultivated soils of sub-Saharan Africa typically have a surface horizon low in clay and ...
Correlations between organic carbon (OC) and fine mineral particles corroborate the important role o...
The kinetics of soil organic matter (SOM) in cultivated tropical soils are characterized by rapid mi...
According to recent conceptual models, the organic carbon (OC) of soils can be divided into OC fract...
The study determined the distribution of organic carbon (OC), cation exchange capacity (CEC) and tot...
As a fundamental characteristic of soil physical properties, the soil Particle Size Distribution (PS...
In addition to soil organic carbon (SOC), soil inorganic carbon (SIC) is also an important reservoir...
Not AvailableAnalyzed particle size distribution, soil water retention properties and organic carbon...
Fractionating soils according to size and/or density of particles improves our understanding of the ...
Soil quality has become an important issue in soil science. Considerable attempts have been made to ...
Determining the effects of fertilization regimes on soil aggregates, carbon (C) and nitrogen (N) dis...
The distribution and storage of soil organic carbon serve as basic data for the study of soil produc...
Every soil has a limited capacity to physical-chemically protect organic matter from biodegradation ...
Non-Peer ReviewedThe capacity of a soil to store organic carbon is related to its particle size dist...
Despite the importance of phosphorus (P) as a macronutrient, the factors controlling the pool sizes ...
Many of the cultivated soils of sub-Saharan Africa typically have a surface horizon low in clay and ...
Correlations between organic carbon (OC) and fine mineral particles corroborate the important role o...
The kinetics of soil organic matter (SOM) in cultivated tropical soils are characterized by rapid mi...
According to recent conceptual models, the organic carbon (OC) of soils can be divided into OC fract...
The study determined the distribution of organic carbon (OC), cation exchange capacity (CEC) and tot...
As a fundamental characteristic of soil physical properties, the soil Particle Size Distribution (PS...
In addition to soil organic carbon (SOC), soil inorganic carbon (SIC) is also an important reservoir...
Not AvailableAnalyzed particle size distribution, soil water retention properties and organic carbon...
Fractionating soils according to size and/or density of particles improves our understanding of the ...
Soil quality has become an important issue in soil science. Considerable attempts have been made to ...
Determining the effects of fertilization regimes on soil aggregates, carbon (C) and nitrogen (N) dis...
The distribution and storage of soil organic carbon serve as basic data for the study of soil produc...
Every soil has a limited capacity to physical-chemically protect organic matter from biodegradation ...