SciELO - Scientific Electronic Library Online

 
vol.40Soil organic carbon depth distribution patterns in different land uses and managementSoil formation from tepetates: structural unities, organic carbon, and structural stability author indexsubject indexsearch form
Home Pagealphabetic serial listing  

Services on Demand

Journal

Article

Indicators

Related links

  • Have no similar articlesSimilars in SciELO

Share


Terra Latinoamericana

On-line version ISSN 2395-8030Print version ISSN 0187-5779

Abstract

PAZ, Fernando et al. Patterns of the distribution of organic carbon by fractions of primary soil particles. Terra Latinoam [online]. 2022, vol.40, e1322.  Epub June 13, 2022. ISSN 2395-8030.  https://doi.org/10.28940/terra.v40i0.1322.

In order to analyze the dynamics of soil organic carbon (SOC) associated with changes in land use / vegetation and management practices, it is necessary to develop models that can be used predictively. A modeling approach is the distribution of SOC by physical fractions of the primary organomineral complexes (clays, silts and sands), using ultrasound soil dispersion techniques, where it is necessary to optimize the sonication energies to achieve complete soil dispersion. Under this consideration of complete dispersion, the COLPOS model and its hypothesis are discussed, as well as its possible extensions when considering the masses and enrichments of the physical fractions of the soil, in addition to the analysis of the relationships between these fractions. To analyze the patterns associated with the COLPOS model and its extensions, the available Mexican soil fractionations using ultrasound are analyzed, in addition to three databases of similar fractionations published in the literature. The results show that the COLPOS model can be parameterized according to the size and mass of the soil particles; although for the case of the masses some results are inconsistent. From the analysis of the organic carbon ratios between fractions for two different kinetics, the relationships show greater dispersion than for the case of only kinetic fractions.

Keywords : organomineral and particulate complexes; dispersion energies; physical fractionaation using ultrasound; COLPOS model; relationships between physical fractions; size and mass of soil particles.

        · abstract in Spanish     · text in Spanish