[article]
| Titre : |
Re-thinking the conservation of carbon, water and soil: a different perspective |
| Type de document : |
Article |
| Auteurs : |
Thomas Shaxson |
| Année de publication : |
2006 |
| Article en page(s) : |
p. 9-19 |
| Langues : |
Anglais (eng) |
| Catégories : |
[Motbis 2025] carbone [Motbis 2025] perméabilité
|
| Note de contenu : |
Sustaining soil productivity requires continuing actions of soil organisms on organic materials for optimizing of soil porosity and of movements of roots, water and gases in the root-zone. Soil is more quickly formed and self-renewed from the top downwards than only by slow additions from the bottom upwards. Loss of porosity diminishes soil's infiltration capacity and water-holding potential. Factors that provide insufficient organic substrates for soil organisms and that unduly accelerate oxidation of soil organic matter hinder the self-recuperation of soil and facilitate 'Stage-1' loss of carbon from within soil aggregates. They predispose the soil to lose rapidly even more carbon, in particulate form, through 'Stage-2' losses during consequent processes of runoff and erosion. Forms of land use and management are advocated that favor the functioning of soil-inhabiting organisms, including plants, such that carbon's capture in photosynthesis is increased, its usefulness in the soil as a rooting medium is prolonged, and its subsequent immobilization in the process of sequestration ameliorates the rate of increase in carbon dioxide concentration in the global atmosphere. |
in Agronomy for Sustainable Development * > Vol.26, n°1 [01/01/2006] . - p. 9-19
[article] Re-thinking the conservation of carbon, water and soil: a different perspective [Article] / Thomas Shaxson . - 2006 . - p. 9-19. Langues : Anglais ( eng) in Agronomy for Sustainable Development * > Vol.26, n°1 [01/01/2006] . - p. 9-19
| Catégories : |
[Motbis 2025] carbone [Motbis 2025] perméabilité
|
| Note de contenu : |
Sustaining soil productivity requires continuing actions of soil organisms on organic materials for optimizing of soil porosity and of movements of roots, water and gases in the root-zone. Soil is more quickly formed and self-renewed from the top downwards than only by slow additions from the bottom upwards. Loss of porosity diminishes soil's infiltration capacity and water-holding potential. Factors that provide insufficient organic substrates for soil organisms and that unduly accelerate oxidation of soil organic matter hinder the self-recuperation of soil and facilitate 'Stage-1' loss of carbon from within soil aggregates. They predispose the soil to lose rapidly even more carbon, in particulate form, through 'Stage-2' losses during consequent processes of runoff and erosion. Forms of land use and management are advocated that favor the functioning of soil-inhabiting organisms, including plants, such that carbon's capture in photosynthesis is increased, its usefulness in the soil as a rooting medium is prolonged, and its subsequent immobilization in the process of sequestration ameliorates the rate of increase in carbon dioxide concentration in the global atmosphere. |
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