Research news on soil formation

Soil formation, or pedogenesis, is the set of physical, chemical, and biological processes that transform unconsolidated parent material into structured soil profiles. It is governed by five classic soil-forming factors: climate, organisms (including vegetation and microbes), relief (topography), parent material, and time. Key mechanisms include weathering of minerals, organic matter accumulation and decomposition, eluviation and illuviation of clays and solutes, and aggregation into distinct horizons (O, A, E, B, C). These processes control soil texture, structure, porosity, pH, nutrient availability, and horizon differentiation, thereby determining soil classification and function in terrestrial ecosystems.

Marsh soils: Biodiversity fostered by self-organization

In the heart of the Marais Poitevin regional nature park, the second-largest wetland in France, a scientific team led by a CNRS researcher has demonstrated the ability of clay soils to self-organize into geometric patterns. ...

From fragile to fertile: The science behind sandy soil recovery

It's soil that slips through your fingers—loose, dry and stubbornly unproductive. Stretching across large parts of South Australia and western Victoria, sandy soils have long resisted conventional farming methods. They shed ...