Les sols forestiers

Les sols forestiers

Les sols forestiers couverts par des forêts de production occupent 15,9 millions d’hectares (Mha) en 2015 (IGN/IFN, campagnes 2013 à 2017), soit 28 % de la surface de la France métropolitaine.

Forest soils covered by production forests occupy 15.9 million hectares (Mha) in 2015 (IGN/IFN, campaigns 2013 to 2017), representing 28% of metropolitan France's surface area.
2 chapters
  • Humus
    • In forest environments, humus—layers of dead plant fragments in various stages of decomposition—are closely linked to soil types. In 2015, nearly half of forest soils, brunified soils (7.4 Mha), are generally moderately acidic and highly aerated due to intense activity of fauna and microorganisms (Corsica, Massif Central, Pyrenees, Vosges). Conversely, excess water in valley soils (2.5 Mha) slows biological activity, hinders plant rooting, and constrains forestry operations. Humus in these two soil types consists of a litter layer of dead leaves when they are evolved and highly fertile (mull and dysmull), or more rarely a dark brown layer of fine organic matter and litter from previous years (moder).
    • Soils from calcareous rocks associated with carbonated humus predominate in the Paris Basin, the Alps, and the Mediterranean (2.3 Mha). Nutritional constraints may hinder the development of certain species, such as Scots pine and maritime pine, Douglas fir, or chestnut. Very acidic and poor soils (1.3 Mha) have developed on the most acidic sandy substrates (Gascony Moors, Sologne, sandstone Vosges, etc.). Generally, the organic layers of their humus are even thicker (dysmoder, mor).
    Humus types in production forest excluding poplar plantations Illustration 108 - Humus types in production forest excluding poplar plantations
  • Water availability of species as indicated by forest soil flora
    Soil properties determine the development and growth of forest stands by affecting their rooting, nutrient uptake, and water supply. Rainfall and water stored in soil provide trees with water. When during drought conditions the soil's usable water reserve falls below a given threshold (40% of maximum reserve for an adult maritime pine for example), the tree reduces its photosynthetic activity and thus its growth.
    Water availability of species as indicated by forest soil flora Illustration 110
    • A quarter of French forest stands (4.1 Mha) experience water deficit linked to climate (Mediterranean) or low soil water reserves (xerorhine or xerophile environments). This applies to three-quarters of the Mediterranean ecological region. Its soils are also particularly exposed to erosion, a risk heightened by fires in summer and autumn. Forests in dry environments are also found in Corsica, along the Atlantic coast (southwest), in the Causses, eastern Pyrenees, southern Alps and Jura, and on Burgundian plateaus.
    • Conversely, excess water in riparian soils or linked to water tables perched on impermeable ground favors species adapted to wet environments (hygrophile or mesohygrophile). Forest stands developing under these conditions are particularly productive (6.4 m³/ha/year). They occupy 0.8 Mha, or 5% of French forest.

Further reading

  • Inventaire forestier nationalinventaire-forestier.ign.fr

    Placé sous la tutelle des ministres chargés du développement durable et des forêts, l’inventaire forestier national est une des missions de l’Institut national de l’information géographique et forestière (IGN).