Soil functions are general capabilities of soils that are important for various agricultural, environmental, nature protection, landscape architecture and urban applications. Soil can perform many functions and these include functions related to the natural ecosystems, agricultural productivity, environmental quality, source of raw material, and as base for buildings.
Six key soil functions are:
Food and other biomass production
Environmental Interaction
Biological habitat and gene pool
Source of raw materials
Physical and cultural heritage
Platform for man-made structures
Soil acts as an anchor for plant roots. It provides a hospitable place for a plant to live in while storing and supplying nutrients to plants. Soil also functions by maintaining the quantity and quality of air by allowing CO2 to escape and fresh O2 to enter the root zone. Pore spaces within soil can also absorb water and hold it until plant roots need it. The soil also moderates temperature fluctuation, providing a suitable temperature for the roots to function normally. A fertile soil will also provide dissolved mineral nutrients for optimal plant growth. The combination of these activities supports plant growth for providing food and other biomass production.
Environmental interactions such as regulating water supplies, water loos, utilization, contamination, and purification are all affected by the soil. They can filter, buffer, and transform materials between the atmosphere, the plant cover, and the water table. Soil interacts with the environment to transform and decompose waste materials in to new materials. Through filtering, soil acts as a filter and captures contaminants through soil particles. Contaminants are captured by the soil particles and water comes out cleaner in the aquifers and rivers. Lastly, it can accumulate large amounts of carbon as soil organic matter, thus reducing the total concentration of carbon dioxide that can mitigate global climate change.
Soils also acts as a biological habitat and a gene reserve for a large variety of organisms.
Cette page est générée automatiquement et peut contenir des informations qui ne sont pas correctes, complètes, à jour ou pertinentes par rapport à votre recherche. Il en va de même pour toutes les autres pages de ce site. Veillez à vérifier les informations auprès des sources officielles de l'EPFL.
Le cours est une introduction aux Sciences du sol. Il a pour but de présenter les principales caractéristiques, propriétés et fonctions des sols. Il fait appel à des notions théoriques mais également
Soil organic matter (SOM) is the organic matter component of soil, consisting of plant and animal detritus at various stages of decomposition, cells and tissues of soil microbes, and substances that soil microbes synthesize. SOM provides numerous benefits to the physical and chemical properties of soil and its capacity to provide regulatory ecosystem services. SOM is especially critical for soil functions and quality.
La science des sols, (soil science en anglais), est l'ensemble des disciplines scientifiques concernant les sols de la surface terrestre. Les deux branches principales de la science des sols sont : la pédologie, qui étudie la formation (pédogenèse) et l'évolution des sols ; l'édaphologie, qui étudie l'influence des sols sur les êtres vivants, particulièrement en tant qu'habitats naturels pour les végétaux (l'agrologie portant plus spécifiquement sur l'étude des seuls sols agricoles).
vignette|Le sol recèle un trésor vivant insoupçonné qui représente 50 % de la biodiversité spécifique sur la terre. En région tempérée, chaque mètre carré (sur de profondeur) abrite en moyenne animales (dont un millier d'espèces d'invertébrés constitués de près de 50 % d'acariens) comprenant, en les distinguant par leur taille, la microfaune, la mésofaune et la macrofaune. Une cuillère à café de sol, soit environ un gramme, héberge en moyenne 100 arthropodes, à , des millions de protozoaires et près d'un milliard de cellules bactériennes, issues de plus de 1 million d'espèces.
In the pursuit of a carbon-neutral chemical industry, minimizing fossil feedstock consumption while integrating renewable carbon sources is imperative. Surfactants, inherently amphiphilic, pose challenges in separation and recovery processes. Given their e ...
Reduction-oxidation (redox) reactions underlie essentially all biogeochemical cycles. Like most soil properties and processes, redox is spatiotemporally heterogeneous. However, unlike other soil features, redox heterogeneity has yet to be incorporated into ...
Hydrological and climatic modeling of near-surface water and energy fluxes is critically dependent on the availability of soil hydraulic parameters. Key among these parameters is the soil water characteristic curve (SWCC), a function relating soil water co ...