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Terms for subject Environment containing soil | all forms | exact matches only
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acidification of soilÜbersäuerung des Bodens
Act containing temporary regulations concerning remedial action in cases of soil contaminationInterimgesetz Bodensanierung
aggressive soil conditionsagressive Bodeneigenschaften
agreements on soilVereinbarungen zur Bodenschutzproblematik
alkali soil Soil that contains sufficient exchangeable sodium to interfere with water penetration and crop growth, either with or without appreciable quantities of soluble saltsAlkalischer Boden
alkali soilAlkalischer Boden
artificial soilkünstlicher Boden
bacterial and fungal flora of the soilBakterien- und Pilzflora des Bodens
basement soilUrgesteinsboden
biological percolator soilbiologischer Rasen
biological percolator soilTropfkörperrasen
block cotton soilRegur
buffer ability of the soilPuffervermoegen des Bodens
buffering capacity of the soilPufferungsvermögen des Bodens
clean soilsanierter Boden
clean soildekontaminierter Boden
contaminated soilVerunreinigter Boden
contaminated soil Soil which because of its previous or current use has substances under, on or in it which, depending upon their concentration and/or quantity, may represent a direct potential or indirect hazard to man or to the environmentVerunreinigter Boden
contaminated soilbelasteter Boden
contaminated soilskontaminierte Böden
decontaminated soildekontaminierter Boden
decontaminated soilsanierter Boden
degradation of soilDegradation
degraded soilgeschädigter Boden
degraded soilverbrauchte Erde
degraded soilverödetes Land
deposit of humus soilHumusbildung
deposit of humus soilBildung einer Humusschicht
deterioration of soil structure through the impact of rainVerschlämmung der Bodenoberfläche durch aufschlagenden Regen
dynamics of soil organic matterHumusdynamik
dynamics of soil organic matter systemHumusdynamik
emissions to land and soilEinträge in den Boden
European Soil CharterEuropäische Bodencharta
European Soils BureauEuropäisches Büro für Böden
European Topic Centre on SoilETC/Bodenschutz
excavated soilErdaushub
heath soilHeideboden
improving soil porosityVerbesserung der Bodenporosität
in situ soil ventingExtraktion von flüchtigen Schadstoffen aus der Erde
injected soilInjektionswand
intergrade soilÜbergangsboden
landfill soilDeponieboden
lateritic soilLaterit
lateritic soilLatosol
marine soilMeeresboden
mobile soil cleaning plantmobile Bodensanierungsanlage
multifunctionality of the soilMultifunktionalität des Bodens
natural regenerative capacity of soilsSelbstreinigungskraft der Böden
night soilFäkalien
organic soil improverorganisches Bodenverbesserungsmittel
paddy soilReisboden
plasticity of soilBodenplastizität
ploughing virgin soilNeuland aufreißen
ploughing virgin soilNeulandgewinnung
ploughing virgin soilRoden
ploughing virgin soilRodung
ploughing virgin soilUrbarmachung
ploughing virgin soilWaldrodung
predicted environmental concentration in soilvoraussichtliche Umweltkonzentration im Boden
protection of soils and groundwatersSchutz des Bodens und des Grundwassers
purification capacity of the soilReinigungsvermoegen des Bodens
purification through the soil The act or process in which a section of the ground is freed from pollution or any type of contamination, often through natural processesReinigung durch den Boden
purification through the soilReinigung durch den Boden
regeneration soil heapSanierungsmiete
regeneration soil heapRegenerationsmiete
release of any polluting substance into soilFreisetzen von Schadstoffen in den Boden
salting of soilÜbersalzung des Bodens
sodic soilNatriumboden
soil accumulationAkkumulation im Boden
soil acidification A naturally occurring process in humid climates that has long been the subject of research, whose findings suggest acid precipitation effects. The generally accepted impact of soil acidification on the productivity of terrestrial plants is summarised as follows: as soil becomes more acidic the basic cations (Ca, Mg) on the soil exchange are replaced by hydrogen ions or solubilized metals. The basic cation, now in solution, can be leached through the soil. As time progresses the soil becomes less fertile and more acidic. Resultant decreases in soil pH cause reduced, less-active population of soil microorganisms, which in turn slow decomposition of plant residues and cycling of essential plant nutrientsBodenversauerung
soil air The air and other gases in spaces in the soil; specifically that which is found within the zone of aeration. Also known as soil atmosphereBodenluft
soil air withdrawalBodenluftentnahme
soil amendmentBodenverbesserer
soil analysis The use of rapid chemical analyses to determine the fertility status of a soil. It is used to identify those nutrients or substances that are present in either insufficient or excessive quantities for optimum plant growth. Analyses are also used to monitor increases or decreases in soil fertility over timeBodenuntersuchung
soil analysisBodenuntersuchung
soil-and air-hygieneBundesanstalt für Wasser-
soil-and air-hygieneBoden-und Lufthygiene
soil and climate conditionsBoden- und Klimaverhältnisse
soil and dredging spoilErde und Hafenaushub
soil and stonesErde und Steine
soil and water conservationBoden- und Wasserschutz
soil bacteriaBodenbakterie
soil-bentonite wallZweiphasendichtwand
soil biology The study of the living organisms, mainly microorganisms and microinvertebrates which live within the soil, and which are largely responsible for the decomposition processes vital to soil fertilityBodenbiologie
soil breathing rateBodenatmungsrate
soil capability The suitability of soils for various uses, e.g. sustained production of cultivated crops, pasture plants, etc., depending on depth, texture, kinds of minerals, salinity, kinds of salts, acidity, etc.Bodennutzbarkeit
soil capabilityBodennutzbarkeit
soil carbon sequestrationKohlenstoffbindung im Boden
soil carbon sequestrationBindung von Kohlendioxid im Boden
soil carbon sequestration capacityKohlenstoffspeicherkapazität des Bodens
soil carbon sequestration capacitySpeicherkapazität des Bodens für C02
soil carbon sequestration capacityKohlenstoffdioxid-Speicherkapazität des Bodens
soil carbon stockCOsub2sub-Vorratskapazität der Böden
soil chemistry The study of the inorganic and organic components of the soil and its life cyclesBodenchemie
Soil Cleaning Interim ActInterimgesetz Bodensanierung
soil colloidBodenkolloid
soil colloidKolloid
soil compaction An increase in bulk density (mass per unit volume) and a decrease in soil porosity resulting from applied loads, vibration, or pressure. More compacted soils (or other materials) can support greater loads (load-bearing capacity). Bulk density can be increased by controlling the moisture content, compaction forces and treatment procedures, as well as by manipulating the type of material being compactedBodenverdichtung
soil condition Description of the character of the surface of the ground at the time of observation, especially in relation to the influence of rain and snowBodenzustand
soil conditionerBodenverbesserer
soil conservation Management of soil to prevent or reduce soil erosion and depletion by wind and water. Preservation of soil against deterioration and loss by using it within its capabilities; application of conservation practices needed for its protection and improvementBodenschutz
soil conservation legislation A binding rule or body of rules prescribed by a government to protect and prevent the loss of an area's surface layer of decomposed rock and organic material, valued for its nutrients and ability to support lifeBodenschutzrecht
soil contaminationBodenverseuchung
soil damage Soil impaired as a consequence of human activity. A study financed by UNEP, reporting in 1992, found that about 10,5% of the world's vegetative surface had been seriously damaged by human activity since 1945. The study found that much of the damage had been masked by a general rise in global agricultural productivity resulting from expanded irrigation, better plant varieties, and greater use of production inputs, such as fertilizers and pesticides. More than 1/3 of the damaged land was in Asia, almost 1/3 in Africa, and 1/4 in Central America. Some land had been damaged beyond restoration. The greatest sources of soil degradation were overgrazing, unsuitable agricultural practices, and deforestationBodenschädigung
soil decontaminationBodendekontamination
soil decontaminationBodensanierung
soil decontamination Technologies employed in the removal of PCBs, PAH, pesticides and, more generally, of organic compounds by physical, chemical or biological treatmentsBodendekontamination
soil decontaminationBodenreinigung
soil decontaminationEntgiftung von Böden
soil degradationBodendegradation
soil degradationVerschlechterung der Böden
soil degradationZustand der Böden
soil degradationLandverödung
soil degradationBodenverarmung
soil degradationBodenverschlechterung
soil degradation Soil may deteriorate either by physical movement of soil particles from a given site or by depletion of the water-soluble elements in the soil which contribute to the nourishment of crop, plants, grasses, trees, and other economically usable vegetation. The physical movement generally is referred to as erosion. Wind, water, glacial ice, animals and tools in use may be agents of erosionBodendegradation
soil degradationDegradation der Böden
soil depletionBodenverheerung
soil deteriorationBodenverschlechterung
soil deteriorationBodenverarmung
soil deteriorationLandverödung
soil dissipationBodenabbau
soil-eaterGeophage
soil-eaterErdeesser
soil erosion Detachment and movement of topsoil or soil material from the upper part of the profile, by the action of wind or running water, especially as a result of changes brought about by human activity, such as unsuitable or mismanaged agricultureBodenerosion
soil erosionBodenverheerung
Soil erosion and land resources projectProjekt Bodenerosion und Landressourcen
soil exhaustionBodenmüdigkeit
soil exhaustionBodenermüdung
soil fabricGefüge
soil fabricBodenstruktur
soil fertilisation The application of any organic or inorganic material of natural or synthetic origins to a soil to supply one or more elements essential to the growth of plantsDüngung
soil fertilisationDüngung
soil fertility The status of a soil with respect to the amount and availability to plants of elements necessary for plant growthBodenfruchtbarkeit
soil filterBodenfilter
soil flushingBodenreinigung
soil flushingBodenwaesche
soil formation The combination of natural processes by which soils are formed. It is also known as pedogenesis. The most important soil-forming factors are parent material, terrain, climate, aspect, vegetation cover, microorganisms in the soil and the age of the land surface. Some pedologists would add to this list the influence of human activities. All the factors exhibit varying degrees of interrelationship and some are more important than others, with climate often being singled out as the most importantBodenbildung
soil from cleaning and washing beetErde aus der Waesche und Reinigung von Zuckerrueben
soil function The main soil function is participation in the material transformation and migrating processes occurring in the natural environment on which the functioning of ecosystems depends. The most active participants in the occurring processes are microorganisms and invertebrates, whose activity, different variety, complex structure, and abundance accurately reflect the soil type and its characteristics: so they are important indicators of ecological stability. The variety of soil organisms determine its self-regulatory and self-cleaning capacityBodenfunktion
soil functionBodenfunktion
soil functionsBodenfunktionen
soil heapRegenerationsmiete
soil heapSanierungsmiete
soil hygieneBodenhygiene
soil improvement Process of protecting the soil from excessive erosion and making soil more fertile and productiveBodenverbesserung
soil improvement materialBodenverbesserer
soil improvement materialBodenverbesserungsmittel
soil improverBodenverbesserer
soil improverBodenverbesserungsmittel
soil investigationBodenuntersuchung
soil layer Distinctive successive layers of soil produced by internal redistribution processes. Conventionally the layers have been divided into A, B and C horizons. The A horizon is the upper layer, containing humus and is leached and/or eluviated of many minerals. The B horizon forms a zone of deposition and is enriched with clay minerals and iron/aluminium oxides from the A layer. The C layer is the parent material for the present soil and may be partially weathered rock, transported glacial or alluvial material or an earlier soilBodenschicht
soil leaching The removal of water or any soluble constituents from the soil. Leaching often occurs with soil constituents such as nitrate fertilizers with the result that nitrates end up in potable watersBodenauslaugung
soil leachingBodenauslaugung
soil lifeBodenleben
soil lifeLeben im Boden
soil loading In soil mechanics and civil engineering the term is used to denote the increased weight brought to bear on the ground surfaceBodenbelastung
soil loadingBodenbelastung
soil lossBodenerosion
soil lossBodenverlust
soil lossBodenabtrag
soil loss equationBodenverlustgleichung
soil loss equationBodenabtragsgleichung
soil map A two-dimensional representation that shows the areal extent or the distribution of soils in relation to other features of the land surfaceBodenkarte
soil materialBodenmaterial
soil mechanics The study of the physical properties of soil, especially those properties that affect its ability to bear weight such as water content, density, strength, etc.Bodenmechanik
soil mineralBodenmineral
soil mineralogy Study of the formation, occurrence, properties, composition, and classification of the minerals present in the soilBodenmineralogie
soil mineralogyBodenmineralogie
soil moisture 1. Water stored in soils. 2. One of the most important elements involved in pedological processes and plant growth. There are three basic forms: 1. water adhering in thin films by molecular attraction to the surface of soil particles and not available for plants is termed hygroscopic water. 2. Water forming thicker films and occupying the smaller pore spaces is termed capillary water. Since it is held against the force of gravity it is permanently available for plant growth and it is this type of soil water which contains plant nutrients in solution. 3. Water in excess of hygroscopic and capillary water is termed gravitational water, which is of a transitory nature because it flows away under the influence of gravity. When the excess has drained away the amount of water retained in the soil is termed its field capacity, when some of its pore spaces are still free of waterBodenfeuchtigkeit
soil moisture regime The water regime of the soil is determined by the physical properties and arrangement of the soil particles. The pores in a soil determine its water-retention characteristics. When all the pores are full of water, the soil is said to be saturatedBodenwasserhaushalt
soil moisture regimeBodenwasserhaushalt
soil moisture tensionWasserspannungsmesser
soil moisture tensionWasserspannung
soil monolithBodenmonolith
soil on pleistocene sedimentsDiluvialboden
soil organic carbonorganischer Kohlenstoff im Boden
soil organismBodenorganismen
soil organism Organisms which live in the soilBodenorganismen
soil particlesBodenteilchen
soil permeabilityDurchlässigkeit
soil photolysisPhotolyse im Boden
soil pollutant Solid, liquid and gaseous substances that detrimentally alter the natural condition of the soilBodenschadstoff
soil pollutantBodenschadstoff
soil pollutantbodenverunreinigende Stoffe
soil pollution Modifications of soil features or, more generally, of its chemical and biological balance, caused by the discharge of polluting substancesBodenverunreinigung
soil pollutionBodenverunreinigung
soil poreBodenpore
soil porosityBodenporosität
soil preparationBodenvorbereitung
soil preparationBodenaufbereitung
soil process The major processes in soils are gains, losses, transfers, and transformations of organic matter, soluble salts, carbonates, silicate clay minerals, sesquioxides, and silica. Gains consist normally of additions of organic matter, and of oxygen and water through oxidation and hydration, but in some sites slow continuous additions of new mineral materials take place at the surface or soluble materials are deposited from groundwater. Losses are chiefly of materials dissolved or suspended in water percolating through the profile or running off the surfaceBodenprozeß
soil processBodenprozeß
soil profile A vertical section of a soil, showing horizons and parent materialBodenprofil
soil profileBodengestaltung
Soil Protection ActBodenschutzgesetz
soil purificationBodenreinigung
soil purificationBodendekontamination
soil purificationBodensanierung
soil quality All current positive or negative properties with regard to soil utilization and soil functionsBodengüte
soil resourceBodenressourcen
soil resource No definition neededBodenressourcen
soil salination The accumulation of soluble mineral salts near the surface of soil, usually caused by the capillary flow of water from saline ground water. Where the rate of surface evaporation is high, irrigation can exacerbate the problem by moistening the soil and causing water to be drawn from deeper levels as water evaporates from the surface. The evaporation of pure water leaves the salts behind, allowing them to accumulate, and they can reach concentrations that are toxic to plants, thus sterilizing the landBodenversalzung
soil salinity Measurement of the quantity of mineral salts found in a soil. Many semi-arid and arid areas are naturally salty. By definition they are areas of substantial water deficit where evapotranspiration exceeds precipitation. Thus, whereas in humid areas there is sufficient water to percolate through the soil and to leach soluble materials from the soil and the rocks into the rivers and hence into the sea, in deserts this is not the case. Salts therefore tend to accumulateSalzgehalt des Bodens
soil salinitySalzgehalt des Bodens
soil science The study of the properties, occurrence, and management of soil as a natural resource. Generally it includes the chemistry, microbiology, physics, morphology, and mineralogy of soils, as well as their genesis and classificationBodenkunde
soil sciencePedologie
soil sealingBodenversiegelung
soil settling Compaction involves the close-packing of the individual grains mainly by the elimination of pore-space and expulsion of entrapped water; this is normally brought about by the weight of the overlying sedimentsBodensetzung
soil settlingBodensetzung
soil settling velocityBodensetzungsgeschwindigkeit
soil solutionBodenlösung
soil stabilisation Chemical or mechanical treatment designed to increase or maintain the stability of a soil mass or otherwise to improve its engineering properties, as by increasing its shear strength, reducing its compressibility, or decreasing its tendency to absorb water. Stabilization methods include physical compaction and treatment with cement, lime, and bitumenBodenverfestigung
soil stability Soil stability depends on its shear strength, its compressibility and its tendency to absorb water. Stabilization methods include physical compaction and treatment with cement, lime, and bitumenBodenstabilität
soil stabilityBodenstabilität
soil standardBodenstandardwert
soil sterilizationBodensterilisierung
soil including excavated soil from contaminated sites, stones and dredging spoilErde und Hafenaushub
soil stress limitBodenbelastbarkeit
soil structure The combination or aggregation of primary soil particles into aggregates or clusters, which are separated from adjoining peds by surfaces of weakness. Soil structure is classified on the basis of size, shape, and distinctness into classes, types, and gradesBodenstruktur
soil structureGefüge
soil subsidence A sinking down of a part of the earth's crust, generally due to underground excavationsBodensenkung
soil surface sealing Any activity or process in which ground surface areas are packed or plugged to prevent percolation or the passage of fluidsBodenversiegelung
soil surface sealingBodenversiegelung
soil temperatureBodentemperatur
soil texture 1. Refers to the relative proportions of the various size groups (sand, silt and clay) of the individual soil grains in a mass of soil. 2. Classification of soil by the proportion and graduations of the three size groups of soil grains, i.e., sand, silt and clay, present in the soilBodentextur
soil type A phase or subdivision of a soil series based primarily on texture of the surface soil to a depth at least equal to plow depth (about 15 cm)Bodenart
soil typeBodentextur
soil useBodennutzung
soil use Functional utilization of soil for agriculture, industry, or residential building purposesBodennutzung
soil use regimeBodennutzungssystem
soil use regime Type of management and utilization of the soilBodennutzungssystem
soil vacuum extractionExtraktion von flüchtigen Schadstoffen aus der Erde
soil vapor extractionExtraktion von flüchtigen Schadstoffen aus der Erde
soil washingBodenreinigung
soil washingBodenwaesche
soil water Water stored in soilsBodenwasser
stability of the soilBodenfestigkeit
steppe soilSteppe
steppe soilSteppenboden
substances hazardous to soilbodengefaehrdende Stoffe
Substances,Soil and Biotechnology DivisionAbteilung Stoffe,Boden,Biotechnologie
surface of the soil particlesOberflaeche der Bodenpartikel
sustainable management of the soilnachhaltige Bewirtschaftung der Böden
top soil coverOberbodenabdeckung
transition soilÜbergangsboden
treated soilbehandelter Boden
unpolluted soilunverschmutzter Boden
working the soilBodenbearbeitung
working the soil Ploughing the soil for agricultural purposesBodenbearbeitung