-
1 влажность почвы
влажность почвы
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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:
a) water adhering in thin films by molecular attraction to the surface of soil particles and not available for plants is termed hygroscopic water.
b) 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.
c) 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 water.
(Source: LANDY / DUNSTE)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > влажность почвы
-
2 почвенная вода
почвенная вода
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
soil water
Water stored in soils. (Source: LANDY)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > почвенная вода
-
3 уровень стояния грунтовых вод
уровень стояния грунтовых вод
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
water table
Water that occupies pores, cavities, cracks and other spaces in the crustal rocks. It includes water precipitated from the atmosphere which has percolated through the soil, water that has risen from deep magmatic sources liberated during igneous activity and fossil water retained in sedimentary rocks since their formation. The presence of groundwater is necessary for virtually all weathering processes to operate. Phreatic water is synonymous with groundwater and is the most important source of any water supply. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > уровень стояния грунтовых вод
-
4 абиотическая среда
абиотическая среда
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
abiotic environment
The non-living components of the environment (rocks, minerals, soil, water and climate). (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > абиотическая среда
-
5 водный баланс почвы
водный баланс почвы
Алгебраическая сумма прихода и расхода воды в почве за выбранный интервал времени и для определенного слоя почвы.
[ ГОСТ 17713-89]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > водный баланс почвы
-
6 водный режим почвы
водный режим почвы
Временное и пространственное изменение составляющих водного баланса почвы.
[ ГОСТ 17713-89]Тематики
Синонимы
- Rw
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > водный режим почвы
-
7 почвенные воды
почвенные воды
Временные скопления капельно-жидких вод в почвенной толще на слабопроницаемых слоях, гидравлически не связанные с нижележащими водоносными пластами.
[ ГОСТ 19179-73]Тематики
Обобщающие термины
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > почвенные воды
-
8 природный ресурс
природный ресурс
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
natural resource
A feature or component of the natural environment that is of value in serving human needs, e.g. soil, water, plantlife, wildlife, etc. Some natural resources have an economic value (e.g. timber) while others have a "noneconomic" value (e.g. scenic beauty). (Source: UNUN)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > природный ресурс
-
9 водная эрозия
водная эрозия
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
water erosion
The breakdown of solid rock into smaller particles and its removal by water. As weathering, erosion is a natural geological process, but more rapid soil erosion results from poor land-use practices, leading to the loss of fertile topsoil and to the silting of dams, lakes, rivers and harbours. There are three classes of erosion by water. a) Splash erosion occurs when raindrops strike bare soil, causing it to splash, as mud, to flow into spaces in the soil and to turn the upper layer of soil into a structureless, compacted mass that dries with a hard, largely impermeable crust. b) Surface flow occurs when soil is removed with surface run-off during heavy rain. c) Channelized flow occurs when a flowing mixture of water and soil cuts a channel, which is then deepened by further scouring. A minor erosion channel is called a rill, a larger channel a gully. (Source: ALL)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > водная эрозия
-
10 режим влажности почвы
режим влажности почвы
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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 saturated. (Source: DUNSTE)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > режим влажности почвы
-
11 сельскохозяйственные работы, осуществляемые по контуру
сельскохозяйственные работы, осуществляемые по контуру
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
contour farming
The performing of cultivations along lines connecting points of equal elevation so reducing the loss of top soil by erosion, increasing the capacity of the soil to retain water and reducing the pollution of water by soil. (Source: ALLa)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > сельскохозяйственные работы, осуществляемые по контуру
-
12 сельскохозяйственные машины
сельскохозяйственные машины
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
agricultural machinery
Machines utilized for tillage, planting, cultivation and harvesting of crops. Despite its benefits in increasing yields, mechanisation has clearly had some adverse environmental effects: deep ploughing exposes more soil to wind and water erosion; crop residues can be removed as opposed to ploughing back into the soil; removal of residues can lead to a serious loss of organic content in the soil, which may increase the risk of soil erosion. (Source: MGH / DOBRIS)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > сельскохозяйственные машины
-
13 почвенный процесс
почвенный процесс
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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 surface. (Source: PARCOR)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > почвенный процесс
-
14 почвенная механика
почвенная механика
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: CED)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > почвенная механика
-
15 щелочная почва
щелочная почва
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
alkali soil
Soil that contains sufficient exchangeable sodium to interfere with water penetration and crop growth, either with or without appreciable quantities of soluble salts. (Source: LANDY)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > щелочная почва
-
16 ухудшение качества пресных вод
ухудшение качества пресных вод
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
freshwater degradation
Pollution immediately or eventually involves the hydrological cycle of the earth, because even pollutants emitted into the air and those present in the soil are washed out by precipitation. Water is considered polluted when it is altered in composition or condition so that it becomes less suitable for any or all of the functions and purposes for which it would be suitable in its natural state. This definition includes changes in the physical, chemical and biological properties of water, or such discharges of liquid, gaseous or solid substances into water as will or are likely to create nuisances or render such water harmful to public health, safety or welfare, or to domestic, commercial, industrial, agricultural, fish or other aquatic life. It also includes changes in temperatures, due to the discharge of hot water. (Source: WPR)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > ухудшение качества пресных вод
-
17 воздействие производства энергии на окружающую среду
воздействие производства энергии на окружающую среду
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
environmental impact of energy
Energy and environmental problems are closely related, since it is nearly impossible to produce, transport, or consume energy without significant environmental impact. The environmental problems directly related to energy production and consumption include air pollution, water pollution, thermal pollution, and solid waste disposal. The emission of air pollutants from fossil fuel combustion is the major cause of urban air pollution. Diverse water pollution problems are associated with energy usage. One major problem is oil spills. In all petroleum-handling operations, there is a finite probability of spilling oil either on the earth or in a body of water. Coal mining can also pollute water. Changes in groundwater flow produced by mining operations often bring otherwise unpolluted waters into contact with certain mineral materials which are leached from the soil and produce an acid mine drainage. Solid waste is also a by-product of some forms of energy usage. Coal mining requires the removal of large quantities of earth as well as coal. In general, environmental problems increase with energy use and this combined with the limited energy resource base is the crux of the energy crisis. An energy impact assessment should compare these costs with the benefits to be derived from energy use. (Source: RAU)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > воздействие производства энергии на окружающую среду
-
18 просачивание воды
просачивание воды
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
water seepage
The slow movement of water through small openings and spaces in the surface of unsaturated soil into or out of a body of surface or subsurface water. (Source: MGH)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > просачивание воды
-
19 фильтрованная вода
фильтрованная вода
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
seepage water
Water that moves slowly through small openings of a porous material such as soil or the amount of water that has been involved in seepage. (Source: BJGEO)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > фильтрованная вода
-
20 охраняемая территория вокруг источника питьевой воды
охраняемая территория вокруг источника питьевой воды
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
drinking water protection area
Area surrounding a water recovery plant in which certain forms of soil utilization are restricted or prohibited in order to protect the groundwater. (Source: AZENP)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > охраняемая территория вокруг источника питьевой воды
См. также в других словарях:
soil water — dirvožemio drėgnis statusas T sritis ekologija ir aplinkotyra apibrėžtis Drėgmės procentinis kiekis dirvožemio masėje arba tūryje. Pagal raiškos būdą būna svorinis (drėgmės kiekis masės procentais) ir tūrinis (drėgmės kiekis tūrio procentais).… … Ekologijos terminų aiškinamasis žodynas
soil water — dirvožemio vanduo statusas T sritis ekologija ir aplinkotyra apibrėžtis Dirvožemio skystoji fazė – vanduo su jame ištirpusiomis mineralinėmis, organinėmis medžiagomis ir dujomis. Iš jo augalai įsisavina maisto medžiagas. Augalų mitybai ir augimui … Ekologijos terminų aiškinamasis žodynas
Soil water (retention) — Soils can process and contain considerable amounts of water. They can take in water, and will keep doing so until they are full, or the rate at which they can transmit water into, and through, the pores is exceeded. Some of this water will… … Wikipedia
soil-water pressure — The pressure (positive or negative), in relation to the external gas pressure on the soil water, to which a solution identical in composition with the soil water must be subjected in order to be in equilibrium through a porous permeable wall… … Lexicon of Cave and Karst Terminology
soil water — See soil moisture … Lexicon of Cave and Karst Terminology
total soil-water potential — The sum of the energy related components of a soil water system; i.e., the sum of the gravitational, matric, and osmotic components [22] … Lexicon of Cave and Karst Terminology
Water content — Soil composition by phase: s soil (dry), v void (pores filled with water or air), w water, a air. V is volume, M is mass. Water content or moisture content is the quantity of water contained in a material, such as soil (called soil moisture),… … Wikipedia
Soil pH — is the pH of soil water. It is based on the measurement of pH, which depends on the activity of hydrogen ions (H+) in a solution.There are many different methods to collect soil water, all which influence the measured soil pH in one way or… … Wikipedia
Soil structure — is determined by how individual soil granules clump or bind together and aggregate, and therefore, the arrangement of soil pores between them. Soil structure has a major influence on water and air movement, biological activity, root growth and… … Wikipedia
Water retention curve — is the relationship between the water content, θ, and the soil water potential, ψ. This curve is characteristic for different types of soil, and is also called the soil moisture characteristic.It is used to predict the soil water storage, water… … Wikipedia
Water potential — is the potential energy of water per unit volume relative to pure water in reference conditions. Water potential quantifies the tendency of water to move from one area to another due to osmosis, gravity, mechanical pressure, or matrix effects… … Wikipedia