Übersetzung für 'vadose zone' von Englisch nach Deutsch

vadose zone [unsaturated zone]

Aerationszone {f} [ungesättigte Bodenzone]geol.

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vadose {adj}

vadosgeol.

Werbung

zone constant angular velocity <zone CAV, Z-CAV, ZCAV>

Zone CAV {f} <Z-CAV, ZCAV>comp.

zone

Gebiet {n}

Zone {f}

Wabe {f} [Zone]transp.

Bereich {m} {n}

joker zone

Jokerzone {f}comp.

protected zone

Schutzzone {f}

currency zone

Währungs­raum {m}econ.

life zone

Lebenszone {f}biol.

accumulation zone

Akkumulationsgebiet {n}geol.meteo.

transition zone

Transitionszone {f}biol.engin.spec.

Wechselzone {f}spec.sports

production zone

Produktionszone {f}

hybrid zone

Hybridzone {f}biol.

taboo zone

Tabuzone {f}

unsorted zone

unsortierte Zone {f}comp.

abscission zone

Abszissionszone {f}bot.

hadal zone

hadale Zone {f}ecol.geol.hydro.

zone assignment

Zonenzuordnung {f}

• SVE has several advantages as a vadose zone remediation technology.
• ... in the vadose zone), and are varieties of entrenched, canyon-like channels as found with surface rivers.
• There are also problems in characterizing the vadose zone (unsaturated zone).
• The Richards equation appears in many articles in the environmental literature because it describes the flow in the vadose zone between the atmosphere and the aquifer.
• This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface.

• (soil moisture tension) in the vadose zone. An ISO standard, "Soil quality — Determination of pore water pressure — Tensiometer method", ISO 11276:1995, "describes methods for the determination of pore water pressure (point measurements) in unsaturated and saturated soil using tensiometers.
• A newer method that allows 1-D groundwater and surface water coupling in homogeneous soil layers, and that is related to the Richards equation is the Finite water-content vadose zone flow method solution of the Soil Moisture Velocity Equation.
• Capillary action supports a vadose zone above the saturated base within which water content decreases with distance above the water table.
• Most soils have a water content less than porosity, which is the definition of unsaturated conditions, and they make up the subject of vadose zone hydrogeology.
• The vadose zone, also termed the unsaturated zone, is the part of Earth between the land surface and the top of the phreatic zone, the position at which the groundwater (the water in the soil's pores) is at atmospheric pressure ("vadose" is from the Latin word for "shallow").

• The phreatic zone, below the phreatic surface where rock and soil is saturated with water, is the counterpart of the vadose zone, or unsaturated zone, above.
• The depth of the dry well allows the water to penetrate soil layers with poor infiltration such as clays into more permeable layers of the vadose zone such as sand.