field capacity

listen to the pronunciation of field capacity
İngilizce - Türkçe
tarla kapasitesi

İlgili Terimler

available field capacity
(Tarım) faydalı tarla kapasitesi
İngilizce - İngilizce
The amount of water the soil can hold once gravitational water has drained away; this water is mostly capillary water held to soil particles with at least 0 3 bars of suction
Following drainage in a soil, which is typically 1 - 3 days after rainfall, this is the amount of water that remains in the soil profile and is the commencing point for the available water capacity It is the maximum amount of water that a soil can retain against the force of gravity
The maximum amount of water that can be held by a soil
the amount of water held in soil against the pull of gravity
The capacity of soil to hold water
The water remaining in a soil after the complete draining of the soil's gravitational water
The water content, (%v), of the soil matrix approximating the water content of a saturated soil that has been allowed to freely drain Estimated as a hydraulic tension of 33 kPa ( 33 Bar) and dependant only on the soil texture and unaffected by salinity or gravel
The total amount of water that may be retained against gravity by landfilled solid wastes, for example after saturation and draining
the amount of water held in soil after gravitational water is drained
The moisture content of soil that has drained by gravity after having been wetted thoroughly with water
the maximum amount of water that a particular soil can hold
The point at which all excess gravitational water has drained from a soil
The state of saturated soil when all the soil moisture that is able to freely drain away has done so
The state at which a soil is holding the maximum amount of water it can after free water has drained through and no surface water remains
The percentage of water remaining in a soil after it has been saturated and after free drainage is negligible
The capacity of soil to hold water Field capacity can vary widely among differing soil types and between soils of similar type with different land-use patterns
the water content of a soil two or three days after it has been saturated by irrigation or rain
Content of water, on a mass or volume basis, remaining in a soil after being saturated with water and after free drainage is negligible
The condition of a soil when it contains all the water retained after draining freely under gravity
Related Topics: [drainage] The maximum water content of a soil when gravitational water is removed The resulting moisture, less the amount remaining when the moisture level reaches the permanent wilting point, is available to support plant growth
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field capacity

    Heceleme

    field ca·pac·i·ty

    Türkçe nasıl söylenir

    fild kıpäsıti

    Telaffuz

    /ˈfēld kəˈpasətē/ /ˈfiːld kəˈpæsətiː/