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Krahasoni metodat

Shqyrtoni metodat e zgjedhura krah për krah; rreshtat që ndryshojnë janë të theksuar.

Kurba e Lagështisë së Tokës×Ekuacioni Penman-Monteith×
FushaAgronomiAgronomi
FamiljaProcess / pipelineProcess / pipeline
Viti i origjinës1956-19801948-1965
KrijuesiWillard Robert Gardner, Rollin H. Brooks, Arthur T. CoreyHoward Latimer Penman, John Monteith
LlojiEmpirical soil water retention modelMechanistic evapotranspiration model
Burimi themeluesGardner, W. R. (1956). Representation of soil aggregate-size distribution by a logarithmic-normal distribution. Soil Science Society of America Journal, 20(2), 151-153. DOI ↗Penman, H. L. (1948). Natural evaporation from open water, bare soil and grass. Proceedings of the Royal Society A, 193(1032), 120-145. DOI ↗
Emërtime të tjeraWater Retention Curve, pF Curve, Characteristic Curve, SWRCPM Equation, FAO-56 PM, Evapotranspiration Model
Të lidhura33
PërmbledhjaThe soil moisture curve (or soil water retention curve, SWRC) describes the relationship between soil water content and soil matric potential (water tension). It characterizes how tightly water is bound in pores of different sizes: large pores drain at low tensions (wet soils), while smaller pores retain water at high tensions (dry soils). Quantifying this relationship is essential for water balance modeling, unsaturated flow prediction, and assessing plant-available water.The Penman-Monteith equation is a mechanistic model for estimating evapotranspiration (ET), the combined loss of water from soil and plant canopies to the atmosphere. First proposed by Penman (1948) for bare soil and water surfaces, then extended by Monteith (1965) to incorporate plant resistance to water vapor diffusion, it has become the international standard for water balance studies, crop water requirement calculation, and hydrological modeling.
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ScholarGateKrahasoni metodat: Soil Moisture Curve · Penman-Monteith Equation. Marrë më 2026-06-19 nga https://scholargate.app/sq/compare