ScholarGate
Asistenti

Krahasoni metodat

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

Modelimi i Pedogjenezës×Kurba e Lagështisë së Tokës×
FushaAgronomiAgronomi
FamiljaProcess / pipelineProcess / pipeline
Viti i origjinës1941 (Jenny's factorial model); process-based numerical models from 1990s onward1956-1980
KrijuesiHans Jenny (foundational framework); later extended by multiple contributors including Simonson, Hoosbeek, and BryantWillard Robert Gardner, Rollin H. Brooks, Arthur T. Corey
LlojiQuantitative process-based simulation modelEmpirical soil water retention model
Burimi themeluesMinasny, B., Finke, P., Stockmann, U., Vanwalleghem, T., & McBratney, A. B. (2015). Resolving the integral connection between pedogenesis and landscape evolution. Earth-Science Reviews, 150, 102–120. DOI ↗Gardner, 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 ↗
Emërtime të tjerasoil formation modeling, soil genesis simulation, pedogenic process modeling, quantitative pedologyWater Retention Curve, pF Curve, Characteristic Curve, SWRC
Të lidhura13
PërmbledhjaPedogenesis modeling is a quantitative method used in agronomy and soil science to simulate the processes by which soils form and evolve over time. Rooted in Hans Jenny's 1941 factorial framework — soil as a function of climate, organisms, relief, parent material, and time — modern approaches translate these conceptual drivers into coupled numerical process equations, allowing researchers to reconstruct past soil states and project future soil properties under changing land use or climate scenarios.The 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.
ScholarGateSeti i të dhënave
  1. v1
  2. 2 Burimet
  3. PUBLISHED
  1. v1
  2. 3 Burimet
  3. PUBLISHED

Shko te kërkimi Shkarko diapozitivat

ScholarGateKrahasoni metodat: Pedogenesis Modeling · Soil Moisture Curve. Marrë më 2026-06-19 nga https://scholargate.app/sq/compare