Linganisha mbinu
Pitia mbinu ulizochagua bega kwa bega; safu zinazotofautiana zinaangaziwa.
| Mifumo ya uhisabati wa ukuaji wa mazao (DSSAT/APSIM)× | Mchoro wa unyevu wa udongo× | |
|---|---|---|
| Nyanja | Agronomia | Agronomia |
| Familia | Process / pipeline | Process / pipeline |
| Mwaka wa asili≠ | 1993-2003 | 1956-1980 |
| Mwanzilishi≠ | James W. Jones, Gerbrand T. Hoogenboom (DSSAT); Brian A. Keating, Peter S. Carberry (APSIM) | Willard Robert Gardner, Rollin H. Brooks, Arthur T. Corey |
| Aina≠ | Mechanistic crop simulation pipeline | Empirical soil water retention model |
| Chanzo asilia≠ | Jones, J. W., Hoogenboom, G., Porter, C. H., et al. (2003). The DSSAT cropping system model. European Journal of Agronomy, 18(3-4), 235-265. 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 ↗ |
| Majina mbadala≠ | DSSAT, APSIM, Crop Simulation Model | Water Retention Curve, pF Curve, Characteristic Curve, SWRC |
| Zinazohusiana | 3 | 3 |
| Muhtasari≠ | Crop growth models are mechanistic simulation systems designed to predict crop development, biomass accumulation, and yield under varying environmental and management conditions. DSSAT (Decision Support System for Agrotechnology Transfer) and APSIM (Agricultural Production Systems Simulator) are the most widely used platforms, developed in the 1990s-2000s to support agronomic decision-making and climate adaptation research. | 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. |
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