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| Dendrocronologia× | Modellizzazione della pedogenesi× | |
|---|---|---|
| Campo | Agronomia | Agronomia |
| Famiglia | Process / pipeline | Process / pipeline |
| Anno di origine≠ | 1909 | 1941 (Jenny's factorial model); process-based numerical models from 1990s onward |
| Ideatore≠ | Andrew Ellicott Douglass | Hans Jenny (foundational framework); later extended by multiple contributors including Simonson, Hoosbeek, and Bryant |
| Tipo≠ | Archival and climate reconstruction method | Quantitative process-based simulation model |
| Fonte seminale≠ | Douglass, A. E. (1909). Weather records in the growth of giant sequoias. Monthly Weather Review, 37(1), 713-714. link ↗ | Minasny, 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 ↗ |
| Alias≠ | Tree-ring analysis, Chronology, Paleoclimatology | soil formation modeling, soil genesis simulation, pedogenic process modeling, quantitative pedology |
| Correlati≠ | 3 | 1 |
| Sintesi≠ | Dendrochronology is the science of dating and interpreting wood and climate from tree rings. Each annual ring records the tree's growth response to weather during that year: wide rings indicate favorable conditions (adequate water, warmth, light); narrow rings indicate stress (drought, cold, shade). By crossmatching ring-width patterns across trees and backward in time using dead wood, researchers construct chronologies extending centuries to millennia, providing archives of regional precipitation, temperature, and hydroclimate independent of instrumental records. | Pedogenesis 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. |
| ScholarGateInsieme di dati ↗ |
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