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| Klorofülli fluorestsents× | Penman-Monteithi võrrand× | |
|---|---|---|
| Valdkond | Agronoomia | Agronoomia |
| Perekond | Process / pipeline | Process / pipeline |
| Tekkeaasta≠ | 1931-2004 | 1948-1965 |
| Looja≠ | Hans Kautsky, Ulrich Schreiber, Reto J. Strasser | Howard Latimer Penman, John Monteith |
| Tüüp≠ | Non-invasive photosynthetic measurement | Mechanistic evapotranspiration model |
| Algallikas≠ | Kautsky, H., & Hirsch, A. (1931). Neue Versuche zur Klärung der Assimilationstätigkeit. Naturwissenschaften, 19(48), 964-964. link ↗ | Penman, H. L. (1948). Natural evaporation from open water, bare soil and grass. Proceedings of the Royal Society A, 193(1032), 120-145. DOI ↗ |
| Rööpnimetused≠ | Fluorescence, Fv/Fm, OJIP curve, PAM fluorometry | PM Equation, FAO-56 PM, Evapotranspiration Model |
| Seotud | 3 | 3 |
| Kokkuvõte≠ | Chlorophyll fluorescence is a non-invasive optical measurement of how efficiently the photosynthetic machinery converts absorbed light into chemical energy (photosynthesis) or heat and light (fluorescence). When photosynthesis is inhibited by stress (drought, cold, salt, pests), chlorophyll fluorescence increases because excitation energy cannot be used for photosynthesis and must be released as light or heat. Fluorescence parameters (Fv/Fm, OJIP curves) act as sensitive, rapid indicators of photosynthetic stress, enabling early detection of plant dysfunction before visible symptoms appear. | 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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