The seasonal and diurnal variation of CO2 flux (F c ) and COs--water flux ratio (CWFR) of alfalfa were studied using micrometeorological techniques during the summer of 1978 at a location in the east central Great Plains. Significant seasonal variation was found in both F c and CWFR. F c and CWFR w
Environmental effects on the CO2 flux and CO2—Water flux ratio of Alfalfa
✍ Scribed by Dennis D. Baldocchi; Shashi B. Verma; Norman J. Rosenberg
- Publisher
- Elsevier Science
- Year
- 1981
- Weight
- 538 KB
- Volume
- 24
- Category
- Article
- ISSN
- 0002-1571
No coin nor oath required. For personal study only.
✦ Synopsis
Environmental effects on the CO2 flux (Fc) and CO2--water flux ratio (CWFR) of alfalfa (Medicago sativa L.) were studied using micrometeorological techniques. The study was conducted in the east central Great Plains of North America. F c was dependent on solar radiation, turbulent mixing and air temperature. The response of F c to increasing irradiance was described by a diminishing returns curve. Increasing turbulent mixing caused a reduction in the boundary-layer resistance to CO2 transfer and increased light penetration into the canopy; both factors caused F c to increase. Under high irradiance, F c decreased with increasing air temperature in the range 23--32°C. This effect was due to both soil plus root and dark respiration increasing with air temperature. Fc was not limited by plant water potentials ranging between --7 and --17 bar. That alfalfa is relatively drought-tolerant is indicated by the fact that no significant stomatal closure seemed to have occurred at water potentials as low as --17 bars. CWFR was correlated with net radiation. Sensible heat advection, however, reduced CWFR since this additional source of energy contributed only to evapotranspiration.
📜 SIMILAR VOLUMES
As the substantial component of the ecosystem respiration, soil CO 2 flux is strongly influenced by infrequent and unpredictable precipitation in arid region. In the current study, we investigated the response of soil CO 2 flux to rain pulses at a saline desert in western China. Soil CO 2 flux was m