Informe sobre l’estada de recerca a la Universitat d’Edimburg; agost, octubre – desembre 2006

Estudi realitzat a partir d’una estada al laboratori del Dr. Maurizio Mencuccini a la School of GeoSciences de la University of Edinburgh, entre els mesos d’agost i desembre del 2006. El treball realitzat s’ha centrat en tres projectes. Primerament, s’ha desenvolupat un sensor per mesurar el flux de saba al xilema i al floema, basat en la utilització de polsos de calor per tal d’estimar la velocitat del flux de massa en un medi porós. A diferència del mètode que es fa servir normalment per estimar el flux al xilema, s’ha aconseguit un nou mètode que assoleix l’escalfament fent servir un làser, la qual cosa fa que el mètode sigui no intrusiu. Per altra banda, s’ha estudiat la variabilitat de l’anatomia del floema en funció de l’edat de l’arbre en poblacions de tres espècies diferents (Pinus sylvestris, Fraxinus excelsior i Acer pseudoplatanus). L’objectiu de l’estudi és veure si l’edat/mida dels arbres afecta la mida dels elements conductors al floema, la superfície de floema funcional, o la relació entre superfície de floema funcional i superfície de fulles. Finalment, s’ha estudiat l’intercanvi de gasos a nivell de branca en funció de l’edat de l’arbre i la posició a la capçada en un bosc de Pinus sylvestris.

Does soil moisture overrule temperature dependence of soil respiration in Mediterranean riparian forests?

Soil respiration (SR) is a major component of ecosystems' carbon cycles and represents the second largest CO2 flux in the terrestrial biosphere. Soil temperature is considered to be the primary abiotic control on SR, whereas soil moisture is the secondary control factor. However, soil moisture can become the dominant control on SR in very wet or dry conditions. Determining the trigger that makes soil moisture as the primary control factor of SR will provide a deeper understanding on how SR changes under the projected future increase in droughts. Specific objectives of this study were (1) to investigate the seasonal variations and the relationship between SR and both soil temperature and moisture in a Mediterranean riparian forest along a groundwater level gradient; (2) to determine soil moisture thresholds at which SR is controlled by soil moisture rather than by temperature; (3) to compare SR responses under different tree species present in a Mediterranean riparian forest (Alnus glutinosa, Populus nigra and Fraxinus excelsior). Results showed that the heterotrophic soil respiration rate, groundwater level and 30 cm integral soil moisture (SM30) decreased significantly from the riverside moving uphill and showed a pronounced seasonality. SR rates showed significant differences between tree species, with higher SR for P. nigra and lower SR for A. glutinosa. The lower threshold of soil moisture was 20 and 17% for heterotrophic and total SR, respectively. Daily mean SR rate was positively correlated with soil temperature when soil moisture exceeded the threshold, with Q10 values ranging from 1.19 to 2.14; nevertheless, SR became decoupled from soil temperature when soil moisture dropped below these thresholds.