1977
DOI: 10.1051/forest/19770203
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Contribution à l'étude de la transpiration et de l'adaptation à la sécheresse des jeunes plants résineux Exemple de 3 sapins du pourtour méditerranéen (Abies alba, A. Nordmanniana, A. numidica)

Abstract: RésuméL'expérience a porté sur 3 espèces de sapins de réputation croissante pour l'adaptation à la sécheresse (Sapin pectine, S. de Nordmann, S. de Numidie). Menée sur 60 semis de 2 ans, elle s'est poursuivie sur 2 an nées consécutives. Trois modalités de régime hydrique ont été imposées en 1 re année: aucune restriction (mod. 1), sécheresse accusée à partir de l'été (mod. 2) ou du printemps (mod. 3) ; seule la modalité 1 a été appliquée en 2 e année. Les plants étaient installés dans des pots étanches permett… Show more

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Cited by 7 publications
(5 citation statements)
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“…This cannot explain the lack of sap flow recovery in 2010, since the soil was well watered during the winter with high levels of snowfall. Therefore, the root system might have been damaged during the drought by moderate root embolism together with an increase in fine root mortality (Mainiero and Kazda 2006;Olesinki et al 2011) and/or the roots might be insufficiently regenerated during and after the drought due to carbon starvation (Lebourgeois et al 1998;Becker 1977). These phenomena would be accentuated in the deeper soil layer.…”
Section: Delayed Effects Of Drought On Water Uptakementioning
confidence: 99%
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“…This cannot explain the lack of sap flow recovery in 2010, since the soil was well watered during the winter with high levels of snowfall. Therefore, the root system might have been damaged during the drought by moderate root embolism together with an increase in fine root mortality (Mainiero and Kazda 2006;Olesinki et al 2011) and/or the roots might be insufficiently regenerated during and after the drought due to carbon starvation (Lebourgeois et al 1998;Becker 1977). These phenomena would be accentuated in the deeper soil layer.…”
Section: Delayed Effects Of Drought On Water Uptakementioning
confidence: 99%
“…A succession of water stress episodes leads to physiological and morphological adjustments of trees to their local environmental conditions, such as changes in xylem conductivity, changes in the ratios between sapwood area, leaf area, and soil-root exchange area and changes in leaf area index (Bréda et al 2006;Limousin et al 2009). Indeed, trees growing in a dry environment seem to adjust their structures to increase the availability of water (uptake and storage) and to reduce their demand for water (Mencuccini and Grace 1995;Bréda et al 2006;Sperry et al 1998;Becker 1977). Hence, larger root system development, lower vulnerability to embolism, and lower maximum canopy conductance limit tree vulnerability to drought as shown with modeling approaches (Martinez-Vilalta et al 2002).…”
Section: Introductionmentioning
confidence: 99%
“…Our understanding of its ecological amplitude is essentially based on the study of its natural range; this conifer cannot tolerate late frosts and dry summers and is the major component of mountain forests (900 to 1 500 m of elevation) where atmospheric humidity is high. Dendrochronological and dendro-ecological studies emphasize the high sensitivity of silver fir to water stress (Bîndiu, 1971;Serre-Bachet, 1986;Levy and Becker, 1987;Becker, 1989) while experiments on young potted trees show that it conserves water quite well (Becker, 1970(Becker, , 1977 and in particular better than Norway spruce (Picea excelsa Link) with which it is frequently mixed in mountain stands. However, silver fir appears to delay the regulation of its water-vapor exchanges, which classifies it among species that are poorly adapted to drought (Aussenac, 1980).…”
Section: Introductionmentioning
confidence: 99%
“…Les précipitations enregistrées en octobre de l'année précédente (P10) jouent un rôle négatif sur l'épaisseur des cernes dans les stations de Djelfa et positif pour les stations de Béchar. À Béchar, les pluies d'automne supérieures à la moyenne peuvent contribuer de façon notable à reconstituer le stock hydrique dans le sol disponible pour la phase ultérieure de croissance par une bonne mise en condition physiologique des plantes (Becker, 1977). Notons le rôle positif des précipitations de l'année en cours qui commencent dès février à Oum Chegag, mars à Djedida et avril pour les stations de Djelfa.…”
Section: Paramètresunclassified