LEAF WATER POTENTIAL AND STOMATAL CONDUCTANCE IN QUERCUS-PYRENAICA WILLD FOREST - VERTICAL GRADIENTS AND RESPONSE TO ENVIRONMENTAL-FACTORS

Two permanent sampling sites were selected at the two extremes of a ra infall gradient in natural forests of Quercus pyrenaica Willd. located in the Sierra de Gata (Salamanca Province, Spain). During 1991 and 19 92, diurnal courses of transpiration rate (E), stomatal conductance (g (s)) and leaf water potential (PSI1) were studied at different levels in the tree canopy. Leaf water potential fell from a high value in the early morning to a minimum at midday and then increased again in the afternoon. Values of PSI1 in the early morning and at midday were lowe r at Fuenteguinaldo (dry site) than at Navasfrias (wet site) and were related to soil water availability. Stomatal conductance increased dur ing the morning and maximum g(s) occurred about 3 h before PSI1 was at its lowest value. The highest values of g(s) were found at Navasfrias during July. The lowest PSI1 values were found in the upper parts of the canopy and differences among canopy levels were greatest when soil water availability was low. In August, minimum values of Ti differed among canopy levels by 1.0 MPa at Navasfrias and by 0.8 MPa at Fuenteg uinaldo. The maximum difference in g(s) among canopy levels was about 150 mmol m-2 s-1 at Navasfrias and about 300 mmol m-2 s-1 at Fuentegui naldo. The results indicate a nonconservative pattern of water use in Quercus pyrenaica.