TRANSPIRATION OF A 64-YEAR-OLD MARITIME PINE STAND IN PORTUGAL .1. SEASONAL COURSE OF WATER FLUX THROUGH MARITIME PINE

Citation
D. Loustau et al., TRANSPIRATION OF A 64-YEAR-OLD MARITIME PINE STAND IN PORTUGAL .1. SEASONAL COURSE OF WATER FLUX THROUGH MARITIME PINE, Oecologia, 107(1), 1996, pp. 33-42
Citations number
29
Categorie Soggetti
Ecology
Journal title
ISSN journal
00298549
Volume
107
Issue
1
Year of publication
1996
Pages
33 - 42
Database
ISI
SICI code
0029-8549(1996)107:1<33:TOA6MP>2.0.ZU;2-W
Abstract
The transpiration, sap flow, stomatal conductance and water relations of Pinus pinaster were deter mined during spring and summer in a 64-ye ar-old stand in Ribatejo (Portugal). The transpiration of the pine can opy was determined from sap flow or eddy covariance techniques. Canopy conductance values (g(c)) were estimated from inversion methods using eddy covariance or sap flow data, respectively, and from scaling-up m ethods using stomatal conductance values measured in the field and lea f area index (LAI) values. The transpiration was closely controlled by the stomatal conductance of pines (Omega was 0.05-0.15). For wet soil conditions, the various estimates of g(c) showed reasonable agreement . g(c) peaked in the morning at 0.01 m x s(-1), exhibited a midday dep ression and showed a secondary peak in late afternoon. This behaviour could be predicted simply on the basis of the stomatal sensitivity to air vapour pressure deficit. On a seasonal basis, monthly average valu es of g(c) decreased from 4 x 10(3) m x s(-1) in spring to 1.7 x 10(-3 ) m . s(-1) in late summer. Accordingly, the transpiration peaked at 3 mm x d(-1) on wet soil in May. It decreased progressive ly during the summer drought to 0.8 mm x d(-1) at the end of August. The minimal va lue of needle water potential was maintained at -1.9 MPa but predawn v alues de creased from -0.6 MPa in May to -0.9 MPa in July. It may have reached lower values in August. The amount of water stored in the tru nk accounted for a 12% (10 kg x tree(-1) x day(-1)) of the daily trans piration in spring. The storage capacity of the canopy was within the same order of magnitude. The trunk storage increased to 25% (13 kg x t ree(-1) x day(-1)) of the daily transpiration at the end of summer und er drought conditions. The sap flow beneath the crown lagged according ly behind transpiration with a time constant estimated between 26 min in spring and 40 min at the end of summer.