Stomatal control of transpiration

 

 

Stomatal control of transpiration in the canopy of a clonal Eucalyptus grandis plantation

by Mielke M. S., Oliva M. A., de Barrros N. F., Penchel R. M., Martinez C. A., de Almeida A. C. (1999)

M. S. Mielke · M. A. Oliva  · C. A. Martinez

Departamento de Biologia Vegetal, Universidade Federal de Viçosa, 36571-000, Viçosa, MG, Brazil; e-mail: moliva@mail.ufv.br Tel.: +55 31 899 2050; Fax: +55 31 899 2580

N. F. de Barros

Departamento de Solos, Universidade Federal de Viçosa, 36571-000, Viçosa, MG, Brazil

R. M. Penchel

Centro de Pesquisa & Tecnologia, Aracruz Celulose S.A., Aracruz, ES, 29197-000, Brazil

A. C. de Almeida

Produção e Suprimento de Madeira, Aracruz Celulose S.A., Aracruz, ES, 29197-000, Brazil&

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in Trees 13: 152–160 –

ftp://ftp.aphis.usda.gov/foia/FOLDER_10/AR00038647%20Mielke%20et%20al%201999.pdf

Abstract

Predawn leaf water potential, stomatal conductance and microclimatic variables were measured on 13 sampling days from November 1995 through August 1996 to determine how environmental and physiological factors affect water use at the canopy scale in a plantation of mature clonal Eucalyptus grandis Hill ex-Maiden hybrids in the State of Espirito Santo, Brazil.

The simple “big leaf” Penman-Monteith model was used to estimate canopy transpiration. During the study period the predawn leaf water potential varied from –0.4 to –1.3 MPa, with the minimum values observed in the winter months (June and August 1996), while the average estimated values for canopy conductance and canopy transpiration fell from 17.3 to 5.8 mm s–1 and from 0.54 to 0.18 mm h–1, respectively.

On the basis of all measurements, the average value of the decoupling coefficient was 0.25. During continuous soil water shortage a proportional reduction was observed in predawn leaf water potential and in daily maximum values of stomatal conductance, canopy transpiration and decoupling coefficient.

The results showed that water vapour exchange in this canopy is strongly dominated by the regional vapour pressure deficit and that canopy transpiration is controlled mainly by stomatal conductance.

On a seasonal basis, stomatal conductance and canopy transpiration were mainly related to predawn leaf water potential and, thus, to soil moisture and rainfall. Good results were obtained with a multiplicative empirical model that uses values of photosynthetically active radiation, vapour pressure deficit and predawn leaf water potential to estimate stomatal conductance.