scholarly journals Measuring Leaf Water Potential

EDIS ◽  
2021 ◽  
Vol 2021 (5) ◽  
Author(s):  
Christian Bartell ◽  
Haimanote K. Bayabil ◽  
Bruce Schaffer ◽  
Fitsum Tilahun ◽  
Fikadu Getachew

This article summarizes the basic concepts of leaf water potential measurements and two available methods for measuring leaf water potential under field and laboratory conditions. Written by Christian Bartell, Haimanote K. Bayabil, Bruce Schaffer, Fitsum Tilahun, and Fikadu Getachew, and published by the UF/IFAS Department of Agricultural and Biological Engineering, October 2021.

Crop Science ◽  
1986 ◽  
Vol 26 (2) ◽  
pp. 380-383 ◽  
Author(s):  
R. C. Johnson ◽  
H. T. Nguyen ◽  
R. W. McNew ◽  
D. M. Ferris

2002 ◽  
Vol 127 (3) ◽  
pp. 448-454 ◽  
Author(s):  
L.E. Williams ◽  
F.J. Araujo

A study was conducted to compare three measurements of determining water status of grapevines (Vitis vinifera L.) in the field. Predawn leaf water potential (ΨPD), midday leaf water potential (Ψl), and midday stem water potential (Ψstem) were measured on `Chardonnay' and `Cabernet Sauvignon' grapevines grown in Napa Valley, California late in the 1999 growing season. Both cultivars had been irrigated weekly at various fractions (0, 0.5, and 1.0 for `Chardonnay' and 0, 0.5, 0.75, and 1.5 for `Cabernet') of estimated vineyard evapotranspiration (ETc) from approximately anthesis up to the dates of measurements. Predawn water potential measurements were taken beginning at 0330 hr and completed before sunrise. Midday Ψl and Ψstem measurements were taken only between 1230 and 1330 hr. In addition, net CO2 assimilation rates (A) and stomatal conductance to water vapor (gs) were also measured at midday. Soil water content (SWC) was measured in the `Chardonnay' vineyard using a neutron probe. Values obtained for ΨPD, Ψl, and Ψstem in this study ranged from about -0.05 to -0.8, -0.7 to -1.8, and -0.5 to -1.6 MPa, respectively. All three measurements of vine water status were highly correlated with one another. Linear regression analysis of Ψl and Ψstem versus ΨPD resulted in r2 values of 0.88 and 0.85, respectively. A similar analysis of Ψl as a function of Ψstem resulted in an r2 of 0.92. In the `Chardonnay' vineyard, all three methods of estimating vine water status were significantly (P < 0.01) correlated with SWC and applied amounts of water. Lastly, ΨPD, Ψl, and Ψstem were all linearly correlated with measurements of A and gs at midday. Under the conditions of this study, ΨPD, Ψl, and Ψstem represent equally viable methods of assessing the water status of these grapevines. They were all correlated similarly with the amount of water in the soil profile and leaf gas exchange as well as with one another.


OENO One ◽  
2004 ◽  
Vol 38 (1) ◽  
pp. 15
Author(s):  
Alain Carbonneau ◽  
Alain Deloire ◽  
Pietro Costanza

<p style="text-align: justify;">An experiment on Syrah in the Ecotron design of the AGRO Montpellier/INRA campus vineyard, with the control of different water regimes, allowed to test the physiological meaning and the field of application of different modalities of leaf water potential measurements : predawn and daily potential for leaves in a normal micro-environment (which keep all of their interest and generality), « stem » potential (which must be called differently and reserved to particular conditions) for shadow enveloped leaves. Field observations on Syrah and Merlot confirm the interest of some methods.</p>


OENO One ◽  
1998 ◽  
Vol 32 (2) ◽  
pp. 59
Author(s):  
Isabelle Mérouge ◽  
Gérard Seguin ◽  
Dominique Arrouays

<p style="text-align: justify;">The soil variability that we evidenced within the Pomerol vineyard (first part) in France (near to Bordeaux) led us to compare the behaviour of Merlot noir, which is the main local cultivar in this area. This study was conducted on four sites, which belong to the main soil map units of the area. Soils (FAO) were: a deep (A) and a shallow (C) planosols with abrupt textural changes between uppest sandy-gravelly horizons and sandy clay (A) or heavy clay (C) deeper layers, a very sandy well-drained neoluvisol (B), and a very stony cambisol with a temporary watertable (D). Water uptake by vines was assessed by leaf water potential measurements undertaken from June to September. Both observations on shoot elongation and leaf water potential measurements were performed together. The year 1995 exhibited a mild winter, then followed by both temperature and insolation higher than mean values. The rainfall in summer was less than the mean value, and the climatic water balance was negative. As a consequence, the vine phenology exhibited a very early development. Various water behaviours were observed amongst the four experimental plots: some were strongly linked to c1imatic events whereas others showed regulating mechanisms attributable to inherent soil properties such as texture and structure. The vine on soil D exhibited the greatest variations in water potential, showing significant periods of droughtiness during summer. On this soil, the variations in leaf water potential were strongly linked to rainfall events in summer. The vine on soil B kept the less negative values of water potential in relation to the very deep root development which was observed in this light and well-drained sandy material. The vine on soil A had a high water uptake during the period of shoot development, but showed a significant reduction of water availability in august. The most progressive regulation of water uptake was observed on soil C, and could be attributed to the elongation of roots with shrinking during summer in the deep c1ayey horizons. The water behaviour variability was mainly linked both to textural and structural soil properties intluencing soil water retention, aeration, and rooting development. The longest shoots were observed in soil (A) where the elongation speed was the highest. On soil (B) shoot elongation was signiticantly reduced, although water supply was the highest. This was attributed to a low nutrient availability in this very sandy soil. The elongation speed in site (D) was rather chaotic, and was related to marked variations in water supply. The lowest shoot elongation was observed in the shallow planosol (C). Preliminary results on grape quality are showed, and seem to be consistent with these behaviours.</p><p style="text-align: justify;">These results are consistent with previous studies on various vines of the Bordeaux region which have already shown that various soil properties might induce a control on water behaviour in soil and thus might result in similar consequencies for water availability for vines. The discussion points out the important role played by water uptake control mechanisms on vintage quality in this area.</p>


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