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Plant Physiol, January 2002, Vol. 128, pp. 282-290

Unraveling the Effects of Plant Hydraulics on Stomatal Closure during Water Stress in Walnut


Hervé Cochard,* Lluis Coll,1 Xavier Le Roux,2 and Thierry Améglio

Unité Mixte de Recherche 547 Physiologie Intégrée de l'Arbre Fruitier et Forestier, Institut National de la Recherche Agronomique-Université Blaise Pascal, Site de Crouelle, 63039 Clermont-Ferrand cedex 02, France


    ABSTRACT
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
LITERATURE CITED

The objectives of the study were to identify the relevant hydraulic parameters associated with stomatal regulation during water stress and to test the hypothesis of a stomatal control of xylem embolism in walnut (Juglans regia × nigra) trees. The hydraulic characteristics of the sap pathway were experimentally altered with different methods to alter plant transpiration (Eplant) and stomatal conductance (gs). Potted trees were exposed to a soil water depletion to alter soil water potential (Psi soil), soil resistance (Rsoil), and root hydraulic resistances (Rroot). Soil temperature was changed to alter Rroot alone. Embolism was created in the trunk to increase shoot resistance (Rshoot). Stomata closed in response to these stresses with the effect of maintaining the water pressure in the leaf rachis xylem (Prachis) above -1.4 MPa and the leaf water potential (Psi leaf) above -1.6 MPa. The same dependence of Eplant and gs on Prachis or Psi leaf was always observed. This suggested that stomata were not responding to changes in Psi soil, Rsoil, Rroot, or Rshoot per se but rather to their impact on Prachis and/or Psi leaf. Leaf rachis was the most vulnerable organ, with a threshold Prachis for embolism induction of -1.4 MPa. The minimum Psi leaf values corresponded to leaf turgor loss point. This suggested that stomata are responding to leaf water status as determined by transpiration rate and plant hydraulics and that Prachis might be the physiological parameter regulated by stomatal closure during water stress, which would have the effect of preventing extensive developments of cavitation during water stress.


    INTRODUCTION
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
LITERATURE CITED

Drought is one of the most limiting environmental stresses for plant production (Kramer and Boyer, 1995). Plants respond to drought by closing their stomata, which reduces leaf transpiration and prevents the development of excessive water deficits in their tissues. The drawback of the stomatal closure for plants is that their carbon gain is lowered and their growth is impaired. Therefore, information about plant responses to drought and their underlying mechanisms will have relevance for plant adaptation to new climatic conditions and breeding programs (Schulze et al., 1987).

Many physiological variables are known to be implicated in the stomatal regulation; some of these variables are involved in the mechanics of stomatal movements, others in the signals triggering these movements (Zeiger et al., 1987). A new set of variables has been proposed in the recent literature, all of which are related to the hydraulics of plants. Indeed, it has been suggested that stomata may respond to drought-induced changes in the hydraulic characteristics of the sap pathway, such as whole-plant hydraulic resistance (Rplant; Meinzer and Grantz, 1990; Cochard et al., 1996a; Lu et al., 1996), soil resistance (Rsoil), root resistance (Rroot; Meinzer and Grantz, 1990; Cochard et al., 2000b), or shoot resistance (Rshoot; Salleo et al., 1992; Sperry et al., 1993). However, during water stress, changes in the above parameters are not independent and, further, correlated to variations in soil water potential (Psi soil), whose impact on stomatal function has long been recognized (e.g. Hinckley and Bruckerhoff, 1975).

It has also been suggested that stomatal closure during water stress might be associated with the maintenance of xylem integrity (Tyree and Sperry, 1988; Jones and Sutherland, 1991). Sap is transported under negative pressures in plants, and, therefore, is susceptible to cavitation events (Pickard, 1981) that render xylem conduits non-conductive. Cavitation occurs when the negative sap pressure exceeds a threshold value defined by anatomical characteristics (Sperry and Tyree, 1988). Many species have been found to operate very close to the point of embolism. Therefore, stomata control both plant water losses and sap pressure and, thus, may actively control the risk of xylem embolism (Jones and Sutherland, 1991).

The first objective of our study was to experimentally uncouple Rsoil, Rroot, Rshoot, and Psi soil to identify the specific hydraulic parameters associated with stomatal regulation during water stress. The experiments were conducted on potted walnut (Juglans regia × nigra) trees in a growth cabinet to minimize the effects of temperature, light intensity, air vapor deficit, and air CO2 concentration on stomatal behavior. The second objective of our study was to test the hypothesis that stomata control embolism during water stress in walnut.


    RESULTS
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
LITERATURE CITED

Vulnerability to Cavitation

Vulnerability curves (VCs) were constructed by plotting the changes in the percentage loss of xylem conductance (PLC) versus xylem pressure. The VCs for the different walnut organs are shown in Figure 1 and the parameters of the logistic fitting (Eq. 4) are given in Table I. Significant differences were found between organs. Leaf rachises were significantly the most vulnerable, roots the least vulnerable, and leaf veins and shoots intermediate. The few measurements obtained on shoot segments were in agreement with our previous study.



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Figure 1.   VCs for walnut leaf midribs and rachis, and current year shoots and roots. Close symbols refer to measures on air-pressurized segments. White symbols refer to leaf midribs and rachis collected on trees during the different experiments. Error bars are ± SE. Lines are logistic fits through the data. For shoots, the lines are logistic fits through the data published by Tyree et al. (1993) for current year (plain line) and previous year (dashed line) segments.


                              
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Table I.   Xylem vulnerability to embolism

Parameters of the logistic function (see equation in the text) fitted to the experimental PLC versus Psi rachis curves. Values are given ± SE. Data having a letter in common are not significantly different at P = 0.01. 

Pressure-Volume Analysis

Turgor pressure (Pleaf  0) at full turgor averaged 0.93 ± 0.06 MPa (n = 5, ±SE) and turgor loss point averaged -1.53 ± 0.04 MPa. The relative change in Pleaf (Pleaf/Pleaf  0) with decreasing leaf water potential (Psi leaf) is shown on Figure 7.

Soil Dehydration

When plants were exposed to different light levels while soil watering was stopped (procedure 1), only a moderate water stress was induced. Figure 2 shows the concurrent changes in Eplant and Prachis for one tree. The other trees behaved the same. After 4 d, Prachis measured on the plants placed in the dark (predawn Prachis) was reduced only by 0.1 MPa (see y intercepts on Fig. 2). However, Eplant, stomatal conductance (gs), and the Prachis at maximum light intensity were considerably reduced at the end of the treatment. This was consistent with a sharp increase in Rplant. This increase could not be attributed to xylem cavitation because the xylem pressure never drops below the threshold for cavitation for all organs measured. The change in Rplant was more probably due to increase in Rsoil and/or Rroot.



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Figure 2.   Typical changes of plant transpiration and xylem water pressure during the first stage of a soil water stress for one of the studied tree. The four different symbols correspond to 4 consecutive d. Four different light intensities were used on each day to vary Eplant. Lines are linear regressions through the data for each day. The slope of the lines represents the Rplant.

When plants were continuously exposed to a constant and high light intensity for 1 week (procedure 2), higher levels of water stress were obtained. Figure 3 shows the results for one tree, the other trees behaving the same. Eplant and gs dropped close to zero whereas Prachis leveled at approximately -1.4Mpa. At this point, the degree of xylem embolism in the leaf rachis was still less than 10 PLC (not shown).



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Figure 3.   Typical time course of plant transpiration and xylem water pressure for a non irrigated tree exposed to a constant light intensity.

Root Chilling

Decreasing soil temperature from ambient to near zero temperature provoked a significant reduction in gs, Eplant, and Prachis (Fig. 4). These changes were reversed when soil temperature was returned to ambient.



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Figure 4.   Typical time course of xylem water pressure and soil temperature (top panel), and plant transpiration and gs (bottom panel) during a soil chilling experiment. Error bars are ± SE (n = 5).

Stem Pressurization

Application of a positive pneumatic pressure around the trunk of a plant induced a sharp decrease of Eplant, gs, and Prachis only for pressures greater than 2.5 MPa (Fig. 5). At this pressure, about 70 PLC was induced in the stem (see the VC for stems plotted on top of Fig. 5). For air pressure applications higher than 3 MPa, more than 95 PLC was induced in the stem, leaf wilting was noticed, and nearly 100 PLC was measured in the leaf rachis.



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Figure 5.   Changes in gs (top panel) and xylem water pressure (bottom panel) of trees exposed to increasing pneumatic pressures around their trunk (x axis). The curve represents the change in embolism in the trunk versus the applied pressure.


    DISCUSSION
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
LITERATURE CITED

The first objective of our study was to combine different experimental approaches to unravel the effect of plant hydraulics on stomatal closure. The second objective was to analyze the effect of stomatal closure on plant hydraulics and to test the hypothesis of a stomatal control of embolism.

Unraveling the Effects of Psi soil, Rsoil, Rroot, and Rshoot in the Response of gs to Water Stress

In this study, we focused our analysis on some of the endogenous physiological parameters likely to be altered during a water stress and that have been reported in the literature to be associated with stomatal responses. These parameters are the Psi soil, the Rsoil, the Rroot, and the Rshoot; all of these parameters are strongly correlated under natural drought conditions. The experiments were designed to alter Rplant in very different ways, which probably had a primary influence on different parts of the pathway.

The effects of the different experiments conducted on the same plant material can be analyzed according to their main impact on Psi soil, Rsoil, Rroot, and Rshoot. Soil dehydration provoked mainly a drop in Psi soil and an increase of Rsoil. The resistance of the interface between the soil and the root probably also increased (Nobel and Cui, 1992). Rroot was modified to the extent that the radial flow into the root xylem was altered. Rshoot was probably not altered, because the level of xylem embolism remained low during these experiments. However, if the ionic composition of the sap changed dramatically as a result of the drought, then Rshoot may have varied (Zwieniecki et al., 2001). Root chilling altered mainly Rroot and Rsoil. The soil being watered to maximum capacity in this experiment, Rsoil was very low compared with Rroot, and its variations were not quantitatively significant. Psi soil remained constant because the temperature dependence of Psi soil is very low (Muromtsev, 1981). Stem pressurization provoked only an increase in Rshoot when the pressure exceeded the point of embolism induction (about 2.0 MPa; Tyree et al., 1993; Fig. 5). If the air was propagated along the xylem flow path significantly beyond the injection point, Rroot and Rleaf may also have being altered. Therefore, combining the results of all these experiments, it is possible to determine whether gs and Eplant were specifically responding to main changes in Psi soil, Rsoil, Rroot, and/or Rshoot or not. Because air humidity, air temperature, and light intensity were maintained constant in our experiments, leaf to air vapor deficits and leaf boundary layer conductances were also constant. Therefore, the gs and Eplant patterns corresponded in our study. The relationship between gs and hydraulic parameters are likely to depend on these environmental conditions, contrary to the relationships with Eplant (Monteith, 1995).

Our results showed that the different experiments all significantly reduced Eplant and gs. Therefore, the response of gs to Psi soil, Rroot, Rsoil, and Rshoot was neither specific nor exclusive. An alternative analysis of the problem is not to consider Psi soil, Rroot, Rsoil, and Rshoot individually but rather to examine their combined effect on Prachis or Psi leaf. The relationship between Prachis, Psi soil, Rroot, Rsoil, Eplant, and gs under steady-state conditions is well described by the Ohm's law analogy (Tyree and Ewers, 1991):
P<SUB><UP>rachis</UP></SUB>=&PSgr;<SUB><UP>soil</UP></SUB>−(R<SUB><UP>soil</UP></SUB>+R<SUB><UP>root</UP></SUB>+R<SUB><UP>shoot</UP></SUB>) · <UP>SF</UP><SUB><UP>plant</UP></SUB>  ·  g<SUB><UP>s</UP></SUB>  ·  D (1)
where SFplant is the plant leaf area and D the air vapor pressure deficit, two parameters that remained constant during our experiments. The gravity term and the xylem sap osmotic potential are assumed negligible in equation 1. A similar relationship is obtained with Psi leaf if we further include the leaf blade hydraulic resistance. The dependency of gs or Eplant on Prachis and Psi leaf is shown on Figure 6 for all of the experiments. The responses were similar whatever the experiments. This would suggest that in these experiments, gs was not correlated to changes in Psi soil, Rsoil, Rroot, or Rshoot per se but rather to Prachis and/or Psi leaf. Another illustration on the combining effects of Rsoil Rroot, and Rshoot on Eplant is shown on Figure 8. An identical relationship was obtained between Eplant and Cplant (defined as [Rsoil + Rroot Rshoot]-1). Data for plants exposed to a high soil water depletion (procedure 2) are not included on Figure 8. These results are in agreement with the finding of Saliendra et al. (1995), Sperry (2000), and Hubbard et al. (2001). Our data do not enable us to test whether gs was more specifically responding to changes in Psi leaf or Prachis because both values were highly correlated and differed only by a few 0.1 MPa. Experiments where Prachis and Psi leaf are uncoupled are awaited.



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Figure 6.   Dependence of gs (top panels) and transpiration (Eplant) on xylem water pressure (left panels) and Psi leaf. The different symbols represent the different experiments conducted in this study. Transpiration was normalized by the transpiration of each tree before treatment (Eplant/Emax).

Evidence for a Stomatal Control of Xylem Embolism in Walnut

From the above discussion, it could be concluded that the effect of the stomatal closure in our study was to maintain Prachis above a threshold value around -1.4 MPa and Psi leaf above approximately -1.6 MPa. To further understand this behavior, we have to identify a major physiological trait that would threaten plant integrity at lower Prachis and/or Psi leaf values. The answer to this question is obviously very complex, because many traits are probably involved and correlations between them probably exist. We will argue that, in our study, xylem cavitation was a trait correlated with the stomatal closure.

A physiological trait associated with a stomatal closure during water stress should meet at least the following three main conditions. First, its impairment should represent a serious threat to plant functioning. This results from the consideration that the cost associated with stomatal closure is high (reduced carbon gain, reduced growth, reduced reproductive success, etc.) so the gain associated with the regulation should overcome the loss. Cavitation is a serious threat for plants because it impairs the xylem conductive capacity and may eventually lead to leaf desiccation and branch mortality (Rood et al., 2000). Indeed, leaf desiccation was not observed in our study as long as the xylem integrity was maintained. Leaf desiccation was noticed only when high levels of embolism were measured in the leaf petioles. The gain associated with stomatal closure was thus the maintenance of leaf vitality, which largely overcomes the drawbacks cited above.

The second condition is that the impairment of the trait should be water deficit dependent because the effect of stomatal closure is precisely to prevent excessive leaf dehydration. The mechanism of water stress-induced cavitation has been well documented (Sperry and Tyree, 1988; Cochard et al., 1992; Jarbeau et al., 1995). Air is sucked into the xylem lumens through pores in the pit wall when pressures in the sap exceed the maximum capillary pressures that can sustain the pores. Therefore, the likelihood of cavitation occurrence is directly determined by the degree of water deficit in the xylem, more precisely by Prachis. The maintenance of leaf turgor above cell plasmolysis is another physiological trait that might also satisfy these first two conditions.

The third condition is that the impairment of the trait should have the same water deficit dependence as stomata. Stomata were completely closed in walnut trees when Prachis reached about approximately -1.4 MPa and Psi leaf about approximately -1.6 MPa. The impairment of the trait associated with stomatal closure should therefore occur at comparable Prachis or Psi leaf values. On Figure 7 (top panel) is represented the dependencies of Eplant and rachis embolism on Prachis. The leaf rachis was the most vulnerable organ along the sap pathway in the xylem and was also exposed to the lowest xylem pressure values. Leaf rachis is therefore the Achilles' heel of the walnut tree sap pathway. Segmentation in xylem vulnerability to cavitation has been demonstrated for several other species (Cochard, 1992; Sperry and Saliendra, 1994). A lot of variation exists between species, and occasionally the roots appear to be the most cavitation sensitive organs in the plant (Sperry and Ikeda, 1997). From Figure 7, it is clear that the dependencies of leaf rachis xylem embolism and transpiration on water deficit were very similar. Stomata were completely closed at the incipience of xylem embolism in the leaf rachis. Figure 7 (bottom panel) shows the concurrent variations of Eplant and leaf turgor pressure (Pleaf) with bulk Psi leaf. It is also clear from this graph that stomata were completely closed at the incipience of leaf cell plasmolysis (turgor loss point). The maintenance of xylem integrity and leaf turgor were closely associated with stomatal closure during water stress in walnut.



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Figure 7.   Dependence of plant transpiration and xylem rachis embolism on rachis xylem pressure (top panel) and dependence of plant transpiration and leaf turgor pressure on Psi leaf (bottom panel). Error bars are ± SE. The VC was replotted from Figure 1, and data for transpiration rate were averaged from Figure 7.

The data from Figure 7 suggest that stomatal closure was rather preemptive in avoiding cavitation. This behavior might be explained by the potential for "catastrophic xylem failure" (Tyree and Sperry, 1988). There is a feedback between xylem conductance and xylem pressure during cavitation. Cavitation decreases xylem conductance, which in turn decreases xylem pressure and thus provokes more cavitation. Tyree and Sperry (1988) and Jones and Sutherland (1991) have computed that catastrophic xylem failure occurs at the expense of some xylem conductance and at a critical transpiration rate (Ecrit) only slightly greater than the actual maximum E. The hypothesis of a stomatal control of catastrophic xylem failure was evaluated with an hydraulic model of a walnut tree explicitly taking into account the feedback between xylem pressure and xylem conductance. Our simulations confirmed the results of Sperry et al. (1998) and Comstock and Sperry (2000). Transpiration was maximized (Ecrit) at the expense of all conductance in the distal leaf rachis segment. Ecrit was therefore much higher than the actual Eplant (Fig. 8, plain line). Using the same model, we have computed Eplant provoking 1% (E1PLC) and 10% (E10PLC) loss of rachis conductance (Fig. 8, dotted and dashed lines, respectively). The onset of tree water loss regulation occurred when Eplant reached E1PLC and Eplant tracked E10PLC when plant conductance was further reduced. This model suggests that the risk of catastrophic xylem failure was not associated with the stomatal regulation in walnut. gs was not maximized at the expense of all xylem conductance. Rather, xylem conductance was maximized at the expense of all gs. To experimentally validate these computations, we have tried, without success, to feed stressed plants with fusiccocine, a drug supposed to promote stomatal opening. The use of mutants lacking efficient stomatal regulation is probably a better way to test such hypotheses (Cochard et al., 1996b).



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Figure 8.   Plant transpiration versus whole plant hydraulic conductance. Different symbols represent different experiments. The plain, dashed, and dotted lines represent the critical transpiration rate provoking 100%, 10%, and 1% loss conductance in the leaf rachis, respectively.

Mechanisms Triggering Stomatal Closure

The mechanisms by which stomata could sense changes in Prachis to adjust gs and avoid cavitation remain hypothetical. It seems improbable that Prachis itself was the triggering parameter, so we must identify a parameter correlated to Prachis during water stress. Our stem pressurization experiments dismiss the implication of parameters associated with soil or root water stress (such as Psi soil or abscisic acid production by roots [Tardieu et al., 1992]). Because the onset of cavitation events in leaf blades was correlated with the onset of stomatal closure in laurel, it has been suggested that stomata were responding to hydraulic signals generated by cavitation (Salleo et al., 2000; Nardini et al., 2001). However, in our study, stomatal closure occurred before the onset of cavitation in leaf blades and midribs (Fig. 6) and only after 70% loss of conductance in the trunk (Fig. 5). The possibility that stomata were responding to Psi leaf cannot be rejected because of the high correlation between Prachis and Psi leaf in our study. Psi leaf could have a direct impact on guard cells turgor (Meidner and Edwards, 1996) or an indirect impact on their sensitivity to abscisic acid (Tardieu and Davis, 1993). A stomatal response to changes in leaf water status has long been suggested (Cowan, 1977) and has recently been supported by root pressure chamber experiments on woody plants (Fuchs and Livingston, 1996; Comstock and Mencuccini, 1998). These experiments demonstrate that stomatal closure caused by soil drought or decreased air humidity can be partially or wholly reversed by root pressurization.


    CONCLUSIONS
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
LITERATURE CITED

In conclusion, combining different experimental procedures, we have established that stomata were not responding to changes in Psi soil, Rsoil, Rroot, or Rshoot per se but rather to their impact on Prachis or Psi leaf. Cavitation avoidance was a likely physiological function associated with stomatal regulation during water stress in these experiments. However, the mechanism triggering the stomatal closure probably resides in the leaf mesophyll itself as stomatal closure was also correlated to bulk leaf turgor. The significance of cavitation avoidance seems crucial to understand plant water relations during water stress, probably more than the occurrence of cavitation itself. The possibility still exists that the striking relations that were observed between cavitation and stomatal function were only correlations and that the main physiological trait involved in the regulation was elsewhere. However, it seems to us that cavitation avoidance fits the three conditions we have identified for such a trait better that any other trait so far.


    MATERIALS AND METHODS
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
LITERATURE CITED

Plant Material and Growth Conditions

Experiments were conducted on 3-year-old walnut (Juglans nigra × regia cv NG38 grafted on Juglans regia rootstocks) trees grown in 35-L pots containing one-third peat and two-thirds natural clay soil from the Limagne region (France). The plants, grown in a nursery, were transferred to growth cabinets where air temperature (25°C) and air humidity (60% relative humidity) were constant. The light intensity at foliage level was adjusted between 0 and 480 µmol m-2 s-1. A total of 17 trees were used in the different experiments. Because the experiments were time consuming, we chose to combine multiple experiments with a rather limited number of repetitions.

Psi leaf and Plant Transpiration

Psi leafs were measured with a Scholander-type pressure chamber on leaflets randomly sampled on the trees. The xylem water pressure at the base of the leaflet blades (Prachis) was measured on leaflets enclosed for at least 2 h in an air proof aluminum bag (Turner and Long, 1980). To minimize the reduction in tree leaf area due to sampling, only one replicate of Prachis and Psi leaf were performed each time.

Plant water loss (Eplant) was estimated with two independent techniques. Sap flow through the trunk was monitored by the heat balance technique of Valancogne and Nasr (1989). Eplant was also measured gravimetrically with an electronic balance (model ID1, resolution 1g, Mettler, Viroflay, Switzerland). In addition, leaf transpiration and leaf gs were measured with a steady-state porometer (model 1600, LI-COR, Linclon, NE). The measurements were performed on five leaflets randomly chosen in each trees.

Xylem Embolism

The degree of xylem embolism due to the presence of air in the vessels was assessed following the procedure introduced by Sperry et al. (1988) and recently substantiated (Cochard et al., 2000a). We used the new XYL'EM apparatus (Xylem Embolism Meter, Instrutec, Montigny les Cormeilles, France), based on a high-resolution liquid mass flowmeter, to determine the PLC in the leaf rachis. For each PLC determination, one leaf was cut from the trees under tap water. Six segments 15 to 20 mm long were excised, still under water, from the leaf rachis, and four segments were detached from the midribs of four leaflets. The segments were attached to the tubing of the XYL'EM apparatus and their initial hydraulic conductance (Kinit) determined with a hydrostatic pressure gradient of approximately 3 kPa. The samples were then flushed with water pressurized to 0.1 MPa and the maximum conductance (Kmax) determined as above. The PLC was calculated as follows:
<UP>PLC</UP>=100×(1−K<SUB><UP>init</UP></SUB>/K<SUB><UP>max</UP></SUB>) (2)

Rplant

The Rplant was computed as the ratio between the water potential drop along the sap pathway and the whole-plant transpiration:
R<SUB><UP>plant</UP></SUB>=(&PSgr;<SUB><UP>soil</UP></SUB>−P<SUB><UP>rachis</UP></SUB>)/E<SUB><UP>plant</UP></SUB> (3)
It should be noted that, as we have defined it, Rplant does not include the leaf blade hydraulic resistance. Psi soil was estimated by the Prachis value measured on the plants placed in the dark (Améglio et al., 1999).

VCs

The vulnerability of the xylem conduits to air embolism was determined following the pressure chamber dehydration technique of Cochard et al. (1992). The technique consisted in inserting a plant segment in a pressure chamber with only the cut end protruding. The pressure in the chamber was then adjusted to a target value and maintained constant until sap exudation ceased (usually after 15-30 min). The pressure was then released and xylem segments were excised under water and their PLC value determined as above. The plot of the PLC value versus the applied air pressure represents the VCs of the plant segment. VCs were first obtained for leaflet midribs, leaf rachises, and fine roots. A few measurements were also made on current year stem segments to confirm our previous results (Tyree et al., 1993).

For midrib and rachis VCs, entire leaves were pressurized. Four to six rachis segments were measured on each leaf. The basal 20 cm of the leaf rachis was discarded to avoid artifacts caused by air entry into cut vessels. On the same leaves, midribs were excised from the four apical leaflets. Root VCs were obtained on lateral roots excised from entire root systems gently washed with tap water. A total of 13 leaves and 13 roots from three different trees were used to construct the VCs. The following logistic function was fitted to the different curves (Cochard et al., 1999).
<UP>PLC</UP>(P<SUB><UP>rachis</UP></SUB>)=100/(1+(P<SUB><UP>rachis</UP></SUB>/P<SUB><UP>rachis50</UP></SUB>)<SUP><UP>s</UP></SUP>) (4)
where Prachis50 is the water pressure inducing 50 PLC and s is a slope parameter.

Pressure-Volume Analysis

Pressure-volume curves were obtained for five individual leaves using the bench top dehydration method (Ritchie and Hinckley, 1975). Leaves were harvested, enclosed in a plastic bag, and let to rehydrate overnight with their petiole immerged in distilled water. Bulk tissue estimates of turgor pressure (Pleaf) and turgor loss point were made using the method of Schulte and Hinckley (1985).

Soil Dehydration

The stomatal response to a soil water deficit was studied on six different trees following two complementary procedures. The water deficit was induced by withholding irrigation. For the first procedure, the light intensity in the chamber was increased by steps during the day. Four light intensities (0, 170, 250, and 450 µmol m-2 s-1) were applied for 2 h each, to obtain different transpiration rates so the slope of E versus Prachis could be determined for getting Rplant. After 2 h, plant transpiration was stable, enabling determination of Psi leaf, Prachis, and gs. During the night, the light level was maintained at 170 µmol m-2 s-1 to progressively lower the soil water content. The procedure was repeated for 4 consecutive d for each of the three trees used in this experiment. In a second procedure, plants were continuously exposed to 450 µmol m-2 s-1 during 7 consecutive d. Psi leaf, Prachis, and gs were determined twice a day. Leaves were periodically sampled for embolism assessment. The second procedure was repeated on three different trees.

Stem Pressurization

The aim of this experiment was to analyze the stomatal response to an increase in trunk hydraulic resistance. We used the air injection technique (Cochard et al., 1992; Salleo et al., 1992) to induce air embolism in the trunk and thus increase the trunk resistance. A 20-cm-long pressure chamber was fastened to the trunk of three different trees exposed to a constant light intensity (450 µmol m-2 s-1). The pressure chamber was similar to the chamber described by Salleo et al. (1992), except that it was divided in two parts and could be clamped on intact trees (Améglio et al., 1994). To facilitate air entry into the xylem conduits, six 1.3-mm-diameter holes were drilled radially through the trunk inside the chamber. The holes were aligned vertically to minimize the damage to the xylem conduits. In a preliminary experiment, we verified that fastening the pressure chamber to the tree had no effect on tree transpiration and Psi leaf. The trunk segment in the chamber was exposed to increasingly higher air pressures (up to 3.5 MPa). Each target pressure was maintained constant for 15 min. Two hours after each pressurization, two leaflets were sampled, one to measured Prachis, and one to measure Psi leaf with a pressure chamber, and gs was measured on five leaflets. Leaves were also periodically sampled for embolism assessment.

Root Chilling

This experiment aimed at altering root and soil hydraulic resistance by changing soil temperature (Brodribb and Hill, 2000; Cochard et al., 2000b). A well-watered tree was placed in the growth chamber with 450 µmol m-2 s-1 light intensity. Psi leaf, Prachis, and gs were measured when Eplant became stable. Solutions with different temperature were obtained by mixing tap water with ice. The solutions were successively poured on the soil to lower its temperature (Tsoil) in a step-wise manner from ambient to approximately 0.5°C. Tsoil was measured with a thermocouple inserted near the center of the pot. After approximately 75 min, Psi leaf, Prachis, and gs were measured, and a cooler solution was poured on the soil. Tsoil was then returned to 20°C by pouring water at ambient temperature on the soil. The whole procedure was repeated three times on two different trees.

Modeling

The relationship between plant hydraulic parameters and water loss regulation was analyzed with a model similar to the ones developed by Tyree and Sperry (1988) and Sperry et al. (1998). The soil-plant continuum is represented by hydraulic resistances in series: Rsoil, Rroot, Rstem, Rtrunk, Rbranch, Rrachis, and Rleaf. The partitioning of resistances within a tree was measured with an high pressure flowmeter (H. Cochard, unpublished data; Tyree et al., 1994). The relationships between the different xylem resistances and the xylem pressure were derived from the logistic fits of their VCs. Rsoil was supposed negligible and not Psi soil dependent. Therefore, our model pertains only for the understanding of stomatal behavior during our root chilling and stem pressurization experiments. Sperry et al. (1998) and Comstock and Sperry (2000) have pointed out that the accuracy of such models depends on how finely the continuum is discretized. In our model, each xylem resistance was divided into 10 tiers. A test with 1,000 tiers yielded only 1.7% higher Ecrit values. Ecrit was determined to the nearest 0.001 mmol s-1 by progressively increasing Eplant until 100 PLC was obtained in one tier. The model was run with increasing Rroot and Rtrunk values to simulate the experimental observations. The model, called "RER," was developed on an Excel (Microsoft, Redmond, WA) spreadsheet.


    ACKNOWLEDGMENTS

We thank Boris Adam, Christian Bodet, Patrice Chaleil, Maurice Crocombette, Robert Falcimagne, and Stéphane Ploquin for their help during this work. The comments of John Sperry and two anonymous reviewers are greatly appreciated.

    FOOTNOTES

Received April 30, 2001; returned for revision July 4, 2001; accepted October 17, 2001.

1 Present address: Centre d'Etude du Machinisme Agricole du Génie Rural des Eaux et Forêts, Unité de Recherche Dynamiques et Fonctions des Espaces Ruraux, 24, Av. des Landais Boite Postale 50085, 63172 Aubiere cedex, France.

2 Present address: Laboratoire d'Ecologie Microbienne, Unité Mixte de Recherche 5557 (Centre National de la Recherche Scientifique-Université Lyon 1), 43 bd du 11 Novembre 1918, 69622 Villeurbanne, France.

* Corresponding author; e-mail cochard{at}clermont.inra.fr; fax 33-4-73-62-44-54.

Article, publication date, and citation information can be found at www.plantphysiol.org/cgi/doi/10.1104/pp.010400.


    LITERATURE CITED
TOP
ABSTRACT
INTRODUCTION
RESULTS
DISCUSSION
CONCLUSIONS
MATERIALS AND METHODS
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© 2002 American Society of Plant Physiologists



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