Physiological and Agronomic Responses of Processing Tomatoes to Deficit Irrigation at Critical Stages in a Semi-Arid Environment
Physiological and Agronomic Responses of Processing Tomatoes to Deficit Irrigation at Critical...
Patanè, Cristina;Corinzia, Sebastiano Andrea;Testa, Giorgio;Scordia, Danilo;Cosentino, Salvatore Luciano
2020-06-04 00:00:00
agronomy Article Physiological and Agronomic Responses of Processing Tomatoes to Deficit Irrigation at Critical Stages in a Semi-Arid Environment 1 , 2 2 2 Cristina Patanè *, Sebastiano Andrea Corinzia , Giorgio Testa , Danilo Scordia 1 , 2 and Salvatore Luciano Cosentino CNR-Istituto per la BioEconomia (IBE), Sede Secondaria di Catania, Via P. Gaifami 18, 95126 Catania, Italy; sl.cosentino@unict.it Dipartimento di Agricoltura, Alimentazione e Ambiente, Università degli Studi di Catania, via Valdisavoia 5, 95123 Catania, Italy; andrea.corinzia@unict.it (S.A.C.); gtesta@unict.it (G.T.); dscordia@unict.it (D.S.) * Correspondence: cristinamaria.patane@cnr.it; Tel.: +39-095-733-8395 Received: 9 May 2020; Accepted: 1 June 2020; Published: 4 June 2020 Abstract: Deficit irrigation is a valid alternative to conventional irrigation to save water while maintaining high productivity in tomatoes. However, crop sensitivity to water stress due to deficit irrigation may change with the growth stage. To assess the physiological and agronomic responses of processing tomatoes to deficit irrigation applied at critical stages, a field experiment was conducted in a coastal site of Southern Italy, where seven irrigation treatments diering for daily evapotranspiration (ETc) restored (100%—full or 50%—deficit) and the time of watering (long-season or limited to the vegetative period or to flowering) were applied to processing tomatoes cv. Hypeel F1. Plants continuously irrigated and those irrigated only at flowering maintained higher rates of leaf transpiration (E) and stomatal conductance (g ) over those irrigated only during the vegetative period. Fruit yield was the greatest under long-season full irrigation (51 t ha ). Severe soil water deficit during flowering, more than during the vegetative period, adversely aected crop productivity. Irrigation water use eciency (IWUE) was maximized under long-season deficit irrigation (>19 kg m ) or deficit irrigation during flowering (>16 kg m ). E and g measured at early or mid-flowering may be adopted as valuable indicators to predict crop productivity; however, they may be altered under high vapor pressure deficit (VPD). Predawn water potential, being little aected by VPD, is a more reliable parameter than leaf transpiration and stomatal conductance under these climatic conditions. Keywords: processing tomatoes; deficit irrigation; soil water content; leaf transpiration; stomatal conductance; vapor pressure deficit; water use eciency 1. Introduction Tomatoes (Solanum lycopersicum L.) are an important economic crop worldwide, with the greatest area of cultivation among vegetables [1]. In 2018, the total tomato production exceeded 182 million tons over a cultivation area of 4.7 million hectares [2]. Tomatoes have a subtropical origin, thus requiring large amounts of irrigation water during summer, which is the cropping season for processing tomatoes in dry areas of Southern Italy. However, in these areas, the scarce availability of irrigation water resources and the lack of rainfall during summertime limit a sustainable cultivation for high water-demanding crops, such as processing tomatoes; besides, the irrigation issues have seriously been worsened due to climate change eects. Indeed, to maximize tomato yields, soil water availability at the root zone must be maintained near field capacity throughout the growth period [3]. Under a semi-arid environment, the development of water-saving irrigation strategies may encourage farmers to revise their irrigation scheduling approach towards a more ecient water Agronomy 2020, 10, 800; doi:10.3390/agronomy10060800 www.mdpi.com/journal/agronomy Agronomy 2020, 10, 800 2 of 17 management, in order to limit water consumption and bring to satisfactory yields. Deficit irrigation approaches result in a reduced water application while maintaining adequate yields and enhancing overall fruit quality [4]. This is also for tomatoes, where the validity of the adoption of this water-saving irrigation strategy has been largely documented [4–7]. One of the greatest benefits of deficit irrigation is that, besides saving large amounts of water, it allows to lessen the production costs, to improve water productivity (i.e., the eciency in its use) and, overall, to reduce the impact of the crop to the environment, as compared to conventional irrigation [8]. However, not all stages of the crop-growing season are sensitive to water stress due to deficit irrigation similarly. In tomato crops, the most sensitive phenological phase to water stress is generally flowering [6]. Significant eects of water deficit at fruit ripening on tomato yields under greenhouse conditions have been also reported [9]. The relationship between soil water deficits at critical stages and the physiological and productive behavior of tomatoes is quite complex and long studied, although controversial results have been reported [1]. Models to estimate the eects of evapotranspiration (ET) were developed as well, either at each growth stage or for the whole growth period, on crop yields. Some of them, like the date crop water production function (DCWPF) [10] or Minhas model with its water deficit sensitivity indexes [11] can be applied to optimize the irrigation water management in areas of water scarcity. As aforementioned, the eects of irrigation at dierent stages of the crop growing season have been extensively studied in tomatoes, although mostly upon fruit yield and quality [12–15]. However, detailed studies on the relationships between crop physiology and growth in field-grown tomatoes exposed to dierent deficit irrigation regimes are still lacking. The identification of the most critical stages to water stress through the measurement of some plant water status parameters may contribute to a better manipulation of deficit irrigation in processing tomatoes. Indeed, both soil water and climate conditions may greatly aect the physiological parameters (stomatal conductance, transpiration and pre-dawn leaf water potential) of the crop, even under unrestricted soil water content conditions [16]. The goal of this study was to assess the eects of deficit irrigation applied to the crop-growing season or at critical stages on physiology, growth, yield and water use eciency in field-grown processing tomatoes under a semi-arid Mediterranean environment of South Italy, in order to identify the most water stress-sensitive period and optimize irrigation water management under water scarcity conditions. 2. Materials and Methods 2.1. Open-Field Experiment Field experiment was conducted during the 2012 season in a site on the Eastern coast of Sicily 0 0 (South Italy, 10 m a.s.l., 37 03 N Lat, 15 18 E Long) on a moderately deep Calcixerollic Xerochrepts soil. The soil characteristics were: clay 24.0%, sand 35.0%, silt 41.0%, organic matter 1.20%, pH 8.0, total N 1 1 3 0.5%, available P 48 mg kg , exchangeable K 940 mg kg , bulk density 1.3 g cm , field capacity 1 1 ( 0.03 MPa) 0.25 g g and wilting point ( 1.5 MPa) 0.15 g g . Fallow preceded the cultivation of tomato crops. In a randomized complete block experimental design with three replicates, seven irrigation treatments were studied (Table 1). The cultivar Hypeel F1 (Seminis Inc., Oxnard, CA, USA) of the processing tomato (Solanum lycopersicum L.) was used for the experiment. Plants were transplanted at the four-leaf stage on June 9 in a single plot of 38.4 m (4.8 m 8 m). Plants were spaced at 0.75 m between rows and 0.40 m within rows, resulting in a plant 2 1 density of approximately 3.3 plants m . Before transplanting 75, 100 and 100 kg ha of N (as ammonium sulphate), P O (as mineral perphosphate) and K O (as potassium sulphate), respectively, 2 5 2 were distributed. Approximately 30 days after transplant (DAT), a further 75 kg ha of N (as ammonium nitrate) was supplied as top dressing. Agronomy 2020, 10, 800 3 of 17 Table 1. Description of the dierent irrigation treatments applied to the processing tomato cv. Hypeel F1. ETc: daily evapotranspiration. Seasonal Volume of Water Irrigation Treatment Description 3 1 (m ha ) NI (no irrigation) Irrigation up to seedling establishment 450 F (full, control) Long-season irrigation, 100% ETc restoration 4050 D (deficit) Long-season irrigation, 50% ETc restoration 2250 Short-season irrigation, early cut-o at the onset of FE (full, early) 1210 flowering, 100% ETc restoration Short-season irrigation, early cut-o at the onset of DE (deficit, early) 830 flowering, 50% ETc restoration FFL (full, flowering) Irrigation only during flowering, 100% ETc restoration 2090 DFL (deficit, flowering) Irrigation only during flowering, 50% ETc restoration 1270 A drip-irrigation system was used. At the time of transplanting, the irrigation water was supplied to fulfil the field capacity at approximately 0.3 m of depth. Thereafter, the volume of irrigation water to supply was determined on the basis of the maximum available soil water content (ASWC) in the first 0.4 m of soil, where most of roots are expected to grow, calculated with the following formula: V = 0.66 (FC WP) D (1) where V = water amount (approximately 34 mm), 0.66 = fraction of promptly available soil water permitting unrestricted evapotranspiration, FC = soil water at field capacity (25% of soil dry weight), WP = soil water at wilting point (15% of soil dry weight), = bulk density (g cm ) and D = soil depth (0.4 m). Irrigation water was supplied when the sum of daily evapotranspiration (ET ) corresponded to V: ETc = ET k k (2) 0 p c where ET = reference ET, measured by means of a class A pan (mm), k = pan coecient, equal to 0.80 in a semi-arid environment and k = crop coecient [3]. Total amount of water distributed to each irrigation treatment is reported in Table 1. No chemical herbicides were used for weed control. A hand-weeding was performed once only, since the crop covered the soil, and weeds could no longer grow. The following meteorological variables were recorded daily throughout the crop-growing season: air temperature, rainfall, class A pan evaporation, using a data logger (CR10, Campbell Scientific, Logan, UT, USA) located approximately 50 m from the experimental field. Along the experiment from mid-July, when plants started to flower, to the end of August, when they were at the ripening stage of fruits, soil water content was measured, at 2 to 3-day intervals, by means of gypsum blocks (Soilmoisture Equipment Corp., Santa Barbara, CA, USA) located at 0.15 and 0.30-m soil depths in all replicates of each irrigation treatment. Thereafter, the available soil water content (ASWC), as a percentage of the maximum available water and according to the following formula, was calculated [17]: ASWC = (WC WP)/(FC WP) 100 (3) 1 1 where WC = soil water content (g g dry soil), FC = soil water content at field capacity (0.25 g g dry soil) and WP = soil water content at the wilting point (0.15 g g dry soil). ASWC ranged between 100% (field capacity) and 0% (wilting point). 2.2. Physiological Measurements 2 1 2 1 Leaf transpiration (E, mmol H O m s ) and stomatal conductance (g , mol m s ) were 2 s measured along the growing season at 10 subsequent dates after transplanting (DAT) from mid-July to Agronomy 2020, 10, 800 4 of 17 the end of August by means of a null balance “steady-state” porometer (Model LI-1600, Li-Cor, Inc., Lincoln, NE, USA). Measurements were made on clear sunshine hours between 11:00 h and 13:00 (solar time) in fully developed and healthy leaves. One reading was carried out on three randomly chosen, fully expanded young leaves from each plot. Leaf water potential ( , MPa) was also measured before sunrise (03:00–05:00 h solar time, “pre-dawn” water potential) at 3–5-day intervals starting in August up to early September by means of a pressure chamber (Soilmoisture Equipment Corp., Santa Barbara, CA, USA). Briefly, a leaflet was excised at the petiole level from a young fully expanded leaf (on the top part of the plant) using a razor blade. The leaflet was partly sealed in the pressure chamber, with the cut end of the petiole protruding through the seal. The chamber was pressurized with compressor gas until the appearance of water in the cut surface (detectable using a magnifying glass). At that point, the pressure was recorded. As for E and g , one reading was carried out on three randomly chosen, fully expanded young leaves from each plot. 2.3. Plant Measurements At five dates, from middle of July to early August (34, 38, 46, 53 and 60 DAT), two representative plants were sampled destructively from each experimental plot, and flowers and fruits (when present) were counted. After that, plant parts (root, stem, leaves, flowers and fruits when present) were dried in a thermo-ventilated oven at 65 C until constant weight (about 3 days) for dry matter (DW) measurement (g DW plant ). 2.4. Calculations The crop was hand-harvested when the ripe fruit rate reached ~95% (early September). At harvest, 1 3 total fruit yield (t ha ) was measured, and irrigation water use eciency (IWUE, kg m ) was calculated from the dierent irrigation treatments as the ratio of total yield (kg) and total water applied by irrigation (m ) [13]. 2.5. Statistical Analyses Data of physiological (E, g and ) and plant production (number of flowers, number of fruits, shoot dry weight, root dry weight and fruit production) measurements were subjected to a one-way repeated-measures analysis of variance (ANOVA) where date of measurement represents the within-subjects factor and the irrigation treatment the between-subjects factor (SPSS, PASW Statistics 18). When the Mauchly’s sphericity test failed to meet the assumption of sphericity, the univariate results were adjusted by using the Greenhouse-Geisser Epsilon and the Huynh-Feldt Epsilon correction factors. Following the univariate test satisfying the sphericity for within-subject eects, the F-values and associated p-values for between-subject eects were tested. Means were separated by the Tukey’s test at a 95% confidence level. For data of the number of flowers and number of fruits per plant, shoot dry weight and root dry weight, a supplemental ANOVA was carried out separately for the date of measurement. Data of final yield and irrigation water use eciency (IWUE) were statistically analyzed by a one-way analysis of variance (ANOVA) using CoStat version 6.003 (CoHort Software, Monterey, CA, USA). Dierences between means were evaluated as described above. Plant dry weight variations over time were interpolated by a nonlinear iterative regression method (SigmaPlot11, Systat Software Inc., San Jose, CA, USA) using the following exponential function: y = (4) 1 + 0 Agronomy 2020, 10, x FOR PEER REVIEW 5 of 18 Data of final yield and irrigation water use efficiency (IWUE) were statistically analyzed by a one-way analysis of variance (ANOVA) using CoStat version 6.003 (CoHort Software, Monterey, CA, USA). Differences between means were evaluated as described above. Plant dry weight variations over time were interpolated by a nonlinear iterative regression method (SigmaPlot11, Systat Software Inc., San Jose, CA, USA) using the following exponential function: Agronomy 2020, 10, 800 5 of 17 𝑦 = (4) 1 + ( ) where a = maximal value of y, x = time (DAT), x = time (DAT) to reach 50% of maximal value a where a = maximal value of y, x = time (DAT), x0 = time (DAT) to reach 50% of maximal value a and and b = fitting parameter of the curve. Thereafter, using values of the curve, crop growth rate (CGR, b = fitting parameter of the curve. Thereafter, using values of the curve, crop growth rate (CGR, g DW 1 1 g DW plant d ) was calculated as follows: −1 −1 plant d ) was calculated as follows: CGR = (W W )/(t t ) (5) 2 1 1 2 𝐶𝐺𝑅 = (𝑊 − 𝑊 )/(𝑡 − 𝑡 ) (5) 2 1 1 2 where W2 and W1 are the values of the plant dry weight (g) at times t2 and t1, respectively, on the where W and W are the values of the plant dry weight (g) at times t and t , respectively, on the 2 1 2 1 curve. Finally, the maximum value of CGR (CGRmax) was considered [18]. curve. Finally, the maximum value of CGR (CGRmax) was considered [18]. The relationships between leaf transpiration and stomatal conductance measured in plants The relationships between leaf transpiration and stomatal conductance measured in plants under under no water limitation (F treatment) and vapor pressure deficit (VPD, kPa) in the atmosphere no water limitation (F treatment) and vapor pressure deficit (VPD, kPa) in the atmosphere were were described by using a nonlinear function (SigmaPlot11, Systat Software Inc., San Jose, CA, USA). described by using a nonlinear function (SigmaPlot11, Systat Software Inc., San Jose, CA, USA). VPD VPD was calculated using air relative humidity (RH, %) and air temperature (°C) recorded by the was calculated using air relative humidity (RH, %) and air temperature ( C) recorded by the same same “steady-state” porometer at the moment of physiological measurements [19]. “steady-state” porometer at the moment of physiological measurements [19]. 3. Results 3. Results 3.1. Meteorological Trend 3.1. Meteorological Trend The meteorological course during the crop-growing season was typical of the semi-arid The meteorological course during the crop-growing season was typical of the semi-arid Mediterranean environment, with a hot and dry summer (Figure 1). Mediterranean environment, with a hot and dry summer (Figure 1). 50 11 rain 10 Tmax Tmin ET 0 1 0 0 0 4 8 12 16 20 24 28 32 36 40 44 48 52 56 60 64 68 72 76 80 84 88 92 Days after transplant Figure 1. Meteorological course (maximum and minimum air temperatures, rainfall, and reference Figure 1. Meteorological course (maximum and minimum air temperatures, rainfall, and reference evapotranspiration (ET0)) recorded during the field experiment. evapotranspiration (ET )) recorded during the field experiment. Maximum Maximum temperatur temperature e ranged ranged between betwee 27.6 n 27.6 C (in °C June) (in Ju and ne) 43.4 andC 43.4 (in July), °C (in witJu h the ly), minimum with the between minimum 14.0 between C (in14.0 June) °Cand (in 22.4 June) C and (in 22. July). 4 °C T(i otal n Jul rainfall y). Total up rto ainfall August up to was August <10 mm; was ther <10 efor mm e, ; soil therefore, water soi availability l water avail wasabi totally lity w due as tto otal irrigation. ly due toRefer irriga ence tion. evapotranspiration Reference evapotranspir (ET ) follows ation (ET the 0) −1 course follows of th the e course air temperatur of the air e,tem and perat values ure, exceeding and values 9 mm exceed d ing wer9 e mm recor d ded were in the recorded first 10-day in the period first and 10-dat aythe perio end d a of nd July at t . he end of July. 3.2. Soil Water Content Soil water content fluctuated during the growth season, according to the irrigation time. It maintained the highest levels at both soil depths under the F regime throughout the crop-growing season (Figure 2). However, even under these experimental conditions, despite continuous irrigation, soil water deficits sometimes exceeded 66% (threshold for irrigation). Indeed, the volume of water supplied by irrigation (approximately constant) was indirectly calculated on the ETc basis, not on the actual soil water content at the irrigation time [20]. Therefore, it is likely that this volume of water sometimes was not adequate to fill the soil up to field capacity even under the F regime. Air temperature (°C) Rainfall, ET (mm) 0 Agronomy 2020, 10, x FOR PEER REVIEW 6 of 18 3.2. Soil Water Content Soil water content fluctuated during the growth season, according to the irrigation time. It maintained the highest levels at both soil depths under the F regime throughout the crop-growing season (Figure 2). However, even under these experimental conditions, despite continuous irrigation, soil water deficits sometimes exceeded 66% (threshold for irrigation). Indeed, the volume of water supplied by irrigation (approximately constant) was indirectly calculated on the ETc basis, not on the actual soil water content at the irrigation time [20]. Therefore, it is likely that this volume of water Agronomy 2020, 10, 800 6 of 17 sometimes was not adequate to fill the soil up to field capacity even under the F regime. 15 cm NI 30 cm 100 0 80 F 15 cm Plot 1 Upper specification 100 30 cm 100 0 FE 100 0 DE 100 0 FFL 100 0 DFL 30 35 40 45 50 55 60 65 70 75 80 85 90 Days after transplant Figure 2. Available soil water contents at depths of 15 cm (red line) and 30 cm (blue line) in each Figure 2. Available soil water contents at depths of 15 cm (red line) and 30 cm (blue line) in each irrigation treatment. Constant horizontal short-dash line indicates the minimum threshold of the irrigation treatment. Constant horizontal short-dash line indicates the minimum threshold of the available soil water content. NI: no irrigation, F: full, D: deficit, FE: full early, DE: deficit early, FFL: full available soil water content. NI: no irrigation, F: full, D: deficit, FE: full early, DE: deficit early, FFL: flowering and DFL: deficit flowering. full flowering and DFL: deficit flowering. In the D treatment, irrigation tended to fulfil the upper layers of the soil. Under no irrigation In the D treatment, irrigation tended to fulfil the upper layers of the soil. Under no irrigation during flowering (NI, FE and DE), soil water contents during the measurements period were always during flowering (NI, FE and DE), soil water contents during the measurements period were always beneath the field capacity at both soil depths. In plots irrigated only at flowering, soil water contents beneath the field capacity at both soil depths. In plots irrigated only at flowering, soil water contents exhibited trends similar to that of the F regime, although, in FFL, only in the upper layer of soil. In DFL, the water content kept higher in the upper layers of the soil (15 cm), up to approximately 50 DAT. However, just after irrigation suspension (at 54 DAT), the soil water content in both FFL and DFL dropped to levels lower than the field capacity already at 57 DAT. Available soil water content (%) Agronomy 2020, 10, x FOR PEER REVIEW 7 of 18 exhibited trends similar to that of the F regime, although, in FFL, only in the upper layer of soil. In DFL, the water content kept higher in the upper layers of the soil (15 cm), up to approximately 50 DAT. However, just after irrigation suspension (at 54 DAT), the soil water content in both FFL and DFL dropped to levels lower than the field capacity already at 57 DAT. Agronomy 2020, 10, 800 7 of 17 3.3. Course of Leaf Transpiration and Stomatal Conductance 3.3. Course of Leaf Transpiration and Stomatal Conductance ANOVA evidenced a highly significant effect of the irrigation treatment (I) and time of measurement (T) upon all the physiological parameters examined (p ≤ 0.001) (Table 2). The significant ANOVA evidenced a highly significant eect of the irrigation treatment (I) and time of measurement interaction I × T (p ≤ 0.001) suggests that the physiological response of tomato plants to changing soil (T) upon all the physiological parameters examined (p 0.001) (Table 2). The significant interaction water contents varies with the time of measurement. I T (p 0.001) suggests that the physiological response of tomato plants to changing soil water contents varies with the time of measurement. Table 2. Repeated-measures ANOVA for main effects and interactions on the physiological traits. Table 2. Repeated-measures ANOVA for main eects and interactions on the physiological traits. gs ψ Source df df E Adj MS g Adj MS Source df df Irrigation (I) 6 1615.2 *** 3.829 *** 6 1.350 *** Adj MS Adj MS Time (T) 9 1497.9 *** 3.367 *** 8 0.150 *** Irrigation (I) 6 1615.2 *** 3.829 *** 6 1.350 *** I × T 54 408.6 *** 0.811 *** 48 0.040 *** Time (T) 9 1497.9 *** 3.367 *** 8 0.150 *** I T 54 408.6 *** 0.811 *** 48 0.040 *** Error (T) 126 267.8 0.823 112 0.011 Error (T) 126 267.8 0.823 112 0.011 Error 14 22.6 0.119 14 0.006 Error 14 22.6 0.119 14 0.006 Leaf transpiration—E, stomatal conductance—gs and predawn water potential—ψ. Degree of Leaf transpiration—E, stomatal conductance—g and predawn water potential— . Degree of freedom (df) and freedom (df) and adjusted mean square (Adj MS). Significant at p ≤ 0.001 (***). adjusted mean square (Adj MS). Significant at p 0.001 (***). Leaf transpiration (E) and stomatal conductance (gs) were measured from approximately a Leaf transpiration (E) and stomatal conductance (g ) were measured from approximately a month after transplanting (when plants were at the floral initiation and water treatments were overall month after transplanting (when plants were at the floral initiation and water treatments were overall differentiated) onward (Figure 3). In all the experimental situations, E exhibited an increasing trend dierentiated) onward (Figure 3). In all the experimental situations, E exhibited an increasing trend from the initial measurement up to approximately 50 DAT, when the first fruit buds were quite from the initial measurement up to approximately 50 DAT, when the first fruit buds were quite visible. −2 −1 visible. After that, E steeply decreased down to values ≤5.55 mmol H2O m s measured at 61 DAT 2 1 After that, E steeply decreased down to values 5.55 mmol H O m s measured at 61 DAT in all in all water treatments. water treatments. 2 1 2 1 Figure 3. Course of leaf transpiration (E, mmol H O m s ) and stomatal conductance (g , mol m s ) during the growth period in processing tomatoes cv. Hypeel F1 under dierent irrigations. This was probably due to quite a low air humidity and quite a high air temperature recorded in that period (between 52 and 62 DAT), which determined a high VPD and, consequently, a high water demand from the atmosphere. This, in turn, induced a partial stomatal closure and a reduced E even Agronomy 2020, 10, x FOR PEER REVIEW 8 of 18 −2 −1 −2 −1 Figure 3. Course of leaf transpiration (E, mmol H2O m s ) and stomatal conductance (gs, mol m s ) during the growth period in processing tomatoes cv. Hypeel F1 under different irrigations. This was probably due to quite a low air humidity and quite a high air temperature recorded in that period (between 52 and 62 DAT), which determined a high VPD and, consequently, a high water Agronomy 2020, 10, 800 8 of 17 demand from the atmosphere. This, in turn, induced a partial stomatal closure and a reduced E even under the unrestricted soil water conditions in F. Indeed, an exponential function well describes the under the unrestricted soil water conditions in F. Indeed, an exponential function well describes the overall changes in E and gs measured in plants under good soil water conditions (those of F), overall changes in E and g measured in plants under good soil water conditions (those of F), according according to the variation in VPD (Figure 4). to the variation in VPD (Figure 4). −2 −1 2 1 Figure 4. Variation of leaf transpiration (E, mmol H2O m s ) and stomatal conductance (gs, mol Figure 4. Variation of leaf transpiration (E, mmol H O m s ) and stomatal conductance (g , 2 s −2 −1 2 1 m s ) in relation to the increase of the vapor pressure deficit (VPD, kPa) in the atmosphere under mol m s ) in relation to the increase of the vapor pressure deficit (VPD, kPa) in the atmosphere under full irrigation (F treatment) in processing tomatoes cv. Hypeel F1. Measurements were made between full irrigation (F treatment) in processing tomatoes cv. Hypeel F1. Measurements were made between 2 −2 1 −1 11:00 and 13:00, with PAR (Photosynthetic active radiation) varying from 1500 to 2000 μmol m s as 11:00 and 13:00, with PAR (Photosynthetic active radiation) varying from 1500 to 2000 mol m s as measured by the PAR sensor of the porometer. Symbols represent the observed values. Black vertical measured by the PAR sensor of the porometer. Symbols represent the observed values. Black vertical bars bars rrepr epresent esent the the s standar tandard d err eror ror. . The course of this function indicates that an increase in the VPD determines a progressive raise in The course of this function indicates that an increase in the VPD determines a progressive raise both parameters up to a maximum (at a VPD of approximately 1.9 kPa for E and 1.7 kPa for g on the in both parameters up to a maximum (at a VPD of approximately 1.9 kPa for E and 1.7 kPa for gs on curve). Beyond this, the values of E and g start to decline down to a minimum at 2.4 kPa of the VPD. the curve). Beyond this, the values of E an s d gs start to decline down to a minimum at 2.4 kPa of the Later on, the leaf transpiration increased again except under severe soil water deficit conditions VPD. (NI, FE and DE), thus slowly decreasing down to the minimum measured late in the growing season Later on, the leaf transpiration increased again except under severe soil water deficit conditions (82 DAT), when plants started to senesce. (NI, FE and DE), thus slowly decreasing down to the minimum measured late in the growing season Same trend was observed for stomatal conductance, although its maximum value was achieved (82 DAT), when plants started to senesce. later (approximately 55 DAT) than that measured for E. Same trend was observed for stomatal conductance, although its maximum value was achieved According to the water supply, plots continuously irrigated (F and D) and those receiving water at later (approximately 55 DAT) than that measured for E. flowering only (FFL and DFL) maintained higher rates of leaf transpiration and stomatal conductance According to the water supply, plots continuously irrigated (F and D) and those receiving water 2 1 over those exposed to a drying soil (NI, FE and DE), with maximum values11 mmol H O m s at flowering only (FFL and DFL) maintained higher rates of leaf transpiration and stomatal 2 1 (for E) and 0.56 mol m s (for g ) in all. conductance over those exposed to a drying soil (NI, FE and DE), with maximum values ≥11 mmol −2 −1 −2 −1 H2O m s (for E) and 0.56 mol m s (for gs) in all. 3.4. Course of “Predawn” Water Potential 3.4. Course of “Predawn” Water Potential The course of water potential ( ) at the first hours of the day (“predawn”) was measured under nonlimiting air temperature and relative humidity conditions to the plant-water flux (Figure 5). The course of water potential (ψ) at the first hours of the day (“predawn”) was measured under Predawn was measured during the growing season, starting from the first days of August (55 DAT), nonlimiting air temperature and relative humidity conditions to the plant-water flux (Figure 5). when plants were near the end of the flowering period, to early September (88 DAT). Under rainfed Predawn ψ was measured during the growing season, starting from the first days of August (55 conditions (NI), predawn kept always the lowest values (<