Responses to Saturation Deficit in a Stand of Groundnut (Arachis hypogaea L.). 2. Growth and Development

Stands of groundnut were grown in four glasshouses with themaximum saturation deficit (D) of the air limited to 1.0, 2.0,2.5 or 3.0 kPa. The soil was near field capacity when plantsemerged and no water was applied thereafter. In a fifth glasshouse,a stand was grown at low D on soil irrigated to field capacityevery few days. Developmental processes such as timing of flowering, peggingand pod formation were unaffected by D, but the numbers of branches,flowers and pegs were reduced in the drier treatments. Measurementsduring the first 30 d showed that in the drier treatments leafgrowth was reduced, and the partitioning of dry matter intoroots was enhanced. In the unirrigated stands, dry matter production in shoots wasreduced by 40 per cent as the maximum D increased from 1.0 to3.0 kPa. Growth was affected through reductions both in leafarea (and therefore light interception) and in the productivityper unit of light intercepted. These responses to D and soilwater were linked to changes in bulk water potential of leaves. Productivity per unit of water transpired (q) decreased withincreasing D. The product of q and the mean daytime value ofthe difference in vapour pressure between leaf and air was moreconservative than q, and ranged from 3.1 to 5.6 g kPa kg^–1. Groundnut, Arachis hypogaea L., saturation deficit, growth, development, light interception, water use efficiency     

Soil water deficits decrease the internal conductance to CO2 transfer but atmospheric water deficits do not

The internal conductance to CO₂ supply from substomatal cavitiesto sites of carboxylation poses a large limitation to photosynthesis.It is known that internal conductance is decreased by soil waterdeficits, but it is not known if it is affected by atmosphericwater deficits (i.e. leaf to air vapour pressure deficit, VPD).The aim of this paper was to examine the responses of internalconductance to atmospheric and soil water deficits in seedlingsof the evergreen perennial Eucalyptus regnans F. Muell and theherbaceous plants Solanum lycopersicum (formerly Lycopersiconesculentum) Mill. and Phaseolus vulgaris L. Internal conductancewas estimated with the variable J method from concurrent measurementsof gas exchange and fluorescence. In all three species steady-statestomatal conductance decreased by 30% as VPD increased from1 kPa to 2 kPa. In no species was internal conductance affectedby VPD despite large effects on stomatal conductance. In contrast,soil water deficits decreased stomatal conductance and internalconductance of all three species. Decreases in stomatal andinternal conductance under water deficit were proportional,but this proportionality differed among species, and thus therelationship between stomatal and internal conductance differedamong species. These findings indicate that soil water deficitsaffect internal conductance while atmospheric water deficitsdo not. The reasons for this distinction are unknown but areconsistent with soil and atmospheric water deficits having differingeffects on leaf physiology and/or root–shoot communication. Key words: Carbon dioxide, drought, internal conductance, mesophyll conductance, photosynthesis, stomatal conductance, transfer conductance, vapour pressure deficit, water deficit Received 11 October 2007; Revised 9 November 2007 Accepted 15 November 2007     

Rectifier-like Activities of Roots of Two Desert Succulents

Axial and radial water flows for roots in response to appliedhydrostatic pressure drops, water loss from roots after variousperiods of drying, and development of new roots after rewettingdroughted plants were examined for two sympatric desert succulents.Agave deserti Engelm. and Ferocactus acanthodes (Lemaire) Brittonand Rose. For a 40 kPa hydrostatic pressure drop applied to20 mm long root pieces, radial water flows from the epidermisto the root xylem were 2- to 5-fold greater at the tip thanat midlength and were much less than axial flows along the xylem.Upon drying detached roots in air at 20 °C and a water vapoursaturation deficit of 1.2 kPa (50% relative humidity), radialwater flow decreased more than 10-fold in 3–6 h, and couldrecover to the original level 6 h after rewetting. The rateof water loss from attached roots of plants dried in air at20 °C and a 1.2 kPa saturation deficit decreased about 200-foldin 72 h, which would greatly limit water loss from the plantto a drying soil. At 96 h after rewetting roots of A. desertithat had been exposed to air at 20 °C and a 1.2 kPa saturationdeficit for 120 h, rehydration of existing roots and developmentof new roots contributed about equally to water uptake by thewhole plant. In summary, roots of these desert succulents canreadily take up water from a wet soil but do not lose much waterto a dry soil, thus effectively acting like rectifiers withrespect to plant-soil water movement. Key words: Agave, Cactus, Drought, Root, Water flow, Xylem     

Dependence of Yields of Wheat Varieties on their Leaf Area Durations

In a field experiment three wheat varieties: autumn-sown CappelleDesprez, Prestige, both autumn-sown and spring-sown, and spring-sownJufy I, each supplied with 0.5 or 1.0 cwt nitrogen/acre (6₃or 126 kg/ha), had grain yields nearly proportional to theirLeaf Area Durations (D) during grain development. Squarehead'sMaster had a smaller grain yield relative to its total D, butwith 0.5 cwt N/acre the ratio of its grain yield to D of partsabove the flag leaf node (D_F) was similar to the other varieties.The difference in this ratio between varieties was less whenD_Fwas calculated from anthesis than from ear emergence to ripening.Squarehead’s Master with 1.0 cwt N/acre had a smallerratio of grain yield to D_F than other treatments, implying lessgrain per ear relative to D_Y per shoot, perhaps because of lodging,or because factors limiting size of ears restricted their abilityto accept all the assimilate the shoots could produce with thisamount of N.     

Root Growth and Water Uptake by Maize Plants in Drying Soil

Sharp, R. E and Da vies, W. J. 1985. Root growth and water uptakeby maize plants in drying soil.— J. exp. Bot. 36: 1441–1456. The influence of soil drying on maize (Zea mays L.) root distributionand use of soil water was examined using plants growing in thegreenhouse in soil columns. The roots of plants which were wateredwell throughout the 18 d experimental period penetrated thesoil profile to a depth of 60 cm while the greatest percentageof total root length was between 20–40 cm. High soil waterdepletion rates corresponded with these high root densities.Withholding water greatly restricted root proliferation in theupper part of the profile, but resulted in deeper penetrationand higher soil water depletion rates at depth, compared withthe well watered columns. The deep roots of the unwatered plantsexhibited very high soil water depletion rates per unit rootlength. Key words: Maize, roots, water deficit, soil water depletion     

Global change‐type drought‐induced tree mortality: vapor pressure deficit is more important than temperature per se in causing decline in tree health

Drought‐induced tree mortality is occurring across all forested continents and is expected to increase worldwide during the coming century. Regional‐scale forest die‐off influences terrestrial albedo, carbon and water budgets, and land‐surface energy partitioning. Although increased temperatures during drought are widely identified as a critical contributor to exacerbated tree mortality associated with “global‐change‐type drought”, corresponding changes in vapor pressure deficit (D) have rarely been considered explicitly and have not been disaggregated from that of temperature per se. Here, we apply a detailed mechanistic soil–plant–atmosphere model to examine the impacts of drought, increased air temperature (+2°C or +5°C), and increased vapor pressure deficit (D; +1 kPa or +2.5 kPa), singly and in combination, on net primary productivity (NPP) and transpiration and forest responses, especially soil moisture content, leaf water potential, and stomatal conductance. We show that increased D exerts a larger detrimental effect on transpiration and NPP, than increased temperature alone, with or without the imposition of a 3‐month drought. Combined with drought, the effect of increased D on NPP was substantially larger than that of drought plus increased temperature. Thus, the number of days when NPP was zero across the 2‐year simulation was 13 or 14 days in the control and increased temperature scenarios, but increased to approximately 200 days when D was increased. Drought alone increased the number of days of zero NPP to 88, but drought plus increased temperature did not increase the number of days. In contrast, drought and increased D resulted in the number of days when NPP = 0 increasing to 235 (+1 kPa) or 304 days (+2.5 kPa). We conclude that correct identification of the causes of global change‐type mortality events requires explicit consideration of the influence of D as well as its interaction with drought and temperature.     

Quantitative analysis of the combined effects of temperature, evaporative demand and light on leaf elongation rate in well-watered field and laboratory-grown maize plants

The respective effects of meristem temperature, vapour pressuredeficit (VPD) and photosynthetic photon flux density (PPFD)on leaf elongation rate (LER) of maize, in the absence of waterdeficit in the soil have been quantified. This analysis wascarried out in a series of field experiments in northern andsouthern France over several seasons and years, and in growthchamber experiments. LER was measured with 10 min steps, togetherwith meristem temperature, VPD and PPFD at leaf level in threetypes of experiments: in growth chamber experiments with stepsin PPFD or VPD at constant meristem temperature, in growth chamberexperiments with several combinations of constant, but contrasting,PPFDs, VPDs and meristem temperatures, and in the field withfluctuating conditions, (i) When evaporative demand was low(night or day with low air VPD), LER was only linked to meristemtemperature, regardless of other climatic conditions, (ii) Lighthad no effect per se on LER in the range from 0 to 1500 molm^–2 s^–1 for time-scales longer than 2 h, providedthat its indirect effects on meristem temperature and on evaporativedemand were corrected (in the growth chamber) or taken intoaccount (in the field), and provided that cumulated PPFD overa weekly time-scale was compatible with field conditions, (iii)Evaporative demand sensed by growing leaves, as estimated bymeristem-to-air vapour pressure difference, markedly affectedLER in the range from 1–4 kPa, at all time-scales understudy, with a unique relationship in the growth chamber (constantconditions) and in the field (fluctuating conditions). Thiseffect was only observed when PPFD was high enough for stomatato open. The negative effect of evaporative demand on LER wasprobably not due to long distance root-to-shoot signalling,since soil was wet, calculated root water potential remainedclose to 0 MPa and concentration of ABA in the xylem sap wasvery low. Therefore, it is proposed to model maize LER witha two-step process, involving the calculation of the maximumLER at a given meristem temperature and then the calculationof the reduction in LER due to evaporative demand. Joint analysisof the whole set of data by using the two equations yieldeda r² of 0.75. This two-step process would be more accurate thanthe provision of LER from temperature only in cases where airVPD frequently exceeds 2 kPa. Key words: Leaf growth, light, evaporative demand, temperature, thermal time, water deficit, ABA, Zea mays L.     

Influence of Saturation Deficit on Leaf Production and Expafision in Stands of Groundnut-{Arachis hypogaea L.) Grown Without Irrigation

The response of leaf area expansion to atmospheric saturationdeficit (SD) and soil moisture deficit was examined in termsof leaf water potential (₁) and turgor potential (_p), as partof a wider study of the effects of SD on groundnut growth. Standsof plants were grown at four levels of SD and without irrigationin controlled environment glasshouses. A fifth stand was grownat low SD on soil kept irrigated to field capacity. Large saturation deficits accelerated the depletion of soilmoisture reserves in the unirrigated stands and greatly reducedleaf area index, particularly in the driest treatment. Leafnumber per plant and leaf size both decreased as SD increased,but the effect on leaf size was greater than on number. SD hadless effect than soil water deficit on leaf production. Turgorpotential and leaf extension rate (R) were both reduced at highsaturation deficits and R was linearly related to _p between0900 and 1600 h. However, leaf extension rate and turgor potentialwere poorly correlated between 0400 and 0700 h in the driesttreatment. Arachis hypogaea L., groundnut, saturation deficit, leaf growth, canopy development     

Water transport and the distribution of aquaporin-1 in pulmonary air spaces

Effros, R. M., C. Darin, E. R. Jacobs, R. A. Rogers, G. Krenz, and E. E. Schneeberger. Water transport and thedistribution of aquaporin-1 in pulmonary air spaces.J. Appl. Physiol. 83(3): 1002-1016, 1997.Recent evidence suggests that water transport between the pulmonary vasculature and air spaces can be inhibited byHgCl₂, an agent that inhibitswater channels (aquaporin-1 and -5) of cell membranes. In the presentstudy of isolated rat lungs, clearances of labeled(³HOH) and unlabeled water werecompared after instillation of hypotonic or hypertonic solutions intothe air spaces or injection of a hypotonic bolus into the pulmonaryartery. The clearance of ³HOHbetween the air spaces and perfusate after intratracheal instillation and from the vasculature to the tissues after pulmonary arterial injections was invariably greater than that of unlabeled water, indicating that osmotically driven transport of water is limited bypermeability of the tissue barriers rather than the rate of perfusion.Exposure to 0.5 mM HgCl₂ in theperfusate and air-space solution reduced the product of the filtrationcoefficient and surface area(P_fS)of water from the air spaces to the perfusate by 28% afterinstillation of water into the trachea. In contrast, perfusion of 0.5 mM HgCl₂ in air-filled lungs reducedP_fSof the endothelium by 86% after injections into the pulmonary artery, suggesting that much of the action of this inhibitor is on the endothelial surfaces. Confocal laser scanning microscopy demonstrated that aquaporin-1 is on mouse pulmonary endothelium. No aquaporin-1 wasfound on alveolar type I cells with immunogold transmission electronmicroscopy, but small amounts were present on some type II cells.

     

Mechanisms of Inhibition of Water Movement in Anaerobically Treated Roots of Zea mays L.

Changes in water flux (Jv) across detopped, 7-d-old, maize rootswere characterized during the initial 24 h of being made anoxicby exposure to an anaerobic nutrient solution. Suction (50 kPa)was applied to the xylem and samples of the xylem sap were collectedat intervals and the osmolality and ionic content were measured. Values of Jv through anoxic roots fell below those of aerobiccontrols 1 h after the equilibrium oxygen partial pressure inthe bathing medium dropped below 20 kPa (air = 20.6 kPa). Thereduction in Jv was due primarily to a nullification of thediurnal rhythm in hydraulic conductivity (Lp) that was measuredin aerobic roots. However, about one-quarter of the reductionin Jv could be accounted for by a smaller osmotic componentof the driving force () on water movement. The significance of changes in Jv in anoxic roots is discussedin terms of the reliability of estimates of Lp, the reflectioncoefficient () and . Key words: Anaerobiosis, hydraulic conductivity, osmotic potential, water     

Effects of Drought on Water Relations, Mineral Uptake, Water-soluble Carbohydrate Accumulation and Survival of Two Contrasting Populations of Cocksfoot (Dactylis glomerata L.)

The role physiological responses in survival of prolonged soilmoisture deficit was investigated in vegetative plants of twoDactylis glomerata populations: KM2 (drought-resistant) andLutetia (susceptible). The plants were grown in 1 m-deep soilcolumns in a controlled environment. After 56 d of full irrigation,water was withheld for 80 d, by which time all soil moisturehad been consumed; the plants were then rewatered for a further19 d. As drought progressed, leaf extension decreased to zero,water status declined, and water-soluble carbohydrates (WSC)at first increased and then decreased. The most pronounced differencesbetween the two populations was that all KM2 tillers survivedthe drought, but 34% of Lutetia tillers died. In comparisonwith Lutetia, KM2 was characterized by (a) slower shoot growthrate, (b) greater root density at depth, (c) maintenance ofhigher lamina relative water content, (d) greater osmotic adjustmentin leaf bases, (e) higher concentration of WSC in tiller bases,(f) greater ability to export WSC out of dying leaves, (g) lowercontent of metal ions but improved maintenance of P status,and (h) lower proline:amino acid ratio. The contribution ofthese responses to tiller survival under severe drought in controlledenvironments is contrasted with performance and persistenceof swards in the field in the harsher Mediterranean environment.Copyright1995, 1999 Academic Press Dactylis glomerata L., cocksfoot, water-stress, osmotic asjustment, drought survival, root-growth, water-soluble carbohydrates, phosphate, proline, variety comparison     

Saturation Deficit, Canopy Formation and Function in Sorghum bicolor (L.)

Hamdi, Q. A., Harris, D. and Clark, J. A. 1987. Saturation deficit,canopy formation and function in Sorghum bicolor (L.).—J.exp. Bot. 38: 1272–1283. Stands of two sorghum genotypes, SPV 354 and MK. 35-1, weregrown in controlled-environment glasshouses at three levelsof saturation vapour pressure deficit (SD), at the same temperatureand with unrestricted soil moisture. Vegetative growth was monitoredby growth analysis and non-destructive measurements were madeof leaf appearance, leaf extension and final size, and fractionallight interception. Rates of leaf appearance were reduced athigh SD in both genotypes, although this may have been an artefactof the method of measurement, and MK 35-1 produced leaves moreslowly than SPV 354. Leaf extension was also slowed as SD increasedand, since the duration of extension for individual leaves ofa given age remained constant, resulted in smaller leaf areaindices (L) in dry air than in humid air. The cumulative interceptionof radiation and the dry matter/radiation quotient (e) bothdecreased as SD increased. Key words: Sorghum, saturation deficit, canopy formation     

Resistance to Water Loss in the Mesophyll of Leek (Allium porruni)

Measurement of the rate of water loss and the gradient in water-vapourconcentration from the evaporating surface to the air enabledcalculation of the resistance to water loss from the leaf mesophyllof leek (Allium porruni) and from green blotting-paper. Theadditional resistance found in the case of mesophyll estimatesthe mesophyll cell-wall resistance (wall resistance). Wall resistancewas, however, small, less than 0.09 sec cm^–1 in turgidmesophyll and only 0.15 sec cm^–1 greater when the mesophyllwater deficit was 50 per cent. Results are discussed in relationto the evidence of other workers indicating greater resistancesto water loss in the mesophyll.     

Water Deficit Enhanced Cotton Resistance to Spider Mite Herbivory

We investigated the responses of cotton (Gossypium hirsutumL.)to the combined effects of soil water deficit and two-spottedspider mite (Tetranychus urticaeKoch) infestation. Two mitetreatments (-M: uninfested, +M: artificially infested 83 d aftersowing), and two water regimes (+W: well watered, -W: waterstressed) were combined factorially in four treatments. Mitecolonies developed at similar rates in well-watered and water-stressedcrops. Despite the similar intensity of infestation, visualsymptoms of mite injury were more marked in well-watered hostplants (+M+W) than in their water-stressed counterparts (+M-W).Lint yield of unstressed controls (-M+W) was 175 g m^-2. In uninfestedcrops, water deficit reduced yield by 30%, mites reduced theyield of well-watered crops by 92%, and the combination of miteinfestation and water deficit reduced yield by 72% (water effect:P<0.01;mite and interaction effect:P<0.0001). Differences in yieldresponses to mites between well-watered and water-stressed cropswere mostly related to differences in reproductive partitioning.The interaction between mites and water deficit was also significantfor other crop variables including canopy temperature, leafwater potential, concentration of nitrogen in reproductive structuresand seed oil concentration. The magnitude and consistency ofthe interaction between both stresses indicates that, underour experimental conditions, mechanisms of adjustment to waterdeficit may have enhanced cotton resistance to mites. This isfurther supported by (a) an increase in specific leaf weightand a parallel increase in leaf penetration resistance due towater deficit; (b) a negative association between macroscopicsymptoms of mite injury and leaf penetration resistance; and(c) a choice test showing that adult female mites preferredto feed and oviposit on leaves from well-watered plants.Copyright1998 Annals of Botany Company Gossypium hirsutumL.;Tetranychus urticaeKoch; leaf water potential; leaf penetration resistance; canopy temperature; multiple stresses; specific leaf weight; radiation use efficiency; nitrogen concentration; reproductive allocation.     

Stomatal responses to changing irradiance in Phaseolus vulgaris L.

The effects of air temperature (T_o), leaf-air vapour pressuredifferences [VPD) and water deficit on stomatal responses tochanging irradiance were studied in Phaseolus vulgaris L. Responseswere approximately sigmoidal, with rates of closure being fasterthan the rates of opening. The mean half-time for closure was5.4 min and for the opening 9.2 min. Under water deficit, bothstomatal opening and closing were faster than in well-wateredconditions. Stomata were more sensitive to VPD and water stressthan to T_o. The higher the VPD or T_o the more rapid was thestomatal response, except in stressed plants where there wasno significant effect of T_o. Under water stress, stomata weremore sensitive to water potential (     

Photosynthesis and Transpiration in Rice as Influenced by Soil Moisture and Air Humidity

The paper describes the effect of soil moisture content andair humidity on CO₂ exchange (P_N), CO₂ diffusion resistance(Cr) and transpiration (E) in four varieties of japonica rice(Oryza sativa L.). A decrease in soil moisture content reducedthe rate of photosynthesis to a varying degree in the varieties.Reduction in photosynthesis was attributed to increase in Cr.The effect of low soil moisture on photosynthesis and CO₂ diffusionwas further intensified by decrease in air humidity. By maintaininga high humidity in the air around the leaves however, the effectof soil moisture deficiency was reduced considerably, exceptin Rikuto Norin 21 which was very sensitive to soil-moisturedeficiency alone. Dryness of the air enhanced the transpirationrate, although the increase was relatively less in the plantsfacing a simultaneous water crisis at the root surface. In plantsgrowing under flooded conditions, a decrease in air humiditycaused a slight depression in P_N despite the simultaneous decreasein Cr. Oryza sativa L., rice, photosynthesis, transpiration, diffusion resistance, soil moisture, air humidity     

Plasticity in hydraulic architecture of Scots pine across Eurasia

Widespread tree species must show physiological and structural plasticity to deal with contrasting water balance conditions. To investigate these plasticity mechanisms, a meta-analysis of Pinus sylvestris L. sap flow and its response to environmental variables was conducted using datasets from across its whole geographical range. For each site, a Jarvis-type, multiplicative model was used to fit the relationship between sap flow and photosynthetically active radiation, vapour pressure deficit (D) and soil moisture deficit (SMD); and a logarithmic function was used to characterize the response of stomatal conductance (G _s) to D. The fitted parameters of those models were regressed against climatic variables to study the acclimation of Scots pine to dry/warm conditions. The absolute value of sap flow and its sensitivity to D and SMD increased with the average summer evaporative demand. However, relative sensitivity of G _s to D (m/G _s,ref, where m is the slope and G _s,ref is reference G _s at D = 1 kPa) did not increase with evaporative demand across populations, and transpiration per unit leaf area at a given D increased accordingly in drier/warmer climates. This physiological plasticity was linked to the previously reported climate- and size-related structural acclimation of leaf to sapwood area ratios. G _s,ref, and its absolute sensitivity to D (m), tended to decrease with age/height of the trees as previously reported for other pine species. It is unclear why Scots pines have higher transpiration rates at drier/warmer sites, at the expense of lower water-use efficiency. In any case, our results suggest that these structural adjustments may not be enough to prevent lower xylem tensions at the driest sites.     

A Finite-element Model of Radial and Axial Conductivities for Individual Roots: Development and Validation for Two Desert Succulents

A morphologically explicit numerical model for analysing wateruptake by individual roots was developed based on a conductornetwork, with specific conductors representing axial or radialconductivities for discrete root segments. Hydraulic conductivity(L_p; m s^–1 MPa^–1) was measured for roots of Agavedeserti Engelm. and Opuntia ficus-indica (L.) Miller by applyinga partial vacuum to the proximal ends of excised roots in solution.L_p was also measured for 40- to 80-mm segments along a root,followed by measurements of axial conductivity and calculationof radial conductivity. Predicted values of L_p for entire rootsbased on two to ten segments per root averaged 1.04±0.07(mean±s.e. mean for n = 3) of the measured L_p for A.deserti and 1.06±0.10 for O. ficus-indica. The modelalso closely predicted the drop in water potential along theroot xylem (^xylem); when a tension of 50 kPa was applied tothe proximal ends of 0.2 m-long roots of A. deserti and O. ficus-indica,the measured ^xylem to midroot averaged 30 kPa compared witha predicted decrease of 36 kPa. Such steep gradients in ^xylemsuggest that the driving force for water movement from the soilto young distal roots may be relatively small. The model, whichagreed with an analytical solution for a simple hypotheticalsituation, can quantify situations without analytical solutions,such as when root and soil properties vary arbitrarily alonga root. Agave deserti, electrical circuit analog, hydraulic conductivity, Opuntia ficus-indica, water potential     

A Two-dimensional Model for Water Uptake by Desert Succulents: Implications of Root Distribution

Water uptake by Agave deserti and Ferocatus acanthodes was predictedusing a two-dimensional simulation model in which the soil arounda plant was divided into a series of layers and concentric cylindricalshells. Root lengths in 0.05 m thick soil layers were determinedfor both species in the field, where mean root depths were only0.11 m for A. deserti and 0.10 m for F. acanthodes. For a yearwith average precipitation (159 mm), 42 per cent of the annualprecipitation could be taken up by A. deserti and 25 per centby F. acanthodes. Predicted water uptake by both species wasgreater from the upper soil layers (above 0.15 m) for averageand dry years, but was greater from the deeper layers for awet year. The actual root distribution for both species ledto more water uptake than when all of the roots were in a singlelayer. The large number of days per year when the soil temperaturesexceeded 57 °C (the temperature for 50 per cent inhibitionof uptake of a vital stain by root cells) may exclude rootsfrom the 0.00–0.05 m soil layer, even though water uptakewhen all roots were located there was predicted to be maximal.Therefore, the observed root distribution of A. deserti andF. acanthodes may be limited near the soil surface by high temperaturesand at maximum depths by water availability for all but wetyears. Agave deserti, Ferocactus acanthodes, desert succulents, root system, root distribution, soil temperature, water uptake     

The Effects of Soil Water and Atmospheric Vapour Pressure Deficit on Stomatal Behaviour and Photosynthesis in the Oil Palm

The oil palm (Elaeis guineensis Jacq.) maintains a large leafarea throughout the year, but its productivity is limited bya low rate of dry matter production per unit leaf area. Stomatalclosure, at times of low soil water availability and high atmosphericvapour pressure deficit, is an important factor limiting photosynthesisand hence dry matter production. In this paper, laboratory andfield data are used to prepare a model of the relationshipsbetween net photosynthetic rate and stomatal conductance, andbetween stomatal conductance and environmental variables. Resultsshow that high atmospheric vapour pressure deficits may limitproduction even in parts of the world where oil palms are notnormally considered to suffer from water stress. The model canbe used to design and evaluate irrigation systems, and to helpquantify the potential value of oil palm genotypes with lowstomatal sensitivity to either VPD or available soil water foruse where irrigation is impractical. Key words: Elaeis guineensis Jacq., drought, irrigation, plant breeding