The impact of long term management strategies of irrigation with saline water in semi-arid region of Gordonia, South Africa is the highest interest to optimize water consumption, soil conservation, and crop yield for sustainable water allocations to human food production and ecosystem without irreversible damages to soil and water body. An integrated ecosystem assimilation, in shape of soil-water storage model based on physical approach for 30-year simulation run defined in form of digital ecosystem modelling with help of CoupModel tool to assemble together the most important underlying processes of soil hydraulics, irrigation demands, leaching fraction, evapotranspiration, salt transport. Two scenarios of water management strategy; surface as traditional and drip as subsurface irrigation considered to apply water and salt into the ecosystem model. Gaining high food production for human with respect to ecosystem sustainability, in each water management scenario studied by evaluating general and detailed result from water and salt balance for the entire simulation period plus long term nitrogen and carbon turnover as crop yield indicator. Non-productive water losses, salt accumulation in root zone, carbon and nitrogen turnover, salt transport to aquifer via deep percolation observed thoroughly. Decline in crop yield due to water and salt stress, conducted by monitoring biomass production with respect to water consumption and soil osmotic pressure in root zone. Drip scenario had better functionality to perform less water wastage by decreasing soil evaporation as non-productive water loss almost 40 %, however productive water consumption decreased 20 % due to insufficient leaching fraction and also salt accumulation increased in root zone. Precipitation had a significant role to accomplish leaching deficiency and removing salt from root zone. Salt accumulation flushed out from root zone by more leaching, though resulting more water wastage and more possibility of salinization threatening beneath aquifer. Ecosystem in terms of soil-water and plant responding differently facing salinity in different water management practices and salt as source of pollution could either stabilized in soil by accumulating in root zone causing anthropogenic soil desertification or percolate to beneath aquifer resulting aquifer salinization.

Plant responses to different soil moisture regimes have been extensively studied. Because of interactions between the soil, plant and climatic factors, few convincing generalizations concerning the influence of soil water on the transpiration of water by plants have been established. Generally single factors or at most the interaction of two have been studied at any one time. Useful theories describing the conditions of water retention in plant tissues and movement of water through plants have been proposed. Equally useful theories have been suggested for describing the retention and transmission of water in soil. The integration of these theories and their applications to evapotranspiration remains to be elucidated. This indicates a need for studying the total free energy path that causes water transport from soil to atmosphere through plants. Two interrelated categories of processes or factors, atmospheric desiccation and rate of soil water uptake, need to be studied simultaneously. The energy status of plant water, herein called total plant water potential, in conjugation with soil water potential appears to be critically involved in the process of water transfer through the soil-plant-atmosphere system. Plant water potential is the best criterion for detecting the degree of plant water stress. By studying water retention and flow properties of both plants and the supporting soil, one may be able to find relations that will help to predict the behavior of plants as they remove water from soil. For example, water retention characteristics of drought resistant plants may suggest reasons why some desert plants survive desiccating conditions that cause death to more succulent plant species. The major objective of this study was to investigate the influence of soil water potential and atmospheric environment on both the transpiration rates and components of the plant water potential.

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第19686号 / 工博第4141号 / 新制||工||1639(附属図書館) / 32722 / 京都大学大学院工学研究科航空宇宙工学専攻 / (主査)教授 稲室 隆二, 教授 青木 一生講師杉元 宏 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM

Trunk height, diameter, and stomatal conductance measurements were taken over a three-year time frame on clonal red maple cultivars [Acer rubrum ‘Frank Jr’] on two sites with varying conditions. Physiological and morphological effects on tree growth were measured on both sites in response to Pneumatic Fracturing (PF) and Liquid Injection (LI) treatments. The primary questions asked in study one were: (1) Does stomatal conductance differ among the two sites during mid-summer? and (2) Do height and diameter measures differ among the two sites? In study two, I asked: (1) Do height, diameter and stomatal conductance differ between site modification treatments within each site? Control samples on the Site 2 had significantly more growth than the controls on the Site 1. PF and LI treatments showed significantly more diameter growth on the Site 1 while a significant difference was also seen in stomatal conductance following treatments on Site 1.

The cuticle is constituted of the biopolymer cutin and intra- and epicuticular waxes. In some cases, it has epicuticular wax crystals, protruding from the epicuticular wax film. One of the most important tasks is protection against desiccation. Many investigations were conducted to find the transport limiting component of the cuticle. It is evidentially confirmed that the waxes form this barrier. These waxes are multifactorial blends made of very-long-chain aliphatic (VLCA) compounds and triterpenoids (TRP). The VLCAs were proposed to constitute the transpiration barrier to water. However, experimental confirmation was lacking so far. The present study focuses on the development of a method to selectively extract TRPs from the cuticle and the impact of the removal on the transpiration barrier. The plants deployed in this study exhibited several features. They had no epicuticular crystals on their surfaces, were astomatous, had a rather durable and possibly isolatable cuticle. A broad range of wax compositions was covered from plants with no TRP content and low wax load like Hedera helix and Zamioculcas zamiifolia to plants with high TRP content and high wax load like Nerium oleander. The selective extraction was conducted using a sequence of solvents. TRPs were extracted almost exhaustively from CMs with the first MeOH extract. Only a minor amount of shorter chained VLCAs was obtained. The remaining waxes, consisting mostly of VLCAs and some remnant TRPs, were removed with the following TCM extract. After the extractions, the water permeance of native cuticular membranes (CM), MeOH extracted (M) and dewaxed cuticular discs (MX) was investigated gravimetrically. Compared to the water permeance of CMs, Ms showed no or only a small increase in water conductance. MXs, however, always showed strongly increased values. The knowledge about the wax compounds constituting the transport-limiting properties is vital for different projects. For various issues, it would be favourable to have a standardized wax mixture as an initial point of research. It could be used to develop screening procedures to investigate the impact of adjuvants on cuticular waxes or the influence of wax constituents on the properties of cuticular waxes. This work concentrated on the development of an artificial wax mixture, which mimics the physical properties of a plant leaf wax sufficiently. As target wax, the leaf wax of Schefflera elegantissima was chosen. The wax of this plant species consisted almost exclusively of VLCAs, had a rather simple composition regarding compound classes and chain length distribution and CMs could be isolated. Artificial binary, ternary and quaternary waxes corresponding to the conditions within the plant wax were investigated using differential scanning calorimetry (DSC), X-ray diffraction (XRD) techniques and Fourier-transform infrared (FTIR) spectroscopy. Phase diagrams were mapped out for a series of binary, ternary and quaternary wax mixtures. FTIR experiments were conducted using, ternary and a quaternary artificial wax blends. The blends were chosen to represent the conditions within the wax of the adaxial CM plant wax. The FTIR experiments exhibited an increasing resemblance of the artificial wax to the plant wax (adaxial CM wax) with an increasing number of compounds in the artificial wax. The same trend was found for DSC thermograms. Thermograms of ternary and quaternary blends exhibited more overlapping peaks and occurred in a temperature range more similar to the range of the whole leaf plant wax. The XRD spectrum at room temperature showed good conformity with the quaternary blend. The current work illustrates a method for selective extraction of TRPs from isolated CMs. It gives direct experimental proof of the association of the water permeance barrier with the VLCA rather than to the TRPs. Furthermore, the possibility to mimic cuticular waxes using commercially available wax compounds is investigated. The results show promising feasibility for its viability, enabling it to perform as a standardized initial point for further research (e.g. to examine the influence of different constituents on waxes), revealing valuable knowledge about the structure and the chemistry-function relationship of cuticular waxes. / Die Kutikula ist eine der vielen Anpassungen, die Pflanzen entwickelten um nach der Besiedelung des Landes mit den Herausforderungen ihrer neuen Umgebung fertig zu werden. Sie überzieht überirdische Pflanzenorgane, wie Blüten oder Blätter und erfüllt verschiedene Aufgaben. Hierzu besteht sie aus dem biopolymer Kutin und intra- sowie epikutikulären Wachs. Studien, die sich mit der Lokalisierung der transporteinschänkenden Barriere beschäftigten, zeigten, dass die Wachse sie bilden. Diese sind vielschichtige Mischungen aus langkettigen aliphatischen Verbindungen (VLCA) und pentazyklischen Verbindung wie Triterpenen (TRP). Es wird davon ausgegangen, dass VLCAs die Barriere aufbauen, ein direkter experimenteller Nachweis dafür wurde jedoch noch nicht erbracht. In dieser Arbeit wurde daher ein Verfahren zur selektiven Extraktion von TRPs aus isolierten kutikulären Membranen (CM) entwickelt und deren Auswirkung auf die Transpirationsbarriere untersucht. Die untersuchten Pflanzen wiesen keine epikutikuläre Kristalle auf, hatten keine Stomata auf der Kutikula der Blattoberseite und es war möglich ihre Kutikula zu isolieren. Die Zusammensetzung der Wachse variierte von wenig Wachs ohne TRPs (z. B. Hedera helix, Zamioculcas zamiifolia) hin zu pflanzen mit großer Wachsmenge und hohem TRP- Anteil (Nerium oleander). Die selektive Extraktion wurde durch die sequenzielle Nutzung zweier Lösemittel erreicht. TRPs wurden fast vollständig mit Methanol (MeOH) entfernt, während VLCAs überwiegend nur mit Chloroform (TCM) extrahiert werden konnten. Die gravimetrische Bestimmung der Wassertranspiration von unbehandelten, mit Methanol extrahierten (M) und entwachsten Membranen (MX) in Transpirationskammern zeigte bei allen untersuchten Pflanzenarten einen einheitlichen Trend auf. Im Vergleich zu CMs erhöhte sich die Transpirationsrate bei Ms nicht oder nur geringfügig, während bei MXs ein starker Anstieg festgestellt werden konnte. Diese Ergebnisse stellen den ersten direkten experimentellen Nachweis der Verbindung von VLCAs zur Transpirationsbarriere kutikulärer Wachse dar. Mit dem Wissen, sich bei der Untersuchung der Permeation durch die Kutikula sich nur auf die VLCA Fraktion beschränken zu müssen können weitere Projekte effizient angegangen werden. Ein leicht erhältliches Standartwachsgemisch könnte Ausgangspunkt für die Untersuchung des Einflusses verschiedener Pflanzenwachskomponenten auf deren physikalische Eigenschaften dienen. Als Zielwachs diente das Blattwachs von Schefflera elegantissima. Es bestand fast ausschließlich aus VLCAs, hatte eine recht einfache Zusammensetzung bezüglich der Stoffklassen und Kettenlängenverteilung und die Kutikula war isolierbar. Mit Hilfe von dynamische Differentialkalorimetrie (DSC), Röntgenbeugung (XRD) und Fouriertransformierter Infrarot (FTIR) Spektroskopie wurden binäre, ternäre und quaternäre Gemische, die Verhältnisse im Pflanzenwachs wiederspiegelten, untersucht und Phasendiagramme erstellt. Phasendiagramme wurden von einer Reihe der binären Gemische, bestehend aus Alkanen oder Alkoholen, ternären Gemischen aus zwei Alkanen und einem Alkohol und quaternären Gemischen aus zwei Alkanen und zwei Alkoholen erstellt. FTIR-spektroskopische Versuche zeigten mit zunehmender Komponentenzahl eine erhöhte Ähnlichkeit der artifiziellen Wachse zum Pflanzenwachs (adaxiale isolierte Kutikula). Ein ähnlicher Trend wurde für die Ähnlichkeit der Thermogramme der artifiziellen Gemische zum Pflanzenwachs (aus dem Extrakt ganzer Blätter) ersichtlich. Das Diffraktogramm des quaternären Waches stimmte auf Raumtemperatur gut mit dem des Pflanzenwachses (adaxiale isolierte Kutikula) ein. Diese Arbeit beschreibt eine Methode zur selektiven Extraktion von TRPs aus isolierten kutikulären Membranen. Sie zeigt einen direkten experimentellen Nachweis für die Assoziation der Transpirationsbarriere zu den VLCAs und nicht zu den TRPs. Zusätzlich wird die Möglichkeit kutikulare Wachse mit Hilfe von kommerziell erhältlichen Wachskomponenten nachzustellen untersucht, was vielversprechende Ergebnisse liefert. Dieses Wachs könnte daher als standardisierter Ausgangspunkt für weitere Experimente (z. B. zur Untersuchung des Einflusses verschiedener Wachskomponenten auf dessen physikalische Eigenschaften) dienen. Dies könnte wertvolle Informationen über die Struktur und die Beziehung zwischen chemischer Zusammensetzung und der Funktion kutikulärer Wachse liefern.

No description available.

Mountain meadows in the western USA are experiencing increased rates of conifer encroachment due to climate change and land management practices. Past research has focused on conifer removal as a meadow restoration strategy, but there has been limited work on conifer transpiration in a pre-restoration state. Meadow restoration by conifer removal has the primary goal of recovering sufficient growing season soil moisture necessary for endemic, herbaceous meadow vegetation. Therefore, conifer water use represents an important hydrologic output toward evaluating the efficacy of this active management approach. This study quantified and evaluated transpiration of encroached conifers in a mountain meadow using sap flow prior to restoration by tree removal. We report results of lodgepole pine transpiration estimates for an approximate 1-year period and an evaluation of key environmental variables influencing water use during a dry growing season. The study was conducted at Rock Creek Meadow (RCM) in the southern Cascade Range near Chester, CA, USA. Sap flow data were collected in a sample of lodgepole pine and scaled on a per-plot basis to the larger meadow using tree survey data within a stratified random sampling design (simple scaling). These estimates were compared to a MODIS evapotranspiration (ET) estimate for the meadow. The 1-year period for transpiration estimates overlapped each of the 2019 and 2020 growing seasons partially. The response of lodgepole pine transpiration to solar radiation, air temperature, vapor pressure deficit, and volumetric soil water content was investigated by calibrating a modified Jarvis-Stewart (MJS) model to hourly sap flow data collected during the 2020 growing season, which experienced below average antecedent winter precipitation. The model was validated using spatially different sap flow data in the meadow from the 2021 growing season, also part of a dry year. Calibration and validation were completed using a MCMC approach via the DREAM(ZS) algorithm and a generalized likelihood (GL) function, enabling model parameter and total uncertainty assessment. We also used the model to inform transpiration scaling for the calibration period in select plots in the meadow, which allowed comparison with simple scaling transpiration estimates. Average total lodgepole pine transpiration at RCM was estimated between 220.57 ± 25.28 and 393.39 ± 45.65 mm for the entire campaign (mid-July 2019 to mid-August 2020) and between 100.22 ± 11.49 and 178.75 ± 20.74 mm for the 2020 partial growing season (April to mid-August). The magnitude and seasonal timing were similar to MODIS ET. The model showed good agreement between observed and predicted sap velocity for the 2020 partial growing season (RMSE = 1.25 cm h-1), with meteorological variables modulating early growing season sap flow and volumetric soil water content decline imposing transpiration decrease in the late growing season. The model validation performed similarly to calibration in terms of performance metrics and the influence of meteorological variables. The consistency of the declining volumetric soil water content effect during the late growing season between periods could not be evaluated due to an abridged validation period. Overall, the implementation GL-DREAM(ZS) showed promise for future use in MJS models. Lastly, the model derived transpiration estimates for the 2020 partial growing season showed some of the potential utility in using the MJS model to scale sap flow at the study locale. It also highlights some of the key limitations of this approach as it is executed in the present study.

No description available.

One goal of this research was to characterize shoot tissue-level responses in loblolly pine to soil moisture limitation in combination with fertilization as well as to more severe soil moisture limitation. We found that neither fertilization alone, nor fertilization in combination with soil moisture limitation resulted in changes to shoot tissue water relations parameters classically characterized in drought response studies. More severe water limitation was necessary to elicit responses, and those responses had not been fully described previously. The more severe water limitation resulted in increased capacitance beyond turgor loss, increased relative water content at turgor loss, a more negative turgor loss point, an increased bulk modulus of elasticity, more negative osmotic potential at 100% relative water content, and an increased apoplastic water fraction. As there were indications of reduced water use and moisture stress in the absence of shoot level responses under less severe drought, such parameters are insufficient alone to characterize moisture stress in fertilized and in less severely water limited loblolly trees. Additionally, we sought a morphological or physiological explanation for the reduced transpiration and increased water use efficiency reported for fertilized trees in the Virginia Piedmont. Our characterizations of the responses of root distribution and hydraulics to limited soil moisture here complement existing research, which demonstrated changes to root distribution and hydraulics in response to fertilization. The responses we discovered in fertilized trees that accompanied reduced transpiration and increased water use efficiency that differed from responses to reduced soil moisture alone were primarily large decreases to shallow root presence. We found this to be readily quantified using measures of root length density. Decreases to whole-tree hydraulic conductivity were also shown to occur with fertilization and were shown not to occur in shoot tissue, suggesting limitation via rhizosphere or root xylem conductance. Our results support the supposition that fertilization narrows hydraulic safety margins and potentially predisposes loblolly trees to moisture stress, particularly prolonged, severe water limitation following fertilization. Finally, we tested the validity of throughfall exclusion for simulating reduced rainfall using a greenhouse 'split-pot' study, which applied spatially fixed heterogeneous soil moisture to young, well-watered loblolly pines. The 'split-pot' experiments demonstrated that spatially fixed soil moisture heterogeneity does not confound drought effects; needle area specific transpiration was not decreased, nor was water use efficiency increased. This supports the validity of inferences taken from drought simulation experiments with loblolly pine where throughfall exclusion troughs reduce soil moisture content in a consistent, spatially heterogeneous manner. / Doctor of Philosophy / We investigated various effects of soil moisture limitation alone, and in combination with common fertilization practices in loblolly pine production. Responses at the shoot and needle level to different levels of soil moisture limitation produced new findings concerning how tissues respond to more severe water limitation. A 30% decrease in throughfall precipitation alone, or in combination with fertilization did not elicit drought related shoot tissue responses despite the presence of other indications of moisture stress and reduced water use. We also sought to explain why fertilized trees experiencing water limitation had environmental sensitivities that were different from unfertilized tree receiving ambient rainfall amounts or from trees only experiencing water limitation without fertilization. We found that changes to shallow root presence, especially root length density, accompanied the different patterns of environmental sensitivity and water use. Also, the water conducting ability of roots changed unevenly in soil with uneven moisture levels. The ability of roots to resist loss of conductivity to water did not change unevenly in the same way. We did another set of experiments to determine if using impervious troughs to catch rain is a valid approach to reducing soil moisture for the purpose of testing how loblolly responds to water limitation. These throughfall exclusion troughs create uneven soil moisture reduction, which can have effects on plant water use that are separate from water limitation alone. We found that in well-watered young trees, uneven soil moisture alone did not produce responses that could be confused with the effects of water limitation. This finding indirectly validates the use of throughfall exclusion troughs to simulate reduced rainfall.

Des modèles empiriques ont été développés pour prédire la transpiration de quatre peuplements de sapin baumier (Abies balsamea L.) de la forêt Montmorency, Québec, à partir de mesures heat pulse velocity (HPV) et de mesures dans une chambre ventilée. La réponse à la blessure due à l'installation de la sonde HPV dans l'arbre expliquait 16% de la variabilité des mesures HPV dans le peuplement testé. Un facteur de correction polynomial est proposé pour l'atténuation du signal HPV dans le sapin baumier. Les taux de transpiration des quatre peuplements étaient tous significativement différents. Les coefficients d'atténuation des effets hydrologiques de la coupe (Ca) ont été calculés et des relations ont été ajustées en fonction de propriétés des peuplements. Les Ca étaient hautement corrélés avec l'âge, la hauteur et en particulier avec la surface terrière. La fonction de Ca indique qu'une récupération hydrologique de 50% est atteinte 16 ans après la coupe. Les valeurs estimées de Ca basés sur la transpiration étaient similaires à celles obtenues à partir des mesures de fonte de la neige pour les peuplements de 2, 12 et 22 ans.