Cowpea (Vigna unguiculata L.) is an important legume, especially in the hot, dry tropics and subtropics of sub-Saharan Africa. It has been widely reported to be drought tolerant. Cowpea is a highly nutritious, multi-purpose crop, used as a leafy vegetable and grain legume with potential to contribute to food security in marginal areas. However, the crop is still classified as a neglected underutilised species; legume research focus has been mainly devoted to established legumes such as common bean and soybeans. There is a need to collect empirical information on cowpea which could be used to advise farmers on management strategies. This study evaluated cowpea responses to water stress under controlled and field conditions. Initially, two cowpea varieties (Brown and White birch) were evaluated for seed quality using the standard germination that was laid out in a completely randomised design and each variety was replicated for times. Electrolyte conductivity test was also performed under laboratory conditions. Thereafter, a pot trial was conducted to evaluate cowpea response to water stress imposed at different growth stages under varying growth temperatures. The pot trial comprised three factors: temperature [High (33/27ºC), Optimum (27/21ºC) and Low (21/15ºC)], water regimes (no stress, terminal stress, intermittent stress – vegetative and intermittent stress - flowering) and cowpea varieties. Lastly, a field trial was conducted to evaluate cowpea production as well as the effect of sequential leaf harvesting on yield under irrigated and rainfed conditions. The field trial was laid out as a split-plot design, with water regime (irrigation vs. rainfed) as main factors, cowpea varieties as sub-factor and sequential harvesting (no harvest, harvested once and harvested twice), replicated three times. All treatments were arranged in a randomised complete block design. Results of the initial study showed that germination capacity and vigour of cowpea varieties were significantly different (P < 0.001). White birch had higher electrolyte leakage than Brown birch. Pot trial results showed that cowpea growth (leaf area, leaf number and plant height) was vigorous in the high temperature regime compared with optimum and low temperature regimes. Chlorophyll content index was higher under high temperature relative to optimum and low temperature regimes, respectively. Under low and optimum temperature regimes, cowpea growth was stunted; cowpea failed to flower and form yield. Whereas, under high temperature regime, cowpea growth was vigorous hence flowered and formed yield. Vegetative growth was more sensitive to water stress than flowering stage. Terminal stress and stress imposed during flowering resulted in increased proline accumulation relative to no stress and stress imposed during vegetative growth. Harvest index was lower when water stress was imposed during vegetative relative to flowering stage. Field trial results showed that cowpea growth was sensitive to water stress. Plant height, leaf number, chlorophyll content index and stomatal conductance were lower under rainfed relative to irrigated conditions. Sequential harvesting of leaves had no significant effect on cowpea yield. It is concluded that tropical temperature conditions are most suitable for cowpea production; the controlled environment study showed best crop performance under 33/27ºC. In the context of varieties used for the present study, vegetative growth was the most sensitive stage to water stress. Cowpea performed better under rainfed relative to irrigated conditions with respect to yield formation. Low temperature was found to be more limiting to cowpea growth, development and productivity compared with water stress. Whereas, under high temperature conditions, water stress was more limiting to plant growth and productivity. White birch may be used as a dual purpose crop due to its ability to produce reasonable grain yield regardless of defoliation. / Thesis (M.Sc.Agric)-University of KwaZulu-Natal, Pietermaritzburg, 2012.

This paper describes the processes, methods, backgrounds, and economic challenges, of Desalination and Water Recycling and provide current examples of both. To create a baseline with which to compare the two methods, I will also delve into the history of California water policy. This complicated past is the reason water importation into Southern California remains the main method of obtaining water. Yet, as the current drought continues and technology advances, the need for imported water will become obsolete as the methods for recycling and desalinating water become less expensive, more convenient and more equitable. In the conclusion, all the methods will be compared and I will give suggestions on potential solutions for solving San Diego’s water dependence.

The characterization of natural climate variability is important in order to understand the climate response to natural forcings and to identify anthropogenic influences. The aim of this thesis is to reconstruct climate changes in the southwest of France, a region which is characterised by recurrent drought periods, where high resolution proxy records of the last millennia were lacking.The reconstruction is based on multiple proxies from two continental archives: speleothems and tree rings. Their combination can make use of the strengths of each archive while compensating their weaknesses. There are two principal objectives: first, to gain a better understanding of the climatic and non-climatic influences on each proxy; and second, to reconstruct drought periods in the past.The oxygen isotopic composition (δ18O) of speleothem fluid inclusions and tree ring cellulose is controlled to a large extent by the δ18O of precipitation, which can serve as a tracer of the atmospheric circulation. In order to interpret these proxies in terms of climate, it is necessary to understand how the climate signal becomes recorded in the proxy, and which processes modify the original signal during the formation of the archive.Measurements of δ18O in precipitation, cave drip water, and fluid inclusions in modern speleothem samples from Villars Cave demonstrated that the isotopic composition of cave drip water corresponds to the pluri-annual average precipitation. The speleothem fluid inclusions, in turn, preserve the isotopic composition of the drip water. Based on this calibration, it is possible to reconstruct drip water isotope variability using fluid inclusions in a more than 2000 year old stalagmite, which has been dated by laminae counting, as well as U-Th and 14C measurements. Changes in the cave environment, e.g. the vegetation cover, are indicated by other proxies from the same stalagmite (stable isotopes in calcite and trace element concentrations), but these changes do not seem to impact the fluid inclusion δ18O significantly.The isotopic composition of tree ring cellulose from Quercus spp. in the study area is strongly influenced by climate conditions during the summer. However, non-climatic influences on the isotopic composition of cellulose are identified. They are linked to the age of the trees and to site hydrology, and must be accounted for in the sampling and analytical procedures. Crossdated cores from living trees and timber wood in historic buildings near Angoulême are used to build an annually resolved chronology of cellulose δ18O. Significant correlations with meteorological data enable a calibration and a reconstruction of drought periods since 1360 AD.Lastly, this thesis explores a novel approach of integrating oxygen isotope records from speleothem fluid inclusions and tree ring cellulose from closely located sites to reconstruct both high- and low-frequency variability of droughts in the past.

This study examines rural household food security and its determinants in drought-prone Amhara Region of Ethiopia by focusing on Lay Gaint district as a case study site. A range of factors from physical environmental circumstances to policy and institutions-related issues determine households‟ vulnerability to food insecurity and livelihood outcomes. The survey results showed that the majority (74%) of the sampled households experienced food insecurity. The situation was worse among female-headed households such that 86% of them were food insecure. The study revealed that, despite the low level of productivity related to local environmental constraints, rural livelihoods remain undiversified with small scale rain-fed agriculture to provide the primary source of livelihood for the large majority of households (~93% of respondents). Only about 25% of the respondents participated in some form of non-farm or off-farm activities, but with only little contribution to their total annual incomes. Food insecurity is a chronic problem in that, on average, households in the study area consume from own production for only about six months. The study found out that the majority of households (about 80%) perceived annual rainfall to be inadequate to support the growing of crops and grazing of animals. The main adaptive strategies employed by the majority of households included diversifying livestock kept, planting trees and diversifying crops. The study revealed that incidence, depth and severity of food insecurity of the food insecure households showed that Woina-Dega and Kolla agro-ecologies are prone to vulnerability to food insecurity. This suggests that development interventions that are geographically differentiated; and build household assets will improve household food security in the study area, and in other similar environments in the country. / Geography

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No description available.

L’agriculture est à l’interface de plusieurs éléments du milieu naturel (eau, sol, climat,…) mais aussi de la société (économie, politique, démographie,…). Si durant des siècles elle a surtout été soumise au milieu naturel et à ses fluctuations (notamment climatiques), l’évolution des sociétés et surtout des techniques l’en ont en partie détachée, rendant les éléments sociaux et économiques premiers. Cette évolution est nette depuis le lendemain de la seconde guerre mondiale. Cependant, à l’heure où l’on parle de changement climatique, de réchauffement global, le climat et l’agriculture sont-ils déconnectés l’un de l’autre ? L’originalité de notre étude tient à sa localisation, un bassin versant déficitaire, au type d’agriculture présente (polyculture et forte part des cultures irriguées) et à la démarche scientifique qui l’accompagne. Celle-ci fait appel à différentes techniques : enquêtes, entretiens, analyses de données climatologiques, hydrologiques) qui seront étudiées à travers leur mise en relation à travers l'approche systémique. L'approche systémique nous permet de mettre en évidence les rapports existant entre les différents éléments concernés mais aussi de nous situer dans le temps. Notre étude prend en compte la place de la sécheresse dans l'évolution des pratiques agricoles ; l'inscription des modifications des pratiques agricoles peuvent inscrire des modifications dans le milieu support de leurs activités ; la modification de la relation à la ressource en fonction de l'adaptation des pratiques agricoles , et l'inscription des relations de pouvoir dans l'espace et le temps. / Farming is at the interface between several elements of the natural environment (water, soil and climate) and of society as well (economy, politics, demography, etc.). If, for centuries, it has been particularly subjected to the natural environment and its variations (mainly climatic), the evolution of societies and especially techniques have partly turned farming away from it, putting social and economic elements first. This evolution has been clear since the afterwards the Second World War. However, as climate change and global warming are being debated, are climate and farming disconnected from one another? The originality of this study is its location, a watershed deficit, its type of farming system (polyculture and the high proportion of irrigated crops) and the scientific process going with it. It uses different techniques such as surveys, interviews, analysis of climatic and hydrologic change), which will be studied through their links by a systems approach. Not only does this approach enable us to highlight the relationship between the elements involved but it also enables us to locate in time through a study of past episodes in order to outline a prospective study. Our study will therefore have to answer the following questions: what is the role of drought in the evolution of agricultural practices? How changes in agricultural practices may include changes in the leading place of their activities? How the relationship to water can be modified by the adaptation of agricultural practices? And how can it fit in the power relations and be located in space and time?

Thesis subject is the evaluation of runoff and flood regime of rivers Lužnice and Skřemelice at the closing profiles just before their confluences. The results are compared with findings from the profile Pilař, which were published in the past by other authors. More attention is paid to the evaluation of the hydrological year 2013 and in detail is described the flood in June of the same year. Daily flow data from the years 1971 - 2014 were used for evaluating of runoff conditions. The assessment of the runoff regime in terms of daily, monthly and annual flows were compared with the runoff regime in Pilař gauge station. The source regions with dominating influence on the resulting runoff were discovered. Analysis of the flood regime confirmed that spring floods in Lužnice came mainly from upland and hilly parts of catchment and large summer floods have main source area in the catchment of Lužnice river itself, before the confluence of the Lužnice river and Skřemelic river. When assessing flood in 2013, the main source areas of flood flows that hit Lužnice river basin were founded. The flood extremity was compared in each closing profiles.

Face aux changements climatiques actuels et à l'augmentation des populations, la vulnérabilité du sol et des services écosystémiques qu’il rend s’accroît. En particulier dans les zones climatiques méditerranéennes, les modèles météorologiques prévoient une augmentation des sécheresses estivales et une augmentation des températures accompagnées par l’apparition plus fréquente d’évènements extrêmes de type canicule et sécheresse. Ces événements, leur intensité, leur durée et la soudaineté avec laquelle ils arrivent, sont de nature à affecter la structure et la fonction des écosystèmes avec des conséquences principalement négatives sur leur biodiversité et leurs fonctions et services. Par ailleurs, l’apport de compost au sol pourrait constituer une solution pour prévenir et atténuer les effets des sécheresses et des canicules dans les agrosystèmes méditerranéens. Les objectifs de ce travail étaient de caractériser les effets à court et à long-terme de perturbations de type canicule et/ou sécheresse appliquées à un sol méditerranéen agricole (structures et fonctions des communautés microbiennes édaphiques) et d’étudier les impacts d’épandage préalable de composts sur la réponse à court et à long-terme de ces communautés microbiennes (structures et fonctions) vis-à-vis d’un événement extrême de canicule-sécheresse. Nos travaux nous ont permis d’évaluer l’influence de chacun des facteurs température élevée et sécheresse dans la perturbation canicule et sécheresse associées sur les paramètres microbiologiques et physico-chimiques du sol. Les effets de cette combinaison des deux perturbations a induit des réponses similaires à l’une ou l’autre des perturbations appliquées individuellement en bénéficiant des effets positifs et négatifs sur la communauté microbienne de chaque type de perturbation. Nous avons mis en évidence une durée seuil de la perturbation canicule-sécheresse sur la résistance de la communauté microbienne induisant un changement de structure taxonomique et fonctionnelle. Cette déstructuration de la communauté microbienne est durable et n’a pas permis de résilience. L’ajout préalable de composts de différents types au champ a amélioré la structure physico-chimique et stimulé les microorganismes indigènes du sol. Cependant, face à des perturbations de type canicule-sécheresse (telles que nous les avons testées), il semble que l’apport préalable de compost n’ait pas d’effets majeurs sur l’amélioration de la qualité du sol en terme de stabilité microbienne, mais que l’historique saisonnier influencerait cette stabilité / Current climate change and increasing populations’ growth enhance soil and ecosystem services vulnerability. Meteorological models predicted an increase in summer drought and higher air temperature with more frequent occurrence of extreme events like heat-waves and drought. Intensity and duration of these events may affect structure and functions of ecosystems and thereby the biodiversity and the functions of soil. The amendment of soils with composts could be an alternative to prevent and mitigate the effects of drought and heat waves in the Mediterranean agroecosystems. The objectives of this work were to characterize the effects of short and long-term high temperature and/or drought perturbation on soil Mediterranean microbial communities (structures and functions) and to study the impacts of compost amendment on short and long-term functional and taxonomic responses of microbial communities subjected to drought and high temperature. Our work allowed us to evaluate the influence of each factor (drought or high temperature) within the combined perturbation (drought and high temperature) on microbiological and physico-chemical soil properties. The effects of this combined perturbation induced similar or different responses of each of perturbations applied individually involving positive and negative effects on the microbial community. This work had shown threshold resistance duration inducing a change in taxonomic and functional microbial community structure after high temperature and drought perturbation. This abrupt shift in the community response did not allow resilience. Compost amendments improved the physico-chemical soil structure and stimulated indigenous soil microorganisms. However, it seemed that seasonal soil variations history rather than compost amendment influences soil microbial stability

Les membranes cellulaires sont des cibles préférentielles de la dégradation induite par les espèces réactives de l’oxygène produites durant la sécheresse et par la stimulation d’activités hydrolytiques. La biosynthèse des lipides des chloroplastes peut être importante pour la tolérance à la sécheresse ainsi que pour la reprise après réhydratation. Dans ce travail nous avons étudié le métabolisme des lipides des membranes chloroplastiques, monogalactosyldiacylglycerol (MGDG), digalactosyl-diacylglycerol (DGDG), sulfoquinovosyldiacylglycerol (SQDG), phosphatidyl-glycerol (PG), dans le cadre de la sécheresse et de la reprise après la fin de la contrainte hydrique. Dans ce but, nous avons mesuré la teneur des lipides des feuilles, suivi l’incorporation du précurseur 14C-acétate dans les lipides et analysé l’expression des gènes codant les enzymes de biosynthèse des lipides (MGD1, MGD2, DGD1, DGD2, SQD2 et PGP1) durant le stress hydrique et après réhydratation. Afin de mieux comprendre le rapport entre le métabolisme de ces lipides et la tolérance à la sécheresse, nous avons travaillé sur deux cultivars de Vigna unguiculata L. Walp, un tolérant (cv. EPACE) et l’autre sensible (cv. 1183) à la sécheresse. Les séquences complètes des ADNc des gènes VuMGD1, VuMGD2, VuDGD1, VuDGD2, VuSQD2 et VuPGP1 ont été obtenues par le criblage d’une banque d’ADNc de V.unguiculata. Les résultats montrent qu’en condition de stress hydrique le cultivar tolérant, en plus de préserver la teneur en lipides, est capable de stimuler la biosynthèse du DGDG augmentant significativement le rapport DGDG:MGDG de ces membranes. Nous suggérons que le DGDG accumulé en sécheresse est exporté vers les membranes extrachloroplastiques et que cela contribue à la tolérance à la contrainte hydrique. Les effets de la perte d’eau cellulaire sur les membranes ont des conséquences directes sur la capacité des plantes à reprendre après réhydratation. 48 heures après réarrosage, le cv. sensible 1183 n’est pas capable de récupérer en termes de teneurs en galactolipides et incorporation de précurseur. Chez le cv. tolérant, par contre, la teneur en DGDG demeure élevé, même après réhydratation. En conclusion, nos résultats suggèrent l’importance des lipides membranaires dans la tolérance/sensibilité des plantes au déficit hydrique, en particulier la balance entre des classes lipidiques de propriétés physico-chimiques différentes (SQDG versus PG et DGDG versus MGDG) qui pourraient affecter la structure et le fonctionnement des membranes / Membranes are main targets of degradation by reactive oxygen species and hydrolytic activities induced by drought. Chloroplasts lipid biosynthesis, especially galactolipids monogalactosyl-diacylglycerol (MGDG) and digalactosyl-diacylglycerol (DGDG) are important for plant tolerance to water deficit and for recovery after rehydration. In this thesis, we studied the metabolism of the chloroplast membrane lipids, MGDG, DGDG, sulphoquinovosyl-diacylglycerol (SQDG), phosphatidyl-glycerol (PG) under drought and during recovery from drought. Aiming this, we measured leaf lipids content, followed 14Cacétate incorporation and expression of genes coding for chloroplast membrane lipid synthases (MGD1, MGD2, DGD1, DGD2, SQD2 and PGP1) during drought and recovery. In order to better understand the relationship between drought tolerance and lipid metabolism, two cultivars of Vigna unguiculata L. Walp, one drought tolerant (cv. EPACE) the other drought susceptible (cv. 1183) were compared. The cDNA complete sequences for VuMGD1, VuMGD2, VuDGD1, VuDGD2, VuSQD2 and VuPGP1 were obtained from screening of a V.unguiculata cDNA library. The results showed that under water stress conditions, the tolerant cultivar, besides its ability to preserve its lipids pool despites drought, is able to strongly stimulate the DGDG biosynthesis, increasing the DGDG:MGDG ratio in its membranes. We suggest that DGDG accumulated under drought condition, when phosphate is deficient, is exported for extrachloroplastic membranes, and thus contributes to plant drought tolerance. Effects of loss of water on cell membranes have direct consequences on plant capacity to recover from stress. 48 hours after rewatering, the susceptible cv. 1183 was not able to fully recover from a moderate stress in terms of leaf galactolipid content and acetate incorporation into MGDG. In EPACE-1, MGDG leaf content remained unchanged after rehydration and DGDG remained higher than in the control plants. In conclusion, our results highlight the importance of membrane lipids in plant adaptation to water deficit and in their capacity to recover from stress. Of particular importance is the balance between lipid classes with various physico-chemical properties (SQDG versus PG, DGDG versus MGDG), since they most likely have a profound influence on membrane structure and function