Submitted by Renata Lopes (renatasil82@gmail.com) on 2016-07-11T12:22:39Z No. of bitstreams: 1 gilvaniakerciadeoliveira.pdf: 3723488 bytes, checksum: b7f5da15fa56d19b7ab5b00c40f91aec (MD5) / Approved for entry into archive by Adriana Oliveira (adriana.oliveira@ufjf.edu.br) on 2016-07-13T16:35:45Z (GMT) No. of bitstreams: 1 gilvaniakerciadeoliveira.pdf: 3723488 bytes, checksum: b7f5da15fa56d19b7ab5b00c40f91aec (MD5) / Made available in DSpace on 2016-07-13T16:35:45Z (GMT). No. of bitstreams: 1 gilvaniakerciadeoliveira.pdf: 3723488 bytes, checksum: b7f5da15fa56d19b7ab5b00c40f91aec (MD5) Previous issue date: 2012-04-20 / CAPES - Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / A cromatografia de íons é a técnica analítica mais utilizada para realizar a determinação de íons em amostras ambientais. Mas, atualmente, a cromatografia líquida de alta eficiência com pareamento iônico (ion-pair HPLC) tem sido usada para fazer este tipo de análise devido a estabilidade e a eficiência da coluna de fase reversa (FR). ion-pair HPLC é uma técnica mais complexa que a cromatografia de fase reversa, uma vez que o equilíbrio entre o reagente de pareamento iônico (RPI) e a fase estacionário (FE) é lento, a separação é mais sensível às variações de temperatura e pH. Além disso, variações na concentração do RPI também afeta a separação do analito. No ion-pair HPLC, vários parâmetros devem ser otimizados tais como: composição e pH da fase móvel, tipo de RPI (modificação permanente ou dinâmca da FE) e concentração do RPI. O presente trabalho teve como objetivo desenvolver uma metodologia analítica para separação e quantificação dos ânions cloreto, nitrito, nitrato e sulfato em amostras de água superficial por ion-pair HPLC. O método de separação dos ânions foi otimizado utilizando uma coluna de FR octadecilsilano (C18) com detecção indireta na região do ultravioleta. Durante a execução deste trabalho a composição e o fluxo da fase móvel por eluição isocrática foram estudados, assim com o comprimento de onda de detecção. Foram testados quatros RPI diferentes para compor a fase móvel. A melhor condição de separação dos íons foi alcançada com a utilização do reagente brometo de cetiltrimetilamônio com modificação permanente da FE. Concluído o processo de separação dos ânions a metodologia foi aplicada na análise das amostras de água do Rio Paraibuna (Juiz de Fora, MG). O método apresentou boa exatidão e boa precisão. Os níveis de concentração encontrados nas amostras de água do Rio Paraibuna ficaram a baixo do limite permitido pela legislação brasileira para água utilizada para consumo humano, indicando baixos níveis de contaminação. / The ion chromatography (IC) is the most widely used analytical technique to perform ion analysis in environmental samples. Nowadays, the ionpair high performance liquid chromatography (ion-pair HPLC) has been used to perform this kind of analysis due to the stability and efficiency of reverse phase (RP) column. The ion-pair HLPC is more complex than the reverse phase chromatography, since the equilibrium between the ion-pairing reagent (IPR) and stationary phase (SP) is slow, the separation is more sensitive to variations in temperature and pH. A variation in the concentration of IPR also affects the separation of the analytes. In ion-pair HPLC, several parameters must be optimized such as: mobile phase (MP) composition, type IPR, the concentration of the IPR in MP and pH of the MP. The present work aims to develop an analytical methodology for the separation and quantification of anions (chloride, nitrite, nitrate and sulfate) in surface water samples from Paraibuna River by ion-pair HPLC. The method of analysis of anions was optimized using RP chromatography column octadecylsilane (C18) with indirect detection in the ultraviolet region (UV). During the execution of this work the composition and flow rate of the MP for isocratic elution were studied as well with the wavelength for detection. We tested four different ion-pairing reagents to from the mobile phase. The best condition for separation of ions was achieved with the use of reagent cetyltrimethylammonium bromide. Once completed, the process of separation of anions the methodology was applied in the analyses of water samples from Paraibuna River. The parameters used for evaluate the accuracy and precision of method presented satisfactory values. The concentration levels found for the anions in the samples were below the limit allowed by brazilian legislation for water used for human consume.

Groundwater chemistry is a function of recharge and the input chemistry of the rain, which gets transformed as it moves through the soil matrix. Apart from mineral transformations, anthropogenic activities are other external factors, which affect the groundwater chemistry. Stream – aquifer interactions alter the chemistry of groundwater in the regions nearer to the stream. A study is carried out to analyse the hydrogeochemical behavior under the influence of lithologic, precipitation and anthropogenic controls in the upper Cauvery basin. This is followed by the analysis of contributions made by the components of the hydrogeochemical cycle. A geochemical model is developed, which is used to study the spatiotemporal variations in groundwater chemistry of a silicatic rock group in a small experimental watershed. In order to study the effects of precipitation control on the groundwater chemistry the Upper Cauvery river basin (~ 10000 km2) is selected for the analysis, which stretches along three climatic zones – ‘semi-arid’ (500 – 800 mm/year rainfall), ‘sub-humid’ (1000 - 1200 mm/year) and ‘humid’ (1200 – 1500 mm/year) zones. The basin is mainly formed by granitic gneissic group of rocks with some traces of amphibolites and charnockites. Groundwater is observed to occur either in the saprolite or in the deeper hard rock zone based on the geomorphology even at the scale of a small watershed. Parts of this basin are under canal irrigation and are drained by Kabini and Cauvery Rivers. Groundwater – surface water interactions play an important role in these regions. Irrigation with different levels of intensities is practiced through groundwater in the upland areas. Observation wells considered in these three zones are classified into four classes based on the mean annual groundwater fluctuations. Wells in each of these four classes are further classified into ‘shallow’ and ‘deep’ categories based on the depth to groundwater. Analysis of the groundwater chemistry in the basin (widely spread with 120 wells in the three zones) shows a gradient in chemistry along the climatic gradient with sub-humid zone bridging between the semi-arid and humid zones. Ca/Na and Mg/Na ratios decrease from humid zone (unimodal rainfall) to semi-arid (bimodal rainfall) zone since both Na and Mg concentrations in groundwater increase along this gradient. These elements are mainly controlled by weathering reactions. Apart from the weathering of Ca, calcrete formations also play an important role in the semi-arid zone. Ion exchange process cycles between Cl and SO4 and between Ca and Na. Dissolution of CaCO3, silicate weathering and evaporation are the major mineralogical reactions. Variations in Na/Cl and Ca/Cl molar ratios indicate that shallow wells have higher molar ratios with higher variance than the deeper wells. Semi-arid zone is more silicaceous (higher Na/Cl value) than the humid zone, which has higher Ca/Cl ratio (~ 14). Effective seasonal patterns are identified using ‘recharge – discharge’ concept based on the rainfall intensity. Wells under normal scenario have low Na/Cl and Ca/Cl ratios in the ‘recharge period’ than in the corresponding ‘discharge period’ (dilution chemistry). Wells in the relatively higher pumping regions, which receive sufficient annual recharge exhibit dilution chemistry though groundwater level fluctuations are higher. However, wells in regions with insufficient recharge show ‘anti - dilution’ chemistry. Thus, the ‘recharge – discharge’ concept is useful in identifying the pumped wells from deeper wells and helps in characterizing the anthropogenic effects on the basin. Rainfall and its chemistry are to be analysed to understand the groundwater chemistry. Hence, data from various monitoring stations in India are analyzed for assessing the influence of several major factors such as, topographic location of the area, its distance from sea and annual rainfall. These stations are categorized as ‘urban’, ‘suburban’ and ‘rural’. pH, HCO3, NO3 and Mg concentrations have not changed much from coast to inland. On the other hand, SO4 and Ca concentrations changes are subjected to local emissions. Cl and Na (marine elements) originate solely from sea and a model is developed to quantify the variation in concentration of these elements under the influence of inland distance and annual rainfall. Non – linear regression model for the various categories shows that both rainfall amount and precipitation chemistry follow a power law reduction with distance from sea. Cl and Na decrease rapidly for the first 100 km distance from sea, then decrease marginally for the next 100 km and then later stabilize. Regression parameters estimated for different cases are found to be consistent (R2 ~ 0.8). Variation in one of the regression parameters accounts for the effect of urbanization. Model developed for precipitation chemistry is validated using stations from the southern peninsular region of the country. Model predictions are found to be in good correlation with observations with a relative error of ~ 5%. This relationship between the three parameters – rainfall amount, coastline distance, and concentration (in terms of Cl and Na) was validated with experiments conducted at Mule Hole SEW and Kalekere. Monthly variations in precipitation chemistry at these stations are predicted from a downscaled (in time) model and then compared with the observed data. Models developed at both annual and monthly scale are found to perform well with the field observations. Hence, this model is used for predicting the precipitation chemistry (in terms of Cl and Na) of different station points in the upper Cauvery basin. Comparative performance of alternate methods of recharge estimation i.e. Chloride mass balance (CMB) and water table fluctuation (WTF) approaches, is analyzed at various stations in the basin. Annual rainfall, Cl concentration in rain (predicted from precipitation model) and the concentration of Cl in the groundwater are the inputs for the CMB approach. Since main source of Na is from atmosphere, Na is taken as an alternative for Cl in the CMB approach and recharge is estimated using sodium mass balance (SMB) approach. Na concentrations contributed from weathering are quantified and eliminated in the analysis. Recharge estimated using SMB approach is found to be higher than CMB estimate in the semi-arid and the sub-humid zones. Water table fluctuation (WTF) method is used to compare the recharge obtained from both CMB and SMB approaches. Estimates using WTF approach are found to be higher than both CMB and SMB in the semi-arid and the sub-humid zones while SMB is found to be higher than CMB estimates. SMB and WTF estimates match well in the humid zone. An exponential relationship between recharge and annual rainfall is observed. Recharge coefficient estimated on an annual scale varied from 0.1 to 0.25 across the basin. Among CMB and SMB approaches, SMB is a better alternative for recharge estimation in semi-arid zones, where WTF approach performed poorly. Water – rock reactions are driven by the inequilibrium reactions of water with the mineral assemblage in the rock. These reactions evolve towards equilibrium with the primary minerals while a series of secondary minerals precipitate. Mass balance approach is adopted to quantify the rate at which the water – rock interactions occur in order to reach the equilibrium. Field experiments in the experimental watershed (Mule Hole SEW, ~ 4.5 km2) are carried to identify the minerals present in the region and their composition. Quartz, oligoclase, sericite, epidote and chlorite are the primary minerals while kaolinite and Fe-oxides are the secondary minerals present in this region. Percentages of oxides of different elements in each of these minerals are determined from the field experiments. Stoichiometric coefficients of different elements in each of these minerals are determined from these percentages. Long – term weathering rates are determined using these stoichiometric coefficients along with the mass fluxes of each element. Set of minerals present at different depths are found to vary among the thirteen observation wells of Mule Hole SEW. Hence, the mass balance calculations resulted in different weathering rates for a particular mineral based on the spatial location and the particular depth of the occurrence of the mineral. These weathering rates are tested for the sensitivity to carbonates with the inclusion of calcite in the mass balance calculations. With this sensitivity analysis it is observed that the presence of carbonates in the nodular form in the shallow wells has not changed the weathering reactions and their rates, and hence these wells are termed to be in the ‘silicate with secondary carbonate’ system. On the other hand, carbonates are not present in deeper wells, inclusion of which alters the equilibrium of the mass balance calculations. Thus, these wells are said to belong to the ‘silicate’ system. Anorthite present in some of the wells (MH2 and MH6) dissolves accompanied with the dissolution of carbonates. These wells are observed to belong to the third group the ‘amphibolites with primary carbonate’ system. Weathering rates of all the minerals present in these three different systems are also determined annually (short term rates). Mean of these short – term rates are observed to be the same as the long – term (over a period of 4 years) weathering rates with a minor difference of 3 – 10% in values. Thus, the weathering rates determined using mass balance approach is used to determine the quantities of concentrations of different elements contributed from the mineralogical reactions. Temporal variations in the concentrations of different chemical species in this small experimental watershed are simulated using a hydrogeochemical model. The model is developed based on a mixing cell approach, which considers the spatiotemporal variations in the recharge and the weathering inputs. Most of the weathering reactions are observed to take place in the saturated zone, which is termed as the ‘mixing zone’. This zone extends from few meters above the groundwater table to few meters below the water table. Mixing zone is discretized into series of ‘cells’ and concentrations in this zone are simulated. This group of cells is assumed to move along with the groundwater fluctuation. Sensitivity of the model is analysed subject to the variations in the recharge and the weathering fluxes. The developed model is used to simulate the concentrations of the groundwater in the three systems – ‘silicate’, ‘silicate with secondary carbonate’ and ‘amphibolites with primary carbonate’. Field data for chemical species is observed to vary in this mixing zone, boundaries of which are defined from the model simulations. Simulations corresponding to the cell at the mid depth of this mixing zone are observed to correlate well with the field data. Hence, the model developed is able to simulate the temporal variations in the groundwater chemistry. In summary, the study analyses the effects of lithological, climatic and anthropogenic factors on groundwater chemistry. The transformations in the rainwater chemistry as it reaches groundwater are analysed along different stages. A hydrogeochemical model is developed to simulate the groundwater concentrations in three different mineralogical settings over a period of three years.

No description available.

Darbo objektas: Virvyčios upės vandens kokybė. Darbo tikslas: įvertinti pasklidosios taršos, iš ekologinės ir įprastinės žemės ūkio gamybos poveikį Virvyčios upės vandens kokybei. Darbo uždaviniai: atlikti Virvyčios upės vandens kokybės analizę ties ekologinės gamybos ūkiu ir greta esančiu įprastinės gamybos ūkiu pagal svarbiausius taršos rodiklius; nustatyti sezoninę upės vandens kokybės rodiklių kaitą; palyginti ekologinės ir įprastinės žemės ūkių gamybos poveikį Virvyčios upės vandens kokybei. . Tyrimo metodai: loginis – analitinis, matematinis – statistinis. Vandens ištekliai nuolat atsinaujina, tačiau dėl taršos blogėjanti vandens kokybė riboja vandens naudojimą, kelia grėsmę mūsų sveikatai ir vandens ekosistemų funkcionavimui. Paviršinio vandens kokybė labiausiai priklauso nuo į vandens telkinius patenkančių teršalų savybių ir jų kiekių. Pagrindiniai upių cheminiai vandens teršalai yra organinės medžiagos, azoto ir fosforo junginiai, patenkantys iš pasklidosios ir sutelktosios taršos šaltinių. Darbe analizuojama Virvyčios upės vandens kokybė. Remiantis Lietuvos Respublikos aplinkos apsaugos agentūros duomenimis, Virvyčios upė priklauso vandens telkinių rizikos grupei dėl vagos ištiesinimo ir vandens kokybės, nes yra veikiama pasklidosios žemės ūkio taršos. Žemės ūkio taršą, patenkančią į paviršinius vandenis, yra sunku išmatuoti ir kontroliuoti, nes ji patenka iš šaltinių, plačiai pasklidusių tam tikroje teritorijoje. Darbe siekta nustatyti pasklidosios taršos poveikį... [toliau žr. visą tekstą] / Research object: Virvyčia river water quality Research aim: assessment of diffuse pollution from organic and conventional agricultural production, the impact on the water quality of the river Virvyčia. Objectives: Perform Virvyčia river water quality analysis on organic farm and an adjacent conventional farms by main pollution indicators; Identify seasonal river water quality parameters change; Compare organic and conventional production on the farm Virvyčia river water quality. Water resources are constantly renewing, but due to the pollution, water quality is declining and limiting the water usage, threatening our health and lives in the aquatic ecosystems. Surface water quality is the most dependent on the pollutants discharged into water bodies, their characteristics and quantities. The main chemical pollutants in river water are organic matter, nitrogen and phosphorus compounds, finding their way from diffuse or point sources of pollution. This article analyzes the water quality of Virvyčia River, which belongs to the Venta River basin. According to the Lithuanian Environmental Protection Agency, Virvyčia river water may be at risk due to channel straightening and water quality, as it is exposed to diffuse agricultural pollution. Agricultural pollution discharged into the surface water is difficult to measure and control, because it comes from sources widely scattered in a certain area. The research was aimed to determine the effects of diffuse pollution influence to... [to full text]

Thesis (M.A.)--Miami University, Dept. of Geography, 2005. / Title from first page of PDF document. Document formatted into pages; contains [1], iv, 49, [6] p. : ill., maps. Includes bibliographical references (p. 44-49).

La préservation de la richesse aquatique est devenue un souci majeur d'ordre mondial suite au risque de pénurie en eau. Au Liban, les rejets anthropiques incontrôlés et incontrôlables au bord des rivières menacent la qualité de ses eaux de surface. Pour cela, quatre cours d'eau libanais ont été choisis comme cadre d'étude : la rivière Damour, la rivière Kadisha-Abou Ali, la rivière Ibrahim et la rivière Oronte.Les différents paramètres physico-chimiques et microbiologiques étudiés ont permis dans un premier temps la construction d'une base de données de chacune de ces rivières. Une seule analyse spatio-temporelle des paramètres séparément n'aide pas à définir l'état trophique des rivières. Partant de l'idée des corrélations que peuvent exister entre certains paramètres, l'Analyse en Composante Principale (ACP) retenant la totalité de l'information sera utilisée en dépit des méthodes classiques. Cet outil statistique a permis de classer les rivières par niveau de pollution. Il a aussi aidé à observer l'impact des apports des polluants sur les différentes stations de rivières étudiées.Pour suivre le devenir des coliformes fécaux dans les eaux, l'ACP des variables microbiologiques a montré la persistance des colonies bactériennes dans les eaux malgré les conditions climatiques diverses et le régime méditerranéen torrentiel des rivières. En effet, les sédiments constituent des réservoirs potentiels de microorganismes pathogènes. Le décrochage bactérien des agrégats sédimentaires et la remise en suspension dans l'eau pose un problème alarmant de santé publique. / Preservation of aquatic wealth has worldwide become a major concern due to the risk of water shortage. In Lebanon, uncontrolled and uncontrollable anthropogenic rejections along rivers threaten the quality of its surface waters. Four Lebanese rivers were selected as study framework: The Damour river, Kadisha-Abu Ali river, Ibrahim river and Orontes river. The physico-chemical and microbiological parameters analyzed has formed a large database of these rivers. The spatio-temporal analysis of separate parameters did not help defining the trophic status of rivers. The assumption that correlations exist between certain parameters, guides us to use the Principal Component Analysis (PCA) in spite of conventional methods. This statistical tool was used to define the pollution levels in rivers. It also leads to observe the impact of pollutants inflows on different sites studied. To follow the fate of fecal coliform in water, the ACP of microbiological variables showed the persistence of bacterial colonies in water despite the various climatic conditions and the Mediterranean flow rate. Indeed, sediments are potential reservoirs of pathogenic microorganisms. The bacteria aggregated to the sediment can be present again in water column causing an alarming public health problem.

Ce travail de thèse concerne le développement de catalyseurs Fe/Faujasite afin de dégrader un cocktail de micropolluants provenant d’une eau réelle de rivière dans la Meurthe (France) avec le procédé photo-Fenton hétérogène. Les micropolluants étudiés appartiennent à 4 grandes familles : des principes actifs pharmaceutiques, des produits de soins cosmétiques, des perturbateurs endocriniens, et des composés perfluorés. Pour la première fois, dans cette thèse, la dégradation d’un mélange de 21 micropolluants à l’état de traces (2 – 80 ng/L) provenant d’une réelle eau de rivière non-dopée a été effectuée. Cependant, le fait de travailler avec des concentrations très faibles en polluants reste un challenge notamment en ce qui concerne les aspects de chimie analytiques. Ce travail de thèse est donc divisé en deux grandes parties. Dans un premier temps, il a été nécessaire de trouver la meilleure eau réelle contenant un nombre élevé de micropolluants de différentes natures à des concentrations de l’ordre de quelques ng/L mais inférieures à 100 ng/L. Pour cela différentes campagnes de prélèvement ont été effectuées dans les deux principales rivières de la région Lorraine, la Meurthe et la Moselle, en différents lieux et différentes périodes de l’année. L’eau provenant du site de Moulin Noir a été choisie. Dans une deuxième partie, nous avons développé des catalyseurs fer/Faujasite pour pouvoir tester leur efficacité pour la dégradation des micropolluants provenant du site de Moulin Noir par le procédé photo-Fenton hétérogène. Dans une étape intermédiaire, l’optimisation des paramètres opératoires du procédé photo-Fenton avec nos catalyseurs a été effectuée en utilisant deux macropolluants modèles, phénol et diclofenac / Twenty one 21 micropollutants including pharmaceuticals, personal cares product, endocrine disruptors and perfluorinated compounds presenting at ng/L in the real water of Meurthe river, were successfully quantified and removed using heterogeneous photo-Fenton process. To achieve this goal, an analytical-catalytic methodology was developed and the work steps were performed linked together in a cycle-like manner. The use of the sensitive and efficient multi-residual SPE-LC-MS/MS analytical method allowed us to analyze and quantify the mixture of micropollutants present in a complex matrix during 3 periods of the year with different weather conditions, from 5 sampling sites. Results showed that the highest concentrations of most of the present micropollutants are observed in October at ng/L, Moulin Noir sampling site found to contain the largest number and type of these pollutants, the WWTP was not efficient in the removal of the micropollutants present in water and the drinking water used from tab was totally safe from micropollutants. The calculation of the fluxes and estimation of the mass balance at the rivers confluence confirmed the good precision and reliability of our measurement methodology, and specify the most suitable site for water to be taken from to be used in the removal tests which was Moulin Noir. Having the appropriate water sample, an efficient iron impregnated Faujasite catalyst was developed and used in a photo-Fenton process for the micropollutant removal tests. After characterization and optimization of the different experimental factors using the 2 model macropollutants, phenol and diclofenac, the real tests were performed on real water samples from Moulin Noir. The results demonstrated the good efficiency of the photo-Fenton process with the cocktail of 21 micropollutants. Except for sulfamethoxazole and PFOA, the concentrations of all the other micro-contaminants became lower than the limit of quantification of the LC-MS/MS after 30 minutes or 6 hours of photo-Fenton treatment depending on their initial concentrations under the effect of both adsorption and Fenton mechanisms. Comparing the photo-Fenton process to heterogeneous photocatalytic degradation over TiO2, Faster micropollutants removal occurred with the zeolite

No description available.

Thesis (M.Sc. (Microbiology)) -- University of Limpopo, 2016 / Access to safe drinking water is a major problem globally and it mostly affects people living in low-income countries. The lack of potable water leads to the use of raw water from surface or ground water sources for drinking and other household purposes. A water filtration unit was designed and constructed using fabric, gravel and sand, which were wet-packaged into a 20 L bucket. The efficiency of the filter unit to improve the bio-physicochemical properties of contaminated water was tested using surface waters from rivers in the Sekhukhune area. Physico-chemical parameters tested included turbidity, colour, total suspended solids (TSS), total dissolved solids (TDS), total hardness and pH. Turbidity and colour were the most improved characteristics, where turbidity improved by 69% and colour by 80%. Other parameters such as total hardness, TSS and TDS were non-significantly reduced following treatment with the filtration unit. The amount of soluble solids in raw water was well within allowable limits by WHO standards. Microbiological tests included heterotrophic bacteria, total coliform and faecal coliform counts. The bacterial load was too numerous to count for the untreated water, however, after treatment with the filtration unit, heterotrophic bacterial load decreased to 15 x 10103 CFU/ml, total coliforms to 14 x 10 2 CFU/100ml and faecal coliforms to 11 x 10 2 CFU/100ml. Further treatment with UV sterilization unit resulted in undetectable amount of bacteria. The unit designed in this study can be beneficial in those rural communities were clean water is not available, it is easy to construct and simple to operate and most importantly it reduced contaminants in surface water. The UV unit incorporated in this study is not cost effective, therefore, other household treatment options such as chlorination and boiling which are easily accessible to most communities can be used to further eliminate remaining microorganisms after filtration. The effective shortest boiling time and minimum dosage of Na(OCl2) have been previously tested in our laboratory and total elimination of bacteria was achieved within 2 minutes of rolling boil and after 30 minutes following addition of 5ml/20L of liquid chlorine.

Cette recherche évalue le degré de régulation hydrologique induite par le barrage-réservoir Paso de las Piedras sur la Sauce Grande et quantifie les effets de cette régulation sur la hydrologie, la morphologie et la température de l'eau de la rivière en aval. Le travail de thèse consiste en une évaluation exhaustive et systématique des impacts du barrage-réservoir sur le système fluvial basée sur la compréhension des processus naturels qui se produisent en amont. En plus de fournir des informations sur les impacts hydrologiques, morphologiques et thermiques de la construction du barrage Paso de las Piedras et de l'exploitation de son réservoir, cette étude génère des séries de données climatiques et hydrologiques qui fournissent une base significative sur laquelle fonder des recherches futures. Par ailleurs, cette étude met en place un cadre méthodologique appliqué à l'analyse hydrogéomorphologique des bassins versants non jaugés qui a un grand potentiel d'application dans d'autres bassins de la région similaires ainsi que dans d'autres régions semi-arides du monde. / Despite the regional importance of the Sauce Grande River as main source for water supply and the large capacity of the Paso de las Piedras Reservoir, both the hydrology of the river basin and the effects of the impoundment on the river environment remain poorly evaluated. This study provides the very first assessment of the degree of flow regulation induced by the Paso de las Piedras Dam on the middle section of the Sauce Grande River, and quantifies its impacts on the hydrology, morphology and patterns of water temperature of the river downstream from the impoundment. In addition to providing new information on the response of regulated rivers to upstream impoundment and on the effects of impoundment on the Sauce Grande River specifically, this study generates spatial, climatic and hydrologic data and implements a methodological framework to hydrological assessment of ungauged basins.