Les facteurs qui régissent l'intensité et la répartition de la recharge naturelle et artificielle dans les aquifères cristallins altérés et fracturés sont mal connus. Ce sont cependant les caractéristiques déterminantes de ce type de roche—ces roches sont très hétérogènes—qui rendent difficile l’estimation des flux dans ces milieux ainsi que des propriétés hydrauliques qui les contrôlent. La première partie de ce manuscrit fournit un état des connaissances sur la recharge des eaux souterraines et ses méthodes d’estimation, permettant de comprendre les défis scientifiques et sociétaux abordés dans cette thèse. La deuxième partie présente les travaux numériques et expérimentaux menés pour approfondir notre compréhension de la dynamique des flux d’eaux souterraines dans ces milieux hétérogènes à plusieurs échelles. Le premier axe de recherche porte sur les processus de recharge naturelle à l’échelle du bassin versant. La recharge diffuse a été modélisée avec un modèle physique simple d’infiltration et comparée à des estimations préalables de recharge totale. Nos résultats illustrent la forte dépendance de la recharge aux précipitations et à l’irrigation, et l’importance de la recharge focalisée. Les facteurs responsables de la distribution spatiale de la recharge sont aussi étudiés. Le deuxième axe est basé sur le suivi de la mise en eau d’un bassin de recharge artificielle dans un site hautement monitoré et bien équipé. Ces observations ont été interprétées avec des modèles analytiques et numériques. Ces modèles ont mis en évidence l’existence de flux préférentiels horizontaux, mais aussi d’une compartimentation latérale qui entrave la propagation des intrants de recharge. / The factors governing the intensity and distribution of natural and artificial recharge in weathered and fractured crystalline aquifers are poorly understood. However, it is the defining characteristics of this type of rock—these rocks are very heterogeneous—that make the estimation of fluxes and the hydraulic properties controlling them difficult. The first of its two parts provides the theoretical framework on groundwater recharge processes and its estimation methods for comprehending the scientific and societal challenges discussed in this thesis. The second part presents the numerical and experimental work carried out to deepen our understanding of the dynamics of groundwater flows in these heterogeneous underground environments at several scales. The first line of research focuses on natural recharge processes at the watershed scale. Diffuse recharge was modeled with a simple physical infiltration model and compared to previous estimates of total recharge. Our results highlight the strong dependence of recharge on rainfall and irrigation, and the importance of focused recharge. The factors responsible for the spatial distribution of recharge are also studied. The second axis is based on the monitoring of the filling of an artificial recharge basin at a highly monitored and well-equipped site. These observations were interpreted with analytical and numerical models to improve our knowledge of flow dynamics in fractured crystalline rocks at the medium scale. These models illustrated the existence of preferential horizontal flows, but also of a lateral compartmentalization that hinders the propagation of recharge inputs.

<p>Kunskap om grundvattenbildningen är nödvändig för att man ska kunna förutsäga konsekvenserna av grundvattenuttag och underjordsbyggande. Grundvattenbildningen i berggrunden är dock svår att uppskatta. Syftet med avhandlingen var att öka förståelsen av grundvattenbildningen i kristallin berggrund, att undersöka hur grundvattenbildningen ska uppskattas samt att utveckla nya modeller för att beskriva grundvattenbildningen. Studien grundades på tre angreppssätt: grundvattendatering med freoner (CFC), geohydrauliska observationer och matematisk modellering.</p><p>Koncentrationerna av CFC-11 och CFC-113 befanns vara låga i det undersökta berggrundvattnet, vilket i kombination med låga syrgashalter tyder på anaerob nedbrytning. Koncentrationerna av CFC-12 och tritium överensstämde ganska väl, vilket betyder att den skenbara åldern kan vara den sanna åldern. Resultaten tyder på att CFC-datering inte är pålitlig i skogsmiljöer med finkornigt jordtäcke.</p><p>Vid nederbörd observerades ett snabbt gensvar i den hydrauliska potentialen i den studerade bergakviferen, trots det 10 m mäktiga moräntäcket. En avsevärd del av de observerade potentialvariationerna befanns vara belastningseffekter, som inte innebar någon magasinsförändring eller något vattenflöde. Berggrundens belastningseffektivitet uppskattades, ur potentialens svar på lufttrycksförändringar, till 0,95. Ytbelastningen beräknades från mätningar av lufttryck, vatten i jordtäcket och snö. Omkring 20 % av årstidsvariationen hos den hydrauliska potentialen uppskattades bero på enbart belastningsförändringar. En enkel begreppsmässig modell kunde användas för att simulera den observerade hydrauliska potentialen. För att beskriva enskilda grundvattenbildningstillfällen på bästa sätt var det nödvändigt att ta hänsyn till effekten av ytbelastningen.</p><p>Numeriska experiment gjordes med en modell av en jord–bergprofil. När berget modellerades som ett heterogent kontinuum bildades omättade zoner i berget vid stora hydrauliska gradienter. Fenomenet uppträdde i områden där låggenomsläppliga zoner låg uppströms höggenomsläppliga zoner, och ledde till minskad hydraulisk konduktivitet i berget.</p> / <p>Knowledge about the groundwater recharge is essential for the prediction of impacts of groundwater withdrawal and underground construction. Recharge in the bedrock is, however, difficult to estimate. The objectives of this thesis were to increase the understanding of groundwater recharge in crystalline bedrock, to investigate how the recharge could be estimated, and to develop new models to describe the recharge. The study was based on three approaches: groundwater dating using chlorofluorocarbons (CFCs), geohydraulic field measurements, and mathematical modelling.</p><p>Low concentrations of CFC-11 and CFC-113 were found in the bedrock groundwater, which in combination with low dissolved-oxygen levels indicated anaerobe degradation. The CFC-12 and tritium concentrations agreed fairly well, which means that apparent ages could be true ages. The results suggest that CFC dating may not be reliable at forested, humid sites covered by fine-grained soil.</p><p>A quick response in hydraulic head to precipitation was observed in the studied bedrock, despite the 10-m thick till cover. A substantial portion of observed head variations was found to be loading effects, involving no storage changes or water flow. The loading efficiency of the bedrock was estimated, from the air-pressure response, to be 0.95. The surface loading was calculated from measurements of air pressure, water in the soil, and snow. About 20% of the seasonal variation of the hydraulic head was estimated to be related to loading changes only. A simple conceptual model could be used to simulate the observed hydraulic heads. The loading effect had to be included to properly describe individual recharge events.</p><p>Numerical experiments were performed with a soil–bedrock profile. When the rock was modelled as a heterogeneous continuum, unsaturated zones developed at high hydraulic gradients. The phenomenon appeared in areas where low-conductive zones were located upstream of high-conductive zones, decreasing the effective hydraulic conductivity of the material.</p>

Kunskap om grundvattenbildningen är nödvändig för att man ska kunna förutsäga konsekvenserna av grundvattenuttag och underjordsbyggande. Grundvattenbildningen i berggrunden är dock svår att uppskatta. Syftet med avhandlingen var att öka förståelsen av grundvattenbildningen i kristallin berggrund, att undersöka hur grundvattenbildningen ska uppskattas samt att utveckla nya modeller för att beskriva grundvattenbildningen. Studien grundades på tre angreppssätt: grundvattendatering med freoner (CFC), geohydrauliska observationer och matematisk modellering. Koncentrationerna av CFC-11 och CFC-113 befanns vara låga i det undersökta berggrundvattnet, vilket i kombination med låga syrgashalter tyder på anaerob nedbrytning. Koncentrationerna av CFC-12 och tritium överensstämde ganska väl, vilket betyder att den skenbara åldern kan vara den sanna åldern. Resultaten tyder på att CFC-datering inte är pålitlig i skogsmiljöer med finkornigt jordtäcke. Vid nederbörd observerades ett snabbt gensvar i den hydrauliska potentialen i den studerade bergakviferen, trots det 10 m mäktiga moräntäcket. En avsevärd del av de observerade potentialvariationerna befanns vara belastningseffekter, som inte innebar någon magasinsförändring eller något vattenflöde. Berggrundens belastningseffektivitet uppskattades, ur potentialens svar på lufttrycksförändringar, till 0,95. Ytbelastningen beräknades från mätningar av lufttryck, vatten i jordtäcket och snö. Omkring 20 % av årstidsvariationen hos den hydrauliska potentialen uppskattades bero på enbart belastningsförändringar. En enkel begreppsmässig modell kunde användas för att simulera den observerade hydrauliska potentialen. För att beskriva enskilda grundvattenbildningstillfällen på bästa sätt var det nödvändigt att ta hänsyn till effekten av ytbelastningen. Numeriska experiment gjordes med en modell av en jord–bergprofil. När berget modellerades som ett heterogent kontinuum bildades omättade zoner i berget vid stora hydrauliska gradienter. Fenomenet uppträdde i områden där låggenomsläppliga zoner låg uppströms höggenomsläppliga zoner, och ledde till minskad hydraulisk konduktivitet i berget. / Knowledge about the groundwater recharge is essential for the prediction of impacts of groundwater withdrawal and underground construction. Recharge in the bedrock is, however, difficult to estimate. The objectives of this thesis were to increase the understanding of groundwater recharge in crystalline bedrock, to investigate how the recharge could be estimated, and to develop new models to describe the recharge. The study was based on three approaches: groundwater dating using chlorofluorocarbons (CFCs), geohydraulic field measurements, and mathematical modelling. Low concentrations of CFC-11 and CFC-113 were found in the bedrock groundwater, which in combination with low dissolved-oxygen levels indicated anaerobe degradation. The CFC-12 and tritium concentrations agreed fairly well, which means that apparent ages could be true ages. The results suggest that CFC dating may not be reliable at forested, humid sites covered by fine-grained soil. A quick response in hydraulic head to precipitation was observed in the studied bedrock, despite the 10-m thick till cover. A substantial portion of observed head variations was found to be loading effects, involving no storage changes or water flow. The loading efficiency of the bedrock was estimated, from the air-pressure response, to be 0.95. The surface loading was calculated from measurements of air pressure, water in the soil, and snow. About 20% of the seasonal variation of the hydraulic head was estimated to be related to loading changes only. A simple conceptual model could be used to simulate the observed hydraulic heads. The loading effect had to be included to properly describe individual recharge events. Numerical experiments were performed with a soil–bedrock profile. When the rock was modelled as a heterogeneous continuum, unsaturated zones developed at high hydraulic gradients. The phenomenon appeared in areas where low-conductive zones were located upstream of high-conductive zones, decreasing the effective hydraulic conductivity of the material.

The handbook presented in this paper summarises the results of the research initiative “International Water Research Alliance Saxony” (IWAS). The subproject “IWAS Vietnam” (Phase I, October 2008 – December 2010) focuses on the model region “South-East Asia” with emphasis on Vietnam. The project started as a joint research initiative between German and Vietnamese organisations and included contributions from academic, private and public sector in both countries. The handbook was compiled by the Technische Universität Dresden (project coordination), the Institute for Technical and Scientific Hydrology and Dresden Drainage and Sewerage Company, with substantial contributions from Vietnamese partners. / Sổ tay hướng dẫn trong bài viết này tóm lược các kết quả của sáng kiến nghiên cứu từ “Liên minh Nghiên cứu ngành nước quốc tế bang Saxony” (IWAS). Dự án nhánh “IWAS Việt Nam” (giai đoạn 1, 10/2008 - 12/2010) tập trung vào khu vực Đông Nam Á với trọng tâm là Việt Nam. Dự án khởi động như một sáng kiến liên kết nghiên cứu giữa các tổ chức của CHLB Đức và Việt Nam với sự đóng góp từ các đơn vị tư nhân, nhà nước và trường đại học của cả hai quốc gia. Quyển sổ tay này được biên soạn bởi Đại học Kỹ thuật Dresden (cơ quan điều phối dự án), Viện Công nghệ và Khoa học Thủy văn, và Công ty Thoát nước Dresden, cùng với sự đóng góp quan trọng của các đối tác Việt Nam.

The Cuatrociénegas Basin is located in the Chihuahuan Desert, Coahuila, Mexico. Over 500 springs and groundwater-dependent ecosystems with >70 endemic species flank the 2,600-meter Sierra San Marcos that bisects the 1,200 square kilometer valley. The west sub-basin contains fracture-controlled springs with elevated relative discharge (~85 percent of total), temperature (~31.0°-34.0°C), and total dissolved solids (~90 milligrams/liter chloride) compared to the east sub-basin, that has stratigraphically-controlled springs with lower relative discharge (~15 percent), temperature (~28.0°-30.0°C), and total dissolved solids (~30 milligrams/liter chloride). Canals convey spring discharge out of the formerly closed valley. Groundwater development since the 1980s lowered groundwater levels >10 meters in adjacent basins and caused some springs to cease flowing. The author hypothesizes that (1) both local and regional recharge are significant, (2) an integrative data approach can delineate recharge zones, and (3) the low-elevation of the Cuatrociénegas Basin, fault-associated secondary carbonate aquifer permeability, and stratigraphic influences on permeability control spring locations. To test these hypotheses, the research (1) develops hydrogeologic conceptual models of recharge areas using remotely-sensed topography, hydrogeologic data (e.g., spring geochemistry, temperature, and discharge), and geologic mapping; (2) delineates recharge areas by sequentially including upgradient catchments to match observed spring discharge using geographic information system catchment delineation, chloride-balance recharge estimation, and analytical model interbasin flow evaluation; (3) explains spatial variations in spring chloride, discharge, and temperature using environmental tracers (e.g., [delta]¹⁸O, noble gases, ³H) and an elevation-dependent recharge rate; and (4) uses land gravimetry surveys to generate best-fit hydrogeologic cross sections in areas of high spring density. The author concludes that local precipitation is insufficient to generate observed spring discharge. Waters with <0.1 tritium units indicate regional flow and aquifer residence times of >50 years. Water-budget based catchment delineation suggests west basin fractures tap a (>10,000-square kilometer) regional carbonate aquifer. Thus, groundwater management should be extended outside the Cuatrociénegas Basin. East basin canyons intersect the potentiometric surface of a stratigraphically controlled (local/regional) aquifer recharged in the 500-square kilometer Sierra San Marcos. Sierra La Madera recharge explains Ocampo Valley predevelopment flow and chloride concentration. This approach can be applied to delineate similar developing arid aquifers. / text

Public water policy decision making tends to be too complex and dynamic to be described fully by traditional, rational models. Information intended to improve decisions often is rendered ineffective by a failure to understand the process. An alternative, holistic description of how such decisions actually are made is presented here and illustrated with a case study. The role of information in the process is highlighted. Development of a Regional Recharge Plan for Tucson, Arizona is analyzed as the case study. The description of how decisions are made is based on an image of public water policy decision making as 1) a structured, nested network of individuals and groups with connections to their environment through their senses, mediated by their knowledge; and 2) a nonlinear process in which decisions feed back to affect the preferences and intentions of the people involved, the structure of their interactions, and the environment in which they operate. The analytical components of this image are 1) the decision makers, 2) the relevant features of their environment, 3) the structure of their interactions, and 4) the products or outputs of their deliberations. Policy decisions analyzed by these components, in contrast to the traditional analysis, disclose a new set of relationships and suggest a new view of the uses of information. In context of information use, perhaps the most important output of the decision process is a shared interpretation of the policy issue. This interpretation sets the boundaries of the issue and the nature of issue-relevant information. Participants are unlikely to attend to information incompatible with the shared interpretation. Information is effective when used to shape the issue interpretation, fill specific gaps identified as issue-relevant during the process, rationalize choices, and reshape the issue interpretation as the issue environment evolves.

Ziel der Dissertation ist die hydrogeologische Charakterisierung von Karstgrundwasserleitern in der semi-ariden Klimazone, welche oftmals durch Übernutzung und anthropogene Verschmutz-ung bedroht sind. Trotz oft eingeschränkter Datenlage und einem unzureichenden Systemver-ständnis müssen quantitative und qualitative Faktoren, wie z.B. Grundwasserneubildungsrate, Aquiferparameter, Strömungs- und Stofftransportdynamik, Verschmutzungsempfindlichkeit und anthropogene Einflüsse quantifiziert werden. Jedoch können diese Gebiete auch günstige Eigenschaften für eine Charakterisierung, wie eine zeitlich eng begrenzte Impulsfunktion der Grundwasserneubildung durch intensive, kurze Niederschlagsereignisse sowie lange ungestörte Rezessionsperioden, aufweisen. Dies gilt für das in der Levante gelegene Untersuchungsgebiet. Die zeitliche und räumliche hydrologische Variabilität wurde durch ein ausgedehntes Messnetz hochaufgelöst erfasst. Zur Auswertung dieser Daten wurden konzeptionell korrekte, jedoch möglichst einfach anwendbare quantitative Verfahren und Modelle entwickelt und angewandt, was die Übertragbarkeit der Methoden auf weitere Trockengebiete ermöglicht. Durch eine Zusammenstellung und Auswertung hydrochemischer Langzeitdaten konnte die natürliche Hintergrundkonzentration von Chlorid im Grundwasser für 33 Quelleinzugsgebiete ermittelt werden. Darauf aufbauend war es möglich, durch eine Chloridmassenbilanz sowohl den langjährige mittlere Anteil der Grundwasserneubildung am Niederschlag (25–50%) zu bestimmen, als auch den Abwasseranteil im Quellwasser anhand rezenter Proben zu quantifizieren (0–20%). Anhand eines Speicher-Durchflussmodelles konnten sowohl Aquiferparameter im Einzugs-gebietsmaßstab als auch eine Tageszeitreihe der Grundwasserneubildung exemplarisch für die Auja-Quelle, die größte Süßwasserquelle im Unteren Jordantal, erfasst werden. Diese sowie weitere Quellen der Region sind durch ein „röhrengedrosseltes“ Abflussverhalten, d.h. eine Begrenzung der Quellschüttung, gekennzeichnet. Der hydrogeologisch komplexe Aquifer und das nichtlineare Systemverhalten bei Erreichen der maximalen Schüttung erfordern ein besonders angepasstes Modell, welches auch einen ausgeprägten hydraulischen Austausch zwischen den Karströhren und der geklüfteten Gesteinsmatrix berücksichtigen muss. Eine Reihe von Parametern konnte aus einer Rezessions- und Ereignis-Analyse der Abflussganglinie ermittelt werden. Das Speicher-Durchflussmodell benötigt lediglich sechs Kalibrierparameter und erlaubt eine sehr gute Simulation der Abflussganglinie. Die effektive Aquifer-Porosität wurde durch Kalibration ermittelt (ca. 2.4%). Über den simulierten 45-Jahres-Zeitraum führten die fünf niederschlagsreichsten Jahre zu einem Drittel der gesamten Grundwasserneubildung. Die zeitlich hoch aufgelösten Quellmessungen ermöglichten eine Quantifizierung der hydraulischen Reaktionszeiten sowie der mittleren Verweilzeiten, der Durchbruchsdauer und der relativen Anteile der schnellen Fließkomponente nach Niederschlagsereignissen. Diese Daten dienen sowohl einer Abschätzung der schnellen Neubildungsprozesse (vor allem Fokussierung im Epikarst und schnelles präferentielles Fließen durch die Vadose Zone) als auch einer Beurteilung der Verschmutzungsempfindlichkeit der Karstquellen. Weiterhin konnte eine Zugehörigkeit der beiden, 3500 m voneinander entfernten, artesischen Jericho-Quellen Sultan und Duyuk zu einem gemeinsamen Röhren- und damit Karstsystem nachgewiesen werden.

Thesis (M.E.S.)--Evergreen State College, 2009. / Title from title screen (viewed 4/15/2010). Includes bibliographical references (leaves 63-67).

abstract: Population growth within drylands is occurring faster than growth in any other ecologic zone, putting pressure on already stressed water resources. Because the availability of surface water supplies in drylands tends to be highly variable, many of these populations rely on groundwater. A critical process contributing to groundwater recharge is the interaction between ephemeral channels and groundwater aquifers. Generally, it has been found that ephemeral channels contribute to groundwater recharge when streamflow infiltrates into the sandy bottoms of channels. This process has traditionally been studied in channels that drain large areas (10s to 100s km2). In this dissertation, I study the interactions between surface water and groundwater via ephemeral channels in a first-order watershed located on an arid piedmont slope within the Jornada Experimental Range (JER) in the Chihuahuan Desert. To achieve this, I utilize a combination of high-resolution observations and computer simulations using a modified hydrologic model to quantify groundwater recharge and shed light on the geomorphic and ecologic processes that affect the rate of recharge. Observational results indicate that runoff generated within the piedmont slope contributes significantly to deep percolation. During the short-term (6 yr) study period, we estimated 385 mm of total percolation, 62 mm/year, or a ratio of percolation to rainfall of 0.25. Based on the instrument network, we identified that percolation occurs inside channel areas when these receive overland sheetflow from hillslopes. By utilizing a modified version of the hydrologic model, TIN-based Real-time Integrated Basin Simulator (tRIBS), that was calibrated and validated using the observational dataset, I quantified the effects of changing watershed properties on groundwater recharge. Distributed model simulations quantify how deep percolation is produced during the streamflow generation process, and indicate that it plays a significant role in moderating the production of streamflow. Sensitivity analyses reveal that hillslope properties control the amount of rainfall necessary to initiate percolation while channel properties control the partitioning of hillslope runoff into streamflow and deep percolation. Synthetic vegetation experiments show that woody plant encroachment leads to increases in both deep percolation and streamflow. Further woody plant encroachment may result in the unexpected enhancement of dryland aquifer sustainability. / Dissertation/Thesis / Doctoral Dissertation Geological Sciences 2017

As maiores taxas de recarga subterrânea do Sistema Aquífero Guarani (SAG) ocorrem nas áreas de afloramento das Formações Botucatu e Pirambóia. O principal objetivo deste trabalho foi avaliar as taxas de recarga subterrânea e suas relações com as variações da precipitação e do uso do solo na bacia hidrográfica do Ribeirão da Onça, situada em área de afloramento do SAG. A variação do nível freático foi medida em 11 poços de monitoramento, distribuídos em diferentes culturas agrícolas na bacia, durante o período de estudo (Outubro de 2004 até Setembro de 2011). Técnicas de tratamento de imagens multiespectrais foram usadas para mapear o uso do solo na bacia. A recarga direta em cada poço foi estimada por um método de escala local (Water Table Fluctuation, WTF) um método de escala de regional (Recession Curve Displacement Method, RCDM). Outro método de escala local foi avaliado (Chloride Mass Balance, CMB) em poços com cultura de pastagem. Foi estimado o armazenamento subterrâneo, o escoamento direto, o escoamento de base e a percolação profunda do aquífero em direção à Formação Botucatu. A espacialização da recarga direta para a bacia, usando os resultados do método WTF, foi feita de acordo com as áreas das culturas agrícolas. A recarga direta para a bacia foi estimada entre 80 mm e 359 mm, correspondente a 7% e 20% da precipitação anual de aproximadamente 1175 mm e de 1808 mm, respectivamente. A recarga direta, usando o método RCDM, variou entre 16% (229 mm) e 34% (~618 mm) da precipitação do ano 2009-2010 e 2010-2011, respectivamente. Foram observadas menores taxas de recarga nas áreas com cultura de eucaliptos em citros em relação às áreas com pastagem e cana-de-açúcar. Caso haja diminuição das precipitações e aumento das áreas de eucaliptos na bacia do Ribeirão da Onça, a recarga poderá sofrer diminuição, ocasionando menores escoamentos de base em direção ao Ribeirão da Onça. A avaliação contínua da recarga nas áreas de afloramento é essencial para a futura utilização das águas do SAG nas atividades agrícolas, industriais e de abastecimento público. / The major groundwater recharge rates of the Guarani Aquifer System (GAS) occur in the outcrop areas of Botucatu and Pirambóia Formations. This work aimed at estimating recharge rates and its relation with precipitation and land use in Ribeirão da Onça watershed, located in outcrop area of the GAS, during a seven years term monitoring (October 2004 until September 2011). The water table fluctuations were measured at 11 piezometers, located in different crops areas. Processing techniques for multispectral images were used to map the land use. Recharge was estimated trough a local-scale method (Water Table fluctuation, WTF) and a basin-scale method (Recession Curve Displacement Method, RCDM). Another local-scale method was used (Chloride Mass Balance, CMB) to estimate recharge rate in grassland area. The upscaling of recharge estimates using the results of WTF method for the watershed was performed, according to crop areas. Groundwater storage, quickflow, baseflow and deep percolation toward from the shallow aquifer to Botucatu Formation were also estimated. The results demonstrated that recharge estimates for areas with eucalyptus and citrus was lower than areas with grassland, sugar cane and citrus. Annual recharge rates estimated by WTF ranged from 80 mm (7%) to 359 mm (20%) for annual rainfall of about 1175 mm and 1808 mm, respectively. Recharge rates by RCDM ranged between about 229 (2009-2010) mm to 618 mm (2010-2011) for the entire watershed. CMB method provides mean recharge rate about 590 mm (2010-2011). These results suggest that if eucalyptus areas continue rising in the watershed, the recharge rates and baseflow would considerably decrease. The continuing assessment of recharge in outcrop areas is essential for future use of the GAS.