Journal Title
Title of Journal: Hydrogeology Journal
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Abbravation: Hydrogeology Journal
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Publisher
Springer-Verlag
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Authors: Marios Sophocleous
Publish Date: 2002/01/11
Volume: 10, Issue: 1, Pages: 52-67
Abstract
The interactions between groundwater and surface water are complex To understand these interactions in relation to climate landform geology and biotic factors a sound hydrogeoecological framework is needed All these aspects are synthesized and exemplified in this overview In addition the mechanisms of interactions between groundwater and surface water GW–SW as they affect recharge–discharge processes are comprehensively outlined and the ecological significance and the human impacts of such interactions are emphasized Surfacewater and groundwater ecosystems are viewed as linked components of a hydrologic continuum leading to related sustainability issues This overview concludes with a discussion of research needs and challenges facing this evolving field The biogeochemical processes within the upper few centimeters of sediments beneath nearly all surfacewater bodies hyporheic zone have a profound effect on the chemistry of the water interchange and here is where most of the recent research has been focusing However to advance conceptual and other modeling of GW–SW systems a broader perspective of such interactions across and between surfacewater bodies is needed including multidimensional analyses interface hydraulic characterization and spatial variability sitetoregion regionalization approaches as well as crossdisciplinary collaborationsLes interactions entre les eaux souterraines et les eaux de surface sont complexes Pour comprendre ces interactions qui dépendent du climat des paysages de la géologie et de facteurs biotiques il est nécessaire de bien connaître le cadre hydrogéoécologique Tous ces aspects sont synthétisés et donnés en exemple dans cette revue densemble En outre dans la mesure où ils affectent les processus de recharge–décharge les mécanismes des interactions entre les eaux souterraines et les eaux de surface sont largement ébauchés et la signification écologique et les impacts humains de telles interactions sont mises en avant Les écosystèmes des eaux de surface et souterraines sont conçus comme étant des composantes liées appartenant à un continuum hydrologique conduisant à des questions sur le développement durable Cette revue densemble conclut par une discussion sur les besoins de recherche et des problèmes posés par ce thème en développement Les processus biogéochimiques dans les quelques centimètres de sédiments immédiatement sous toutes les eaux de surface la zone hyporhéique ont un effet essentiel sur le chimisme des échanges deau et cest sur ce point que se sont concentrées la plupart des recherches récentes Cependant pour faire progresser la modélisation conceptuelle et les autres modélisations des systèmes eau souterraine–eau de surface une perspective plus large de ces interactions à lintérieur et entre les hydrosystèmes de surface est nécessaire en prenant en compte des analyses multidimensionnelles la caractérisation hydraulique de linterface et la variabilité spatiale les approches par régionalisation du site local à la région aussi bien que des collaborations transdisciplinairesLas interacciones entre aguas subterráneas y superficiales son complejas Para entenderlas en relación con factores climáticos de relieve del terreno geológicos y bióticos se necesita un marco hidrogeoecológico robusto Este artículo resume y presenta ejemplos de todos estos aspectos Además se describe con profusión los mecanismos de interacción entre las aguas superficiales y subterráneas que afectan a los procesos de recarga y descarga haciendo hincapié en la importancia ecológica y en los impactos humanos de tales interacciones Los ecosistemas de aguas superficiales y subterráneas son considerados como elementos unidos de un continuo hidrológico que llevan a plantear su sustentabilidad La revisión concluye con una discusión de las necesidades de investigación y de los retos que afronta este campo tan dinámico Los procesos biogeoquímicos que se producen en los primeros centímetros de los sedimentos en la mayoría de los cursos y reservorios de aguas superficiales zona hiporreica tienen un profundo efecto en la química del intercambio de agua y es aquí donde incide la mayoría de la investigación más reciente Sin embargo se requiere una perspectiva más amplia de las interacciones entre aguas superficiales y subterráneas con el objeto de avanzar en la modelación de estos sistemas incluyendo análisis multidimensionales caracterización de la hidráulica en la interfaz y de la variabilidad espacial métodos de regionalización y colaboraciones interdisciplinares
Keywords:
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Other Papers In This Journal:
- Simulation of seawater intrusion into the Khan Yunis area of the Gaza Strip coastal aquifer
- Modelling groundwater flow of the Trifa aquifer, Morocco
- Competition between topography- and compaction-driven flow in a confined aquifer: Some analytical results
- Remediation scenarios for selenium contamination, Blackfoot watershed, southeast Idaho, USA
- Radiocarbon dating and the 36 Cl/Cl evolution of three Great Artesian Basin wells at Dalhousie, South Australia
- Influence of rainfall on the deformation and stability of a slope in overconsolidated clays: a case study
- Transport and deposition of suspended particles in saturated porous media: hydrodynamic effect
- Model of hydrological behaviour of the anthropized semiarid wetland of Las Tablas de Daimiel National Park (Spain) based on surface water–groundwater interactions
- Determination of hydraulic parameters of an unconfined alluvial aquifer by the floodwave-response technique
- A theoretical analysis of basin-scale groundwater temperature distribution
- Numerical modeling of stress-permeability coupling in rough fractures
- Using Hydrogeochemical Methods To Evaluate Complex Quaternary Subsurface Stratigraphy Block Island, Rhode Island, USA
- Karst groundwater: a challenge for new resources
- Evaluation of retention properties of a semi-synthetic fractured block from modelling at performance assessment time scales (Äspö Hard Rock Laboratory, Sweden)
- Groundwater management by riverbank filtration and an infiltration channel: the case of Obrenovac, Serbia
- A hydrogeological conceptual approach to study urban groundwater flow in Bucharest city, Romania
- Groundwater recharge: an overview of processes and challenges
- Integrating hydraulic conductivity with biogeochemical gradients and microbial activity along river–groundwater exchange zones in a subtropical stream
- Is self-regulation a myth? Case study on Spanish groundwater user associations and the role of higher-level authorities
- Reply to comment on “Geochemical heterogeneity and isotope geochemistry of natural attenuation processes in a gasoline-contaminated aquifer at the Hnevice site, Czech Republic”: report published in Hydrogeology Journal (2007) 15: 961-976, by Barbora Topinkova, Kamil Nesetril, Josef Datel, Ondrej Nol, Petr Hosl
- Automatic estimation of aquifer parameters using long-term water supply pumping and injection records
- Book review: Groundwater around the World: A Geographic Synopsis, by Jean Margat and Jac van der Gun (CRC Press, 2013)
- Effect of sorption intensities on dispersivity and macro-dispersion coefficient in a single fracture with matrix diffusion
- The bailer test: a simple effective pumping test for assessing borehole success
- Groundwater resources in the Upper Guadiana Basin (Spain): a regional modelling analysis
- Evaluation of graphical and multivariate statistical methods for classification of water chemistry data
- Groundwater source assessment program for the state of Hawaii, USA: methodology and example application
- Thermal tracer testing in a sedimentary aquifer: field experiment (Lauswiesen, Germany) and numerical simulation
- Heterogeneous seepage at the Nopal I natural analogue site, Chihuahua, Mexico
- The role of faulting on surface deformation patterns from pumping-induced groundwater flow (Las Vegas Valley, USA)
- Investigating the influence of aquifer heterogeneity on the potential for thermal free convection in the Yarragadee Aquifer, Western Australia
- Dynamics and interaction of organic carbon, turbidity and bacteria in a karst aquifer system
- Effect of advective mass transfer on field scale fluid and solute movement: Field and modeling studies at a waste disposal site in fractured rock at Oak Ridge National Laboratory, Tennessee, USA
- The impact of intensive groundwater abstraction on recharge to a shallow regional aquifer system: evidence from Bangladesh
- Characterization of a Pleistocene thermal spring in Mozambique
- Ground truthing groundwater-recharge estimates derived from remotely sensed evapotranspiration: a case in South Australia
- Estimation of aquifer hydraulic parameters from surface geophysical measurements: a case study of the Upper Cretaceous aquifer, central Sinai, Egypt
- MODFLOW procedure to simulate axisymmetric flow in radially heterogeneous and layered aquifer systems
- Estimating groundwater recharge beneath irrigated farmland using environmental tracers fluoride, chloride and sulfate
- Effects of climate change on groundwater resources at Shelter Island, New York State, USA
- Simulated impacts of artificial groundwater recharge and discharge on the source area and source volume of an Atlantic Coastal Plain stream, Delaware, USA
- Investigating pesticide transport in the León-Chinandega aquifer, Nicaragua
- Simultaneous parameter identification of a heterogeneous aquifer system using artificial neural networks
- A conceptual approach for assessing the impact of climate change on groundwater and related surface waters in cold regions (Finland)
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