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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Groundwater flow. ; Electronic books.
    Description / Table of Contents: This volume provides a thorough overview of gravity-driven groundwater flow from one of the founding fathers of the field. Emphasizing groundwater flow as a fundamental geologic agent, the book examines the history, principles, scientific consequences and practical utilization, illustrated with diverse examples and supplemented by an extensive glossary.
    Type of Medium: Online Resource
    Pages: 1 online resource (311 pages)
    Edition: 1st ed.
    ISBN: 9780511532757
    DDC: 551.49
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Contents -- Preface -- 1 Introduction -- 1.1 The subject matter: definition, history, study methods -- 1.2 Portrayal of groundwater flow-systems -- 1.2.1 Darcy's experiment and Law -- 1.2.2 Fluid-dynamic parameters -- 1.2.2.1 Fluid potential, phi, and hydraulic head, h -- 1.2.2.2 Pore pressure vertical pressure-gradient and dynamic pressure-increment -- 1.2.3 The Laplace and diffusion equations -- 2 The `Unit Basin' -- 2.1 The basic flow pattern -- 2.2 Basic patterns of fluid-dynamic parameters -- 2.2.1 Pore pressure: p -- 2.2.2 Vertical pressure-gradient: dp/ dd=-dp/dz =y: pressure-vs.-depth or p(d)-profile -- 2.2.3 Dynamic pressure increment: Delta p -- 3 Flow patterns in composite and heterogeneous basins -- 3.1 Effects of basin geometry -- 3.1.1 Effect of water-table configuration -- 3.1.1.1 Effects of undulations of the water table -- 3.1.1.2 Effects of the regional slope and local relief of the water table -- 3.1.2 Effect of basin depth -- 3.1.3 Zijl's analysis of the scales of water-table relief, depths of flow-system penetration, and relation between spatial and temporal scales -- 3.1.4 Effects of major regional land-form types -- 3.2 Effects of basin geology -- 3.2.1 Effects of stratification -- 3.2.1.1 Two-layer cases -- 3.2.1.2 Three-layer cases. -- 3.2.1.3 Sloping beds outcropping at the land surface -- 3.2.2 Effects of lenses -- 3.2.2.1 Basin-scale effects of lenticular rock bodies -- 3.2.2.2 Lens-scale effects of lenticular rock bodies -- 3.2.3 Effects of faults -- 3.2.3.1 Barrier faults -- 3.2.3.2 Conduit faults -- 3.2.4 Effects of anisotropy -- 3.3 Effects of temporal changes in the water table: transient pore pressures and flow systems -- 3.3.1 Time lag and time scales in pore-pressure adjustment -- 3.3.2 Effect on basinal flow patterns. , 3.4 Hydraulic continuity: principle and concept -- 3.4.1 The concept of regional hydraulic continuity -- 3.4.1.1 Evolution of the concept -- 3.4.1.2 Additional arguments in support of regional hydraulic continuity -- 3.4.2 Consequences of regional hydraulic continuity -- 3.4.2.1 Regionally extensive groundwater flow systems -- 3.4.2.2 Systematic distribution of matter and heat: the geologic agency of groundwater -- 3.4.2.3 Hydraulic interdependence of different basinal regions and hydrologic components -- 3.4.3 Conclusions -- 4 Gravity flow of groundwater: a geologic agent -- 4.1 Introduction -- 4.2 The basic causes -- 4.2.1 In-situ interaction between groundwater and its environment -- 4.2.2 Flow: a mechanism of systematic transport and distribution -- 4.2.3 Ubiquity and simultaneity -- 4.3 The main processes -- 4.3.1 Chemical processes -- 4.3.2 Physical processes -- 4.3.3 Kinetic or transport processes -- 4.4 Manifestations -- 4.4.1 The hydrogeologic environment -- 4.4.2 Types of manifestations -- 4.4.2.1 Hydrology and hydraulics -- 4.4.2.2 Chemistry and mineralogy -- 4.4.2.3 Vegetation -- 4.4.2.4 Soil and rock mechanics -- 4.4.2.5 Geomorphology -- 4.4.2.6 Transport and accumulation -- 4.5 Summary -- 5 Practical applications: case studies and histories -- 5.1 Characterization and portrayal of regional hydrogeologic conditions -- 5.1.1 The hydrogeological reconnaissance maps of alberta, canada -- 5.1.2 The hydrogeological map of Australia (M=1:5000000) -- 5.1.3 `Hydrologic Investigations: Atlas HA-339', NW Minnesota -- USGS -- 5.1.4 Protection and restoration of wetland ecosystems based on groundwater flow-system analysis, the Netherlands -- 5.1.5 Environmental management of groundwater basins, Japan -- 5.2 Effects of recharge-discharge area characteristics on groundwater-related practical problems. , 5.2.1 Location and development of a municipal groundwater supply, Olds, Alberta, Canada -- 5.2.2 Underestimated rates for required dewatering, and land subsidence at lignite mine in discharge area, Neyveli, Tamil Nadu, India -- 5.2.3 Failure of a municipal sewage lagoon built on local recharge area, Brooks, Alberta, Canada -- 5.2.4 Deep penetration of contaminants in recharge areas and saltwater up-coning in discharge areas, central Netherlands -- 5.2.5 Transport of phosphorous by groundwater into Narrow Lake from near-shore recharge areas Alberta, Canada -- 5.2.6 Cause and reclamation of liquefied ground, Trochu, Alberta, Canada -- 5.2.7 Groundwater flow and heat-flow anomalies: assessing low-enthalpy geothermal potential, northern Switzerland -- 5.2.8 Increased susceptibility of slopes to failure in discharge areas: theoretical analysis -- 5.2.9 Analysis and mitigation of land-slide danger, Campo Vallemaggia, Switzerland -- 5.2.10 Groundwater flow systems and eco-hydrological conditions: study of the effects of land-use changes -- 5.3 Site-selection for repositories of high-level nuclear-fuel waste: examples for groundwater flow-system studies -- 5.3.1 Canada: the Recharge Area Concept (AECL: Atomic Energy ofCanada, Ltd) -- 5.3.2 Sweden: (Swedish Nuclear Fuel Supply Co/Division Kärn-Bränsle-Säkerhet: SKBF/KBS) -- 5.3.3 Switzerland: Nagra (Nationale Genossenschaft für die Lagerung radioaktiver Abfälle) -- 5.3.4 U.S.A: Palo Duro Basin, Texas -- 5.4 Interpretation and utilization of observed deviations from theoretical patterns of gravity-driven groundwater flow -- 5.4.1 Highly permeable rock pods -- 5.4.2 Hydraulic barriers to flow -- 5.4.3 Abrupt change in chemistry across flow-system boundary -- 5.4.4 Identifying mechanisms of subhydrostatic pore-pressure generation -- 5.5 Exploration for petroleum and metallic minerals. , 5.5.1 The hydraulic theory of petroleum migration and its application to exploration -- 5.6 Potential role of flow-system analysis in surface geochemical prospecting -- 5.6.1 Exploration for uranium deposits by groundwater flow-system analysis -- 5.6.2 Gravity-driven flow systems and strata-bound ore deposits -- 6 Gravitational systems of groundwater flow and the science of hydrogeology -- Glossary -- References -- Appendices -- A Appendix A -- A Appendix B -- Index.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK; Malden, USA : Blackwell Science Inc
    Ground water 43 (2005), S. 0 
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Ground water 40 (2002), S. 0 
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 187 (1960), S. 65-65 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Cells of T. corlissi, grown axenically on a tryptone (1 per cent) and yeast extract (0-05 per cent) broth, were washed twice in Prescott solution and kept during the experiments in the same solution. Fresh frozen sections of rat spleen served as food. The animals readily ingested the spleen cells. ...
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1432-2307
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Description / Table of Contents: Summary Cells of malignant melanoma isolated from the blood were studied by light and electron microscopy. Most of the cells were identifiable beyond any doubt by the presence of melanin and by their characteristic structure. All of the tumour cells isolated from the blood showed signs of damage of variable degree.
    Notes: Zusammenfassung Zellen maligner Melanome, die aus dem strömenden Blute isoliert wurden, konnten durch Melaninnachweis und elektronenmikroskopische Besonderheiten charakterisiert werden. Alle zeigten mehr oder weniger starke degenerative Veränderungen.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Virchows Archiv 374 (1977), S. 263-269 
    ISSN: 1432-2307
    Keywords: Myoepithel ; Mammary tumours ; Leiomyoma ; Myofilamentum
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary A leiomyoma-like, multifocal tumour developed from intraductal papillomatosis in the breast of a 42 year old woman. The spindle-shaped tumour cells were examined by light, electron and polarizing microscopy, which revealed that they originated from immature “precursor” myoepithelial cells. The author suggests that the tumour be called “myoepithelioma”. From the morphological characteristics of the tumour the myoepithelial cells appear to be capable of producing leiomyoma-like benign or malignant tumours. The role that has been attributed by some to the myoepithelial cell in the production of epithelial tumours is problematical, in the light of the present finding.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of pest science 49 (1976), S. 137-139 
    ISSN: 1612-4766
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Forest entomological problems in the Hungarian low land A view is given on the most important species of insect pests found in the forests of the Hungarian low land in 1975. These pests become constantly more dangerous because they were favoured by the founding of large monocultures of pines, black pines and poplars. In times to come more attention should be called to plant tree species suitable for the different localities.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Journal of pest science 45 (1972), S. 155-158 
    ISSN: 1612-4766
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Description / Table of Contents: Summary A total of 21 light-traps has been used for collecting Coleoptera-species in Hungaria forests since 11 years. Studies have been carried out on Population dynamics and Phenology ofMelolontha melolontha L. andSerica brunnea L. Some rare Coleoptera-species are reported.
    Notes: Zusammenfassung Seit 11 Jahren arbeitet in Ungarn ein zentralgeleitetes Lichtfallennetz. Die von den 21 Lichtfallen gefangenen Coleopteren-Arten sind vom Jahre 1969 an kontinuierlich bearbeitet. Es hat sich erwiesen, daß gradologische und phänologische Probleme mit Hilfe der Lichtfallen untersucht werden können. Als Beispiele werden die beiMelolontha melolontha L. undSerica brunnea L. gewonnenen Ergebnisse angeführt. Auch die Faunistik wird durch diese Methode bereichert.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Hydrogeology journal 4 (1996), S. 4-25 
    ISSN: 1435-0157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: RÉSUMÉ: Le concept de zone de recharge indique que, dans des environnements naturels du type du Bouclier canadien, les zones de recharge des systèmes aquifères régionaux sont préférables pour les stockages de déchets nucléaires à haut risque aux autres types de régimes d'écoulement souterrain, et particulièrement aux zones de décharge d'eau souterraine. Cette conclusion est tirée d'une analyse des modèles d'écoulements souterrains dans les bassins. Les calculs ont été réalisés pour la partie latérale en 2-D d'un bassin topographique complètement saturé, long de 20 km et profond de 4 km, dans lequel la nappe s'écoule sous l'effet de la gravité. Différentes distributions de la conductivité hydraulique ont été prises en considération: 1) homogène, 2) stratifiée, et 3) stratifiée avec failles. Le plongement des failles a été modifié par étapes depuis la verticale jusqu'à l'horizontale, pour différentes variantes. Dans son concept, le modèle est sensé représenter l'environnement des roches cristallines du Bouclier canadien. Le fonctionnement hydrogéologique d'hypothétiques sites de stockage souterrain à 500 m de profondeur dans les zones de recharge et de décharge ont été caractérisés par 13 paramètres. Les principaux avantages des zones de recharge par rapport aux zones de décharge sont 1) des axes d'écoulement et des temps de retour du lieu de stockage à la surface plus longs; 2) la robustesse des valeurs prédites pour les paramètres de fonctionnement; 3) la possibilité de vérifier sur le terrain les conditions hydrogéologiques favorables (ce qui revient à une validation implicite des valeurs minimales calculées des durées de retour des écoulements); 4) le choix d'un site sur la base des paramètres de contrôle de l'écoulement quantifiables et observables, et 5) une logistique simple et une coût favorable pour la sélection du site et son isolement. Parmi les conséquences de cette modélisation, on démontre que la présence d'eau ancienne n'est pas un indice d'absence d'écoulement.
    Abstract: RESUMEN: El Concepto de Área de Recarga consiste en que, en medios naturales de tipo similar al Escudo Canadiense, las áreas de recarga en sistemas regionales de flujo de aguas subterráneas son mejores para el almacenamiento de residuos nucleares de alta actividad que otras zonas, especialmente las áreas de descarga. A esta conclusión se ha llegado a partir de un análisis del flujo de agua subterránea en modelos de cuenca. Los cálculos se realizaron en una ladera bidimensional de una cuenca topográfica totalmente saturada, de 20 km de largo y 4 km de profundidad, bajo condiciones de flujo subterráneo gravífico. Se consideraron las siguientes variantes respecto a las distribuciones de conductividad hidráulica: 1) homogénea; 2) estratificada; y 3) estratificada-con fallas. La posición de las fallas se varió de manera escalonada desde vertical a horizontal para distintas variantes. Se considera que este modelo conceptual proporciona una buena representación del medio cristalino rocoso del Escudo Canadiense. El comportamiento hidrogeológico de hipotéticos almacenamientos situados a 500 m de profundidad en áreas de recarga y descarga se caracterizó mediante trece parámetros. Las principales ventajas de las áreas de recarga sobre las de descarga son: 1) mayores caminos recorridos y tiempos de llegada desde el almacenamiento a la superficie; 2) robustez de los valores predichos para los parámetros de comportamiento; 3) verificabilidad en campo de las condiciones hidrogeológicos favorables (equivalente a una validación implícita de los valores de tiempos de llegada mínimos calculados); 4) aceptación del emplazamiento basada en parámetros cuantificables y observables; y 5) logística simple y economía de selección des emplazamiento. Como un producto secundario de la modelación, se demuestra que la presencia de paleoagua no es necesariamente una indicación de estancamiento del agua.
    Notes: ABSTRACT: The Recharge Area Concept is the proposition that in Canadian-Shield type natural environments recharge areas of regional groundwater flow systems are superior for high-level nuclear waste repositories to other types of groundwater flow regimes, especially to areas of groundwater discharge. This conclusion is reached from an analysis of basinal groundwater flow models. The calculations were made for a two-dimensional flank of a fully saturated topographic basin, 20 km long and 4 km deep, in which groundwater is driven by gravity. Variants of hydraulic-conductivity distributions were considered: 1) homogeneous; 2) stratified; and 3) stratified-faulted. The faults' attitudes were changed by steps from vertical to horizontal for different variants. The model is assumed conceptually to represent the crystalline-rock environment of the Canadian Shield. The hydrogeologic performances of hypothetical repositories placed 500 m deep in the recharge and discharge areas were characterized by thirteen parameters. The principal advantages of recharge- over discharge-area locations are: 1) longer travel paths and return-flow times from repository to surface; 2) robustness of predicted values of performance parameters; 3) field-verifiability of favourable hydrogeologic conditions (amounting to an implicit validation of the calculated minimum values of return-flow times); 4) site acceptance based on quantifiable and observable flow-controlling parameters; and 5) simple logistics and favourable economics of site selection and screening. As a by-product of modeling, it is demonstrated that the presence of old water is not an indication of stagnancy.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Hydrogeology journal 8 (2000), S. 254-255 
    ISSN: 1435-0157
    Keywords: reviews ; crustal fluids ; heat and solute transport ; geologic processes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
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