Relevant bibliographies by topics / Hydrogeologie

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Hydrogeologie'

Author: Grafiati
Published: 4 June 2021
Last updated: 30 November 2024

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Journal articles on the topic "Hydrogeologie"

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Goldscheider, Nico. "Alpine Hydrogeologie." Grundwasser 16, no. 1 (January 13, 2011): 1. http://dx.doi.org/10.1007/s00767-010-0157-2.

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Schirmer, Mario. "Herausforderung Urbane Hydrogeologie." Grundwasser 12, no. 3 (July 6, 2007): 177. http://dx.doi.org/10.1007/s00767-007-0037-6.

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Holländer, Hartmut, and Ingo Bardenhagen. "Themenheft „Hydrogeologie der Festgesteine“." Grundwasser 27, no. 1 (January 20, 2022): 1–2. http://dx.doi.org/10.1007/s00767-022-00507-4.

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Birk, Steffen, and Thilo Hofmann. "Themenheft: Hydrogeologie in Österreich." Grundwasser 15, no. 1 (January 27, 2010): 3–4. http://dx.doi.org/10.1007/s00767-009-0138-5.

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Scheytt, Traugott. "50 Jahre Fachsektion Hydrogeologie." Grundwasser 24, no. 4 (September 16, 2019): 249. http://dx.doi.org/10.1007/s00767-019-00432-z.

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Sauter, Martin, Maria-Theresia Schafmeister, Stefan Peiffer, David Kuntz, Thomas Schiedek, and Thomas Himmelsbach. "Fracking – Die Rolle der Hydrogeologie." Grundwasser 18, no. 3 (July 12, 2013): 157–58. http://dx.doi.org/10.1007/s00767-013-0228-2.

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Wohnlich, Stefan. "Tracer als Werkzeug in der Hydrogeologie." Grundwasser 2, no. 2 (June 1, 1997): 59. http://dx.doi.org/10.1007/s767-1997-8520-9.

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Wohnlich, Stefan. "Grundwasserökologie—ein Fall für die Hydrogeologie?" Grundwasser 10, no. 3 (September 2005): 135. http://dx.doi.org/10.1007/s00767-005-0088-5.

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Grathwohl, Peter, Ronald Kozel, Hilmar Zetinigg, Rudolf Liedl, and Johannes Barth. "Hydrogeologie unter einem D-A-CH …" Grundwasser 15, no. 2 (April 28, 2010): 87. http://dx.doi.org/10.1007/s00767-010-0140-y.

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Rausch, Randolf, and Christoph Schüth. "Wenig ist mehr: Hydrogeologie arider Gebiete." Grundwasser 15, no. 4 (November 3, 2010): 219. http://dx.doi.org/10.1007/s00767-010-0155-4.

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Dissertations / Theses on the topic "Hydrogeologie"

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Regli, Christian. "Integration of geological and geophysical data of different quality into the stochastic description of aquifers /." Basel : [s.n.], 2003. http://edoc.unibas.ch/diss/DissB_6719.

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Matousek, Federico Matousek Federico Matousek Federico Matousek Federico. "Hydrogeologie und Hydrogeochemie des Waldenburger Tales (Baselbieter Jura) /." [Zürich] : [s.n.], 1985. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=7829.

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Finsterle, Stefan. "Inverse Modellierung zur Bestimmung hydrogeologischer Parameter eines Zweiphasensystems /." Zürich : Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie der ETH, 1993. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=9985.

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Al-Muqdadi, Sameh Wisam. "Groundwater investigation and modeling - western desert of Iraq." Doctoral thesis, Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2012. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-87476.

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The region of interest is part from Iraqi western desert covering an area about 100,000 km². Several of the large wadis such as Hauran, Amij, Ghadaf, Tubal and Ubaiydh traverse the entire region and discharge into the Euphrates River. The present study included the following hydrogeological investigations: Lineaments interpretation was done by using different data sets (SRTM 30 m and Landsat ETM 15m), within different algorithms. Some faults recognized by field survey match rather well with the automatically extracted lineaments with only a small difference between field data and re-mote sensed data. The groundwater flow directions (west to east) for three aquifers were determined by using different spatial interpolation algorithms. Due to the faults impact, the flow direction gets a slightly other direction when reaching the fault’s zone. Two pumping test were performed close to fault 2 in the unconfined aquifer Dammam using well no. 9 and 17. Results of pumping test and recovery were evaluated with the analytical model MLU for Windows. Well 17 shows a slightly higher transmissivity (0.1048 m²/min) in compari-son to well 9 (T= 0.0832 m²/min). This supports the assumption of a zone of unique elevated permeability between fault 1 and fault 2 because of the tectonic stress and the anticline structure. The catchment and watershed delineation was performed by means of four GIS packages utilizing three DTM´s: 90 m and 30 m SRTM (Shuttle Radar Topography Mission) and the ASTER 30 m. A thorough field survey and manual catchment delineation of the same area was available from Division 1944. Software used was Arc Hydrotools, TNTmips, River Tools and TecDEM. Ten 90 m SRTM and twelve 30 m ASTER files were merged by means of ArcGIS. The 30 m SRTM dataset of Iraq was supplied by courtesy of the US Army and the region of interest (ROI) was clipped from this DTM using ArcGIS. No additional steps were performed with both DTM data sets before using the mentioned software products to perform the catchment analysis. As a result the catchment calculations were significantly different for both 30 m and 90 m data and the different software products. The groundwater model implemented in Visual Modflow V.4.2 was built by 5 main layers repre-senting Dammam aquifer, first aquiclude, UmEr Duhmma aquifer, second aquiclude and the Tayarat aquifer. Averaged readings of groundwater head from 102 observation wells were used to calibrate the model. Calculated recharge average was 17.5 mm/year based on the water balance for ~30 years (1980-2008). A sensitivity analysis was performed by using different permeability and recharge values. However, the model showed a rather low sensitivity because the values of the standard error of the estimation were between 2.27 m and 3.56 m. Models with recharge less than 11.85 mm/year or more than 60 mm/year did not converge and thus failed to produce a result. Models with Kf values from 1.1-3 to 1.1-4 m/s for aquifers and from 1.1-7 to 1.1-8 m/s for aquicludes converged. Water budget is about 2.17*10¹⁰ m³/year; by irrigating the greenhouses this budget will cover only 1.75% of the total area. However, this value could be upgraded up to 8 – 9 % by utilizing the groundwater inflow from Saudi Arabia
Das Untersuchungsgebiet umfasst eine Fläche von etwa 100.000 km² und ist Teil der westlichen irakischen Wüste. Einige der großen Wadis wie Hauran, Amij, Ghadaf, Tubal und Ubaiydh durchqueren die gesamte Region und entwässern in den Euphrat. Die vorliegende Arbeit umfasst folgende hydrogeologische Untersuchungen: Die Interpretation der Lineamente wurde anhand verschiedener Datensätze (SRTM 30 m und Landsat ETM 15 m) und unter Nutzung unterschiedlicher Algorithmen durchgeführt. Einige Störungen, welche während Feldmessungen identifiziert wurden, stimmen gut mit automatisch extrahierten Lineamenten überein, der Unterschied zwischen Feld- und Fernerkundungsdaten ist somit gering. Die Ermittlung der Grundwasserfließrichtungen (von West nach Ost) der drei Aquifere erfolgte unter Nutzung verschiedener Algorithmen zur räumlichen Interpolation. Es zeigte sich, dass die Störungen zu einer leichten Veränderung der Fließrichtung mit zunehmender Nähe zur Störungszone führen. Zwei Pumpversuche in den Brunnen 9 und 17 wurden nahe der Störung 2 im ungesättigten Aquifer Dammam durchgeführt. Die Auswertung der Ergebnisse der Pump- und Wiederanstiegsversuche erfolgte mittels des analytischen Modells MLU für Windows. Es zeigte sich, dass Brunnen 17 eine leicht höhere Transmissivität aufweist (T = 0,1048 m²/min) im Vergleich zu Brunnen 9 (T = 0,0832 m²/min). Dies unterstützt die Annahme der Existenz einer Zone erhöhter Permeabilität zwischen den Störungen 1 und 2, verursacht durch tektonischen Stress und die Antiklinalstruktur. Die Erfassung von Einzugsgebiet und Wasserscheiden erfolgte anhand von vier GIS-Paketen unter Nutzung von 3 DTM’s: 90 m und 30 m SRTM (Shuttle Radar Topography Mission) sowie ASTER 30 m. Genaue Daten aus einer Feldkampagne und eine manuelle Abgrenzung des Einzugsgebietes derselben Region standen zur Verfügung (Division 1944). Als Software kamen Arc Hydrotools, TNTmips, River Tools und TecDEM zum Einsatz. Zehn SRTM- (90 m) und zwölf ASTER-Files (30 m) wurden mittels ArcGIS vereinigt. Ein 30 m SRTM-Datensatz des Irak (bereitgestellt durch die US-Armee) diente als Grundlage für das Ausschneiden des Untersuchungsgebietes (ROI) mit Hilfe von ArcGIS. An beiden DTM Datensätzen wurden vor der Ermittlung des Einzugsgebietes mit den genannten Software-Produkten keine zusätzlichen Schritte durchgeführt. Als Resultat ergaben sich signifikante Unterschiede zwischen den 30 m und 90 m Datensätzen sowie der verschiedenen Software. Das in Visual Modflow V.4.2 implementierte Grundwassermodell wurde aus fünf Hauptschichten bestehend aus Dammam Aquifer, erster Stauer, UmEr Duhmma Aquifer, zweiter Stauer und Tayarat Aquifer aufgebaut. Durchschnittliche Werte der Grundwasserstände aus 102 Observationsbrunnen dienten der Kalibrierung des Modells. Die berechnete mittlere Grundwasserneubildung betrug 17,5 mm/a, basierend auf dem Wasserhaushalt der letzten 30 Jahre (1980-2008). Unter Einbeziehung verschiedener Werte für Permeabilität und Grundwasserneubildung wurde eine Sensitivitätsanalyse durchgeführt. Dabei ergab sich allerdings eine geringe Empfindlichkeit des Modells, resultierend aus einer Standardabweichung der Schätzung zwischen 2,27 m und 3,56 m. Modelle mit einer Grundwasserneubildung kleiner 11,85 mm/a und größer 60 mm/a zeigten keine Konvergenz und führten somit zu keinem Ergebnis. Modelle mit kf Werten zwischen 1.1-3 und 1.1-4 m/s für Aquifere und zwischen 1.1-7 und 1.1-8 m/s für Grundwasserstauer konvergierten. Die Grundwasserneubildung betrug etwa 2,17∙10¹⁰ m³/a, für die Bewässerung von Gewächshäusern deckt diese Summe nur 1,75% des gesamten Gebietes ab. Allerdings könnte dieser Wert durch die Nutzung des Grundwasserzuflusses aus Saudi Arabien auf 8 – 9% gesteigert werden
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Hofmann, Beda Anton. "Genese, Alteration und rezentes Fliess-System der Uranlagerstätte Krunkelbach (Menzenschwand, Südschwarzwald) /." Baden : [s.n.], 1989. http://www.ub.unibe.ch/content/bibliotheken_sammlungen/sondersammlungen/dissen_bestellformular/index_ger.html.

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Mederer, Joachim. "Water Resources and Dynamics of the Troodos Igneous Aquifer-system, Cyprus - Balanced Groundwater Modelling -." Doctoral thesis, kostenfrei, 2009. http://www.opus-bayern.de/uni-wuerzburg/volltexte/2009/3730/.

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Baumann, Andrea R. "Geologie und Hydrogeologie des Embracher Tales und des unteren Tösstales (Kanton Zürich) /." Zürich, 1987. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=8357.

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Roth, Christoph. "Contribution de la geostatistique a la resolution du probleme inverse en hydrogeologie." Paris, ENMP, 1995. http://www.theses.fr/1995ENMP0527.

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L'objectif principal du travail concerne le developpement d'un modele geostatistique consacre a la resolution du probleme inverse en hydrogeologie: l'estimation de la transmissivite a l'aide des donnees de transmissivite et de charge hydraulique avec prise en compte des lois physiques regissant les ecoulements souterrains equation de l'ecoulement et conditions aux limites. C'est la prise en compte des conditions aux limites a distance finie et d'un terme de recharge qui elargit le domaine d'application par rapport aux modeles stochastiques anterieurs. Le modele geostatistique est fonde sur la resolution de l'equation de l'ecoulement linearisee. Les conditions aux limites sont prises en compte pour un champ rectangulaire dont deux limites sont impermeables et les deux autres a potentiel impose. Pour l'application a un cas reel, une transformation conforme permet de transformer le domaine naturel de l'aquifere en un rectangle tout en conservant les ecoulements
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LARUT, NIGON PASCALE. "Geologie et hydrogeologie du systeme karstique de la foux de mouans sartoux." Nice, 1991. http://www.theses.fr/1991NICE4452.

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Etude generale du bassin alimentant la foux de mouans sartoux (06) et ses bordures: 1) leve geologique au 1/5000; 2) analyse lithologique et structurale; 3) analyse des donnees hydrologiques du bassin et definition du reservoir a partir des indices karstiques, des tracages peripheriques, de la climatologie, de l'hydrometrie des cours d'eau et de l'exutoire, des pertes de vallons, aboutissant a la definition des unites de drainage; 4) bilan hydrogeologique
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Maréchal, Jean-Christophe. "Les circulations d'eau dans les massifs cristallins alpins et leurs relations avec les ouvrages souterrains /." Lausanne : Ecole polytechnique fédérale de Lausanne, 1998. http://library.epfl.ch/theses/?nr=1769.

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Books on the topic "Hydrogeologie"

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Hölting, Bernward, and Wilhelm G. Coldewey. Hydrogeologie. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-662-59667-8.

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Hölting, Bernward, and Wilhelm Georg Coldewey. Hydrogeologie. Heidelberg: Spektrum Akademischer Verlag, 2013. http://dx.doi.org/10.1007/978-3-8274-2354-2.

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Jordan, H. und H. J. Weder. Hydrogeologie. Leipzig: Grundstoffindustrie, 1987.

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Nonner, Johannes C. Introduction to hydrogeology. 2nd ed. Boca Raton, Fla: CRC Press, 2010.

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Schreiner, Matthias, and Klaus Kreysing. Geotechnik Hydrogeologie. Berlin, Heidelberg: Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/978-3-642-58851-8.

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Schreiner, Matthias. Geotechnik Hydrogeologie. Berlin: Springer, 1998.

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Hölting, Bernward. Hydrogeologie: Einführung in die allgemeine und angewandte Hydrogeologie. 6th ed. Müchen: Spektrum, 2005.

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Dieter, Richter. Ingenieur- und Hydrogeologie. Berlin: de Gruyter, 1989.

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Klaus, Münzing, ed. Hydrogeologie in Baden-Württemberg. Freiburg i. Br: Geologisches Landesamt Baden-Württemberg, 1985.

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Herčík, Ferdinand. Hydrogeologie české křídové pánve. Praha: Český geologický ústav, 1999.

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Book chapters on the topic "Hydrogeologie"

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Heitfeld, Karl-Heinrich, Lutz Krapp, and Torsten Böcke. "Hydrogeologie." In Die Mechernicher Triasbucht, 102–65. Wiesbaden: VS Verlag für Sozialwissenschaften, 1987. http://dx.doi.org/10.1007/978-3-322-88142-7_5.

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Henningsen, Dierk. "Hydrogeologie." In Geologie für Bauingenieure, 143–67. Berlin, Heidelberg: Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-642-56159-7_11.

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Henningsen, Dierk. "Hydrogeologie." In Geologie für Bauingenieure, 103–22. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-97377-2_9.

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Hölting, Bernward, and Wilhelm G. Coldewey. "Allgemeine Hydrogeologie." In Hydrogeologie, 7–238. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-662-59667-8_3.

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Hölting, Bernward, and Wilhelm G. Coldewey. "Angewandte Hydrogeologie." In Hydrogeologie, 239–389. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-662-59667-8_4.

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Hölting, Bernward, and Wilhelm Georg Coldewey. "Allgemeine Hydrogeologie." In Hydrogeologie, 7–238. Heidelberg: Spektrum Akademischer Verlag, 2013. http://dx.doi.org/10.1007/978-3-8274-2354-2_3.

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Hölting, Bernward, and Wilhelm Georg Coldewey. "Angewandte Hydrogeologie." In Hydrogeologie, 239–389. Heidelberg: Spektrum Akademischer Verlag, 2013. http://dx.doi.org/10.1007/978-3-8274-2354-2_4.

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Hölting, Bernward, and Wilhelm G. Coldewey. "Einleitung." In Hydrogeologie, 1–3. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-662-59667-8_1.

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Hölting, Bernward, and Wilhelm G. Coldewey. "Überblick über die Historie." In Hydrogeologie, 5–6. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-662-59667-8_2.

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Hölting, Bernward, and Wilhelm Georg Coldewey. "Einleitung." In Hydrogeologie, 1–3. Heidelberg: Spektrum Akademischer Verlag, 2013. http://dx.doi.org/10.1007/978-3-8274-2354-2_1.

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Conference papers on the topic "Hydrogeologie"

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Murdoch, Larry, Scott DeWolf, Leonid Germanovich, Soheil Roudini, and Robert Moak. "Recent Developments in Hydrogeologic Applications for Strain Tensor Analyses." In 31st Clemson Hydrogeology Symposium. US DOE, 2023. http://dx.doi.org/10.2172/2373046.

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Murdoch, Larry, Scott DeWolf, Rob Moak, and Leonid Germanovich. "Recent Developments in Hydrogeologic Applications for Strain Tensor Analyses." In 31st Clemson Hydrogeology Symposium, Clemson, South Carolina. US DOE, 2023. http://dx.doi.org/10.2172/2373030.

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Burkart, Michael. "HYDROGEOLOGY IN SUPPORT OF LITIGATION: INFLUENCING POLICY WITH HYDROGEOLOGY." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-312558.

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A. van Overmeeren, R. "Georadar for hydrogeology." In 55th EAEG Meeting. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609.201411534.

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López, Robin D., Mark Anthony Nawman, Mark Anthony Nawman, Sarah Elizabeth Heraldo, and Sarah Elizabeth Heraldo. "FLOWS IN HYDROGEOLOGY." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286666.

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Sykes, Jonathan F., Stefano D. Normani, Yong Yin, and Mark R. Jensen. "The Hydrogeologic Environment for a Proposed Deep Geologic Repository in Canada for Low and Intermediate Level Radioactive Waste." In ASME 2011 14th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2011. http://dx.doi.org/10.1115/icem2011-59285.

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A Deep Geologic Repository (DGR) for low and intermediate level radioactive waste has been proposed by Ontario Power Generation for the Bruce nuclear site in Ontario, Canada. As proposed the DGR would be constructed at a depth of about 680 m below ground surface within the argillaceous Ordovician limestone of the Cobourg Formation. This paper describes the hydrogeology of the DGR site developed through both site characterization studies and regional-scale numerical modelling analysis. The analysis provides a framework for the assembly and integration of the site-specific geoscientific data and examines the factors that influence the predicted long-term performance of the geosphere barrier. Flow system evolution was accomplished using both the density-dependent FRAC3DVS-OPG flow and transport model and the two-phase gas and water flow computational model TOUGH2-MP. In the geologic framework of the Province of Ontario, the DGR is located on the eastern flank of the Michigan Basin. Borehole logs covering Southern Ontario combined with site-specific data from 6 deep boreholes have been used to define the structural contours and hydrogeologic properties at the regional-scale of the modelled 31 sedimentary strata that may be partially present above the Precambrian crystalline basement rock. The regional-scale domain encompasses an approximately 18500km2 region extending from Lake Huron to Georgian Bay. The groundwater zone below the Devonian includes units containing stagnant water having high concentrations of total dissolved solids that can exceed 300g/L. The Ordovician sediments are significantly under-pressured. The horizontal hydraulic conductivity for the Cobourg limestone is estimated to be 2 × 10−14 m/s based on straddle-packer hydraulic tests. The low advective velocities in the Cobourg and other Ordovician units result in solute transport that is diffusion dominant with Peclet numbers less than 0.003 for a characteristic length of unity. Long-term simulations that consider future glaciation scenarios include the impact of ice thickness and permafrost. Solute transport in the Ordovician limestone and shale was diffusion dominant in all simulations. The Salina formations of the Upper Silurian prevented the deeper penetration of basal meltwater.
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Young, Charles T. "Estimating hydrogeologic parameters from radar data." In Ninth International Conference on Ground Penetrating Radar (GPR2002), edited by Steven Koppenjan and Hua Lee. SPIE, 2002. http://dx.doi.org/10.1117/12.462251.

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Groten, Joel, and E. Alexander. "Karst Hydrogeologic Investigation of Trout Brook." In National Cave and Karst Research Institute Symposium 5. University of South Florida Tampa Library, 2015. http://dx.doi.org/10.5038/9780991000951.1012.

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Kiss, J., L. Vertesy, G. Csillag, K. Gondar, and L. Koloszar. "Hydrogeology Supported by Geophysic." In 1st EEGS Meeting. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609.201407448.

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D. Knoll, Michael, and Rosemary Knight. "Mapping Hydrogeologic Properties Using Ground Penetrating Radar." In 6th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609-pdb.209.1993_050.

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Reports on the topic "Hydrogeologie"

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Edinberg, Sara C. Hydrogeologic framework of the upper Yellowstone River Valley, Park County, Montana. Montana Bureau of Mines and Geology, January 2024. http://dx.doi.org/10.59691/edpk6554.

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Gaughan, T. F. Burial Ground Expansion Hydrogeologic Characterization. Office of Scientific and Technical Information (OSTI), February 1999. http://dx.doi.org/10.2172/6169367.

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Gaughan, T. F. Burial Ground Expansion Hydrogeologic Characterization. Office of Scientific and Technical Information (OSTI), February 1999. http://dx.doi.org/10.2172/5300.

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Hanson, A. E. H., and M. Sutherland. Analyses of constant-rate aquifer tests in the Quaternary-Tertiary basin-fill sediments and the Tertiary-Archean fractured bedrock near Ennis, Montana. Montana Bureau of Mines and Geology, April 2024. http://dx.doi.org/10.59691/totj2778.

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Groundwater from Quaternary–Tertiary basin-fill sediments and from Tertiary–Archean fractured bedrock units is used to support residential development in the Madison Valley, near Ennis, Montana. To assess the range of transmissivities for the different hydrogeologic units, the Montana Bureau of Mines and Geology Ground Water Investigation Program conducted five constant-rate aquifer tests in three areas of development.
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5

Bledsoe, H. W. SRP Baseline Hydrogeologic Investigation, Phase 3. Office of Scientific and Technical Information (OSTI), August 1988. http://dx.doi.org/10.2172/10106333.

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6

Bledsoe, H. W. SRP baseline hydrogeologic investigation, Phase 2. Office of Scientific and Technical Information (OSTI), November 1987. http://dx.doi.org/10.2172/10135318.

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7

Flach, G. P., L. L. Hamm, M. K. Harris, P. A. Thayer, J. S. Haselow, and A. D. Smits. Characterizing hydrogeologic heterogeneity using lithologic data. Office of Scientific and Technical Information (OSTI), December 1995. http://dx.doi.org/10.2172/555397.

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8

Strom, R. N., and D. S. Kaback. SRP baseline hydrogeologic investigation: Aquifer characterization. Office of Scientific and Technical Information (OSTI), March 1992. http://dx.doi.org/10.2172/7064707.

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9

Flach, G., LL L. Hamm, M. K. Harris, P. A. Thayer, J. S. Haselow, and A. D. Smits. Characterizing hydrogeologic heterogeneity using lithologic data. Office of Scientific and Technical Information (OSTI), June 1997. http://dx.doi.org/10.2172/565245.

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Bledsoe, H. W., R. K. Aadland, and K. A. Sargent. SRS baseline hydrogeologic investigation: Summary report. Office of Scientific and Technical Information (OSTI), November 1990. http://dx.doi.org/10.2172/6655874.

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