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Titlebook: H2Karst Research in Limestone Hydrogeology; Jacques Mudry,François Zwahlen,James W. LaMoreaux Book 2014 The Editor(s) (if applicable) and

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发表于 2025-3-21 19:36:01 | 显示全部楼层 |阅读模式
书目名称H2Karst Research in Limestone Hydrogeology
编辑Jacques Mudry,François Zwahlen,James W. LaMoreaux
视频video
概述Provides a broad overview about groundwater mechanisms in karst aquifers.Covers case studies of karst hydrogeology worldwide.Explains new investigation techniques to protect groundwater resources.Incl
丛书名称Environmental Earth Sciences
图书封面Titlebook: H2Karst Research in Limestone Hydrogeology;  Jacques Mudry,François Zwahlen,James W. LaMoreaux Book 2014 The Editor(s) (if applicable) and
描述Chapters in this book are contributions from the 9th Conference on limestone hydrogeology, organized in Besançon in September 2011 selected by the scientific committee of H2Karst.The book presents latest results on in the field of groundwater flow and storage within the different subsystems of karst aquifers; insights into the complex interaction between groundwater and surface water in karst areas by a multidisciplinary approach; current knowledge on contamination problems and contaminant transport in karst aquifers as well as an overview of karst hydrogeology in different contexts around the world.
出版日期Book 2014
关键词Groundwater Flow; H2Karst; Hydrogeology; Karst Aquifer
版次1
doihttps://doi.org/10.1007/978-3-319-06139-9
isbn_softcover978-3-319-35513-9
isbn_ebook978-3-319-06139-9Series ISSN 2199-9155 Series E-ISSN 2199-9163
issn_series 2199-9155
copyrightThe Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl
The information of publication is updating

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发表于 2025-3-21 21:16:42 | 显示全部楼层
Hydraulic Properties of Karst Groundwater and Its Impacts on Large Structures,he hydraulic properties and specific regime of groundwater in karst are, in many cases, the source of catastrophic failures. The most common destructive influence of groundwater is the consequence of: massive turbulent flows; the fast erosion of unconsolidated deposits in caverns and joints; the gre
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Contribution of Isotopes of the Water Molecule to Determine Recharge Altitude of the Main Springs Wthe recharge altitudes of major springs issuing from the Liassic dolomitic limestone, and helping to delineate protection zones of the springs. Chemical analyses of spring water show a composition that reflects both reservoir lithology and chemical evolution over the flow transit through the reservo
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Distributed Hydrological Modeling and Model Adaption in High Alpine Karst at Regional Scale (Bercht to unknown storage quantities. Missing parameterization in karst catchments at regional scale prevents reliable hydrological modeling of subsurface (unsaturated and saturated) water fluxes; and consequently, climate impact modeling in karst dominated catchments is until today insufficient. The dete
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Diagnostic Plots Applied to Well-Tests in Karst Systems,can be solved by assimilating the horizontal karst conduit to a finite-conductivity vertical fracture. In this case, several flow patterns corresponding to the respective contributions of karst subsystems (fractured matrix, small conduits and main karst drainage network) can be identified on the dia
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