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Saltwater intrusionsAquifer partly or completely saltyOnly lower part of aquifer saltyInland salinization(saltdome leaching and rising of water)borderline pretertiary solid rock (to thesouth) and Tertiary or Quarternaryunconsolidated rock (to the north)Near surface saltdomeDenmarkHamburg(LowerSaxony)QuakenbrückHannover 210
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SWIM22 - 22 nd Salt Water Intrusion
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Local Supporting Organizing TeamMar
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Peter StuyfzandKiwa Water Research,
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PrefaceWelcome to the 22 nd Salt Wa
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SUMMARYKeynote Lectures pg 13Coasta
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Groundwater hypersalinization in a
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Hydrostratigraphic Study of Itaipua
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Keynote Lectures
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22 nd Salt Water Intrusion Meeting:
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Effects of sea levelrise and climat
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Hans Sulzbacher 1 ; Helga Wiederhol
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Resistivity [Ωm]0.1 1 10 100 10000
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2. METHODS Figure 1a.
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4. DISCUSSION AND CONCLUSIONSREFERE
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METHODS 51
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DISCUSSION AND CONCLUSIONS
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2. RESULTS, HOW TO GET THERE AND WH
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STUDY OF THE SALTWATER-FRESHWATER I
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4. DISCUSSION5. CONCLUSIONS67
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Hydrogeochemical and isotopicmethod
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Figure 1 Location map of study area
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Therefore, it was clarified that th
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GROUNDWATER HYPERSALINIZATION IN A
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3. RESULTS AND DISCUSSIONS
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GROUNDWATER ARTIFICIAL RECHARGE IN
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2. GEOLOGICAL SETTING 3. H
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1. INTRODUCTION 2. MATERIALS AND ME
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4. CONCLUSIONS
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Page 165 and 166: 22 nd Salt Water Intrusion Meeting:
Page 173: New approaches onmodelling (general
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Page 199: Selected case studies
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Page 240 and 241: ACKNOWLEDGEMENTREFERENCES234
Page 260 and 261: 1. INTRODUCTION2. EXAMPLE: UPCONING
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Figure 1. Computed density and mole
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Depth (m)22 nd Salt Water Intrusion
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