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22 nd Salt Water Intrusion Meeting: Salt Water Intrusion in Aquifers: Challenges and PerspectivesFig. 6: Vulnerability of a freshwater lens to climate change and sea level rise (under W+ climate scenario): green meansthat concentration in top water system is so high that salt damage to crops is likely to occur. Upconing saline groundwaterfrom deeper parts of the system towards the surface water ditches can clearly be seen.6. COMMUNICATE AND COOPERATE WITH (LOCAL) STAKEHOLDERSPretty straightforward, but communication and cooperation with local stakeholders will make adifference! Site-specific knowledge such as on drainage and ditch characteristics, soil conditions andcrop production in the field can make a measure successful. When correctly instructed, they can evenhelp in data collection during monitoring campaigns.Fig. 7: Communication with stakeholders: their local knowledge and eagerness to adapt to a changing environment isessential to make measures for climate proof fresh water supply, suggested by hydrogeologists (photos by courtesy of VanBaaren, Rentmeester and Van der Hoek).278
22 nd Salt Water Intrusion Meeting: Salt Water Intrusion in Aquifers: Challenges and Perspectives7. COME UP WITH FEASIBLE, ROBUST AND FLEXIBLE STRATEGIESWe will work out three showcases (fig. 8) this coming year, of which two are worked out here:1. Infiltration via drainage, storage and recovery of freshwater in sandy creek ridges in a salineenvironment (ASR), utilizing the potential of the creek ridge for water storage, with the focus oninfiltration of surface water via drains.2. Optimizing the freshwater volume in shallow rainwater lenses by different types of (deep)drains.Fig. 8: Local (ground)water solutions to make Local Climate Proof Fresh Groundwater Supply possible.This coming year, we will use monitoring campaigns and modelling exercises to show the efficiencyof these measures.8. INTERNATIONAL POSSIBILITIESThe fresh water shortages problems we are detecting in the Netherlands are basically worldwideproblems. It is evident that with changing climate and global conditions, the stresses in the coastalzone are intensified. Fig. 9 show some possible regions with future problems. Various watermanagement strategies should be developed to cope with different circumstances.279
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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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New approaches onmodelling (general
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Ruben Caljé 1 ; Frans Schaars 1 ;
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Figure 2: The modeled interface dep
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Selected case studies
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CONCEPTUAL MODEL OF DAR ES SALAAM Q
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1. INTRODUCTION 2. HYDROGEOCHEMI
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1,61,41,210,80,60,40,20H-3 (TU)Luiz
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Saltwater intrusionsAquifer partly
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U4Quakenbrück212
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Understanding of salinewater hydrod
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