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Storage Reservoirs and Deep Wells in Karst Regions Book

Storage Reservoirs and Deep Wells in Karst Regions
Storage Reservoirs and Deep Wells in Karst Regions, Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate, Storage Reservoirs and Deep Wells in Karst Regions has a rating of 3 stars
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Storage Reservoirs and Deep Wells in Karst Regions, Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate, Storage Reservoirs and Deep Wells in Karst Regions
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  • Storage Reservoirs and Deep Wells in Karst Regions
  • Written by author Marko Breznik
  • Published by Taylor & Francis, Inc., January 1998
  • Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate
  • Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate
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Preface
1Introduction1
2Name, Definition and Solubility of Rock Mass2
3Classification of Karst13
4Research for Storage Reservoirs18
5Geological and Hydrogeological Studies for Storage Reservoirs21
6Hydrological Research for Storage Reservoirs39
7Speleological Research for Water Storage45
8Geophysical Research - Electrical Methods48
9Geophysical Research - Variations in Density and Seismic Methods53
10Evaluation and Summary of Research Work for Storage Reservoirs58
11Sealing Storage Reservoirs in Karstified Valleys-Piezometric Surface of Karst Groundwaters at a Higher Level than a River59
12Sealing Karst Poljes - Piezometric Level of Karst Groundwater Lower than the Polje78
13Technical Structures for Sealing Reservoirs120
14Summary and Recommendations for Karst Storage Reservoirs161
15Exploration of Karst Groundwater165
16Position and Depth of Interception Structures170
17Drilling Techniques174
18Temporary and Safe Yields of Karst Groundwater178
19Deterioration of the Quality of Karst Water186
20Exploitation of Karst Groundwater in Coastal Areas189
21Desalination by the Isolation Method207
22Desalination by the Interception Method215
23The Artificial Rise-of-Spring-Level Method221
24Conclusions and Recommendations for Coastal Karst Groundwater234
Glossary237
References239


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Storage Reservoirs and Deep Wells in Karst Regions, Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate, Storage Reservoirs and Deep Wells in Karst Regions

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Storage Reservoirs and Deep Wells in Karst Regions, Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate, Storage Reservoirs and Deep Wells in Karst Regions

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Storage Reservoirs and Deep Wells in Karst Regions, Karst is a dry landscape situated on a soluble rock mass with an underground flow of water. Ten per cent of the world's landscape consists of karst. During rainy periods, karst valleys and poljes are flooded, whereas in dry periods there is a lack of wate, Storage Reservoirs and Deep Wells in Karst Regions

Storage Reservoirs and Deep Wells in Karst Regions

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