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1987
Spring is a points of natural, concentrated discharge of groundwater at a rate high enough to maintain flow on the surface. Generally springs are formed where water table intersects with the earth’s surface, or groundwater rises to the surface through rock faults, fractures or depressions.
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Spring is a points of natural, concentrated discharge of groundwater at a rate high enough to maintain flow on the surface. Generally springs are formed where water table intersects with the earth’s surface, or groundwater rises to the surface through rock faults, fractures or depressions.
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Karst Terminology and Karst Types in China
1995Before discussing the main karst types in China, some aspects of Chinese karst terminology should be described. In geomorphology, Chinese geographers and hydrogeologists are more concerned with groupings of landforms than with the origins of individual forms.
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Karst spring catchment: an example from Dinaric karst
Environmental Earth Sciences, 2015Definition of karst spring catchment or basin area and boundaries belongs to one of the greatest problems of karst hydrology and hydrogeology, not adequately solved until now. This paper tries to address main problems in defining this crucial parameter. The theoretical aspect of this issue is discussed in the first two chapters.
Bonacci, Ognjen, Andrić, Ivo
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Sustainability of the karst environment - Dinaric karst and other karst regions
2010The objective of the international interdisciplinary scientific conference “Sustainability of the karst environment - Dinaric karst and other karst regions”, organized by Centre for Karst, Gospić, Croatia, was to give a theoretical and practical contribution to the concept of sustainable development in karst regions, with a special emphasis on the ...
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Karst and karst water recourses of Albania and their management
Carbonates and Evaporites, 2020Albania is situated in the western part of Balkan Peninsula, on the eastern coast of the Adriatic and the Ionian Sea, which is one of the most water−rich regions of the world. The karst landscape in Albania covers about 2750 km2 consisting of nearly 24% of the countries territory. Karstic aquifers are the richest in the country.
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6.4 Karst Geomorphology: Sulfur Karst Processes
2013Recognition and understanding of the important role of sulfur redox processes in developing karst has grown over the last 25 years with the discovery of remarkable sulfur-rich caves worldwide and advances in geomicrobiology. Recent work has shown that microbes interact with hydrocarbons, calcium sulfate bedrock, magmatic fluids, and sulfide ore ...
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Karst Hydrogeology and Chemical Characteristics of the Karst Water
1995Reference has been made several times in the discussions of the karst geomorphology to the springs and underground waters of the karst areas. This chapter gives a summary review of the karst hydrogeology and the characteristics of the karst waters, particularly in relation to the geomorphology.
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