Results 181 to 190 of about 7,708 (210)
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Hydrogeochemistry of Lake Gallocanta (Aragón, NE Spain)
Hydrobiologia, 1990Lake Gallocanta has undergone drastic changes during the last thirteen years. Water level changed from a high level (Zmax = 2 m) to total dryness in 1985. From 1986 to 1988 slow refilling occurred. The water volume fluctuations have been studied in relation to climatic variations recorded for that period.
F. A. Com�n +3 more
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Hydrogeochemistry of Roccamonfina volcano (Southern Italy)
Environmental Earth Sciences, 2009This is the first hydro-geochemical investigation carried out on the Roccamonfina Volcanic Complex groundwaters. The chemistry of Roccamonfina waters is defined by water–rock and water–rock–gas interactions. In fact, interactions between rocks of the first eruptive high-K formations and circulating groundwaters are recognized by high K concentrations ...
CUOCO E +3 more
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Hydrogeochemistry of the Chiang Mai Basin, northern Thailand
Journal of Asian Earth Sciences, 1997Abstract Chemical composition of groundwater samples collected from 247 boreholes throughout the Chiang Mai Basin was determined in order to describe the background ion concentrations and to identify the major hydrogeochemical processes that control the observed water chemistry.
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HYDROGEOCHEMISTRY OF GROUNDWATER IN CENTRAL ISRAEL
International Association of Scientific Hydrology. Bulletin, 1966ABSTRACT The regional groundwater groups of central Israel include: bicarbonate waters representing the replenishment areas; chloride waters representing the confined and the base-level zones; sulfate waters of the intermediate zones (fig. 2). These water types were found to fit broadly into five hydrogeographical groups.
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Geohydrology: Hydrogeochemistry
2021Janet S. Herman, Christopher A. Gellasch
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Hydrogeochemistry and origin of mineral waters
1997Many people regard mineral waters as something extraordinary but, in most cases, they (and here we include thermal waters) acquire their characteristic chemistry in the same way that any groundwater does. Much of the character of mineral water comes from the dissolution or leaching of components from minerals, but that is not the whole story, so let’ s
Marius Albu, David Banks, Harriet Nash
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Hydrogeochemistry – A Journey of Discovery
Understanding the origin of geogenic solutes (dissolved chemical elements unaffected by human activity) in groundwater has broader implications than a traditional water resource investigation. Humans evolved over millions of years drinking water from springs and seeps within a narrow range of solute compositions and concentrations as did nearly all ...openaire +1 more source