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Evangelos P Tziritis
National and Kapodistrian University of Athens
Faculty of Geology & Geoenvironment
Department of Economic Geology and Geochemistry

e-mail: evtziritis@geol.uoa.gr
tel: +030 210-7274103
mob: +030 6974-016686
evtziritis@geol.uoa.gr
Evangellos Tziritis is a Geologist, with an expertise in the fields of Geochemistry, Environmental and Applied Geochemistry, Water Resoucres Managment, Hydrogeology and Geoinformatics. He entered in 1998 in the Faculty of Geology of the National and Kapodistrian University of Athens and graduated in 2002 with the grade of 7,7/10. In 2004 he finished his postgraduate studies (M.Sc.) in the field of "Environment and Development" in the intredisciplinary postgraduate programm of the National Technical Univeristy of Athens, with the grade of 8,5/10. In 2004 he granted a scholarship from the National Greek Foundation of Scholarships in the field of Environmental Geochemistry for PhD research. He finished his PhD thesis in 2008 with grade 10/10 (excellent) in the Faculty of Geology and Geoenvironment of the National and Kapodistrian University of Athens.

Since 2002 he has participated as major researcher in various applied and research programms (national and intrnational). Since 2008 he has been an external partner (researcher, project manager / project leader) of ECHMES Ltd. Environmental Consultants, while since 2009 he is research and teaching staff in the Department of Economic Geology and Geochemistry of the Geological and Geoenvironmental Faculty of the National and Kapodistrian University of Athens, in the subjects of Geochemistry, Environmental Geochemistry and Industrial Minerals

Journal articles

2009
 
DOI 
Evangelos P Tziritis (2009)  Groundwater and soil geochemistry of the Eastern Kopaida region (Beotia, central Greece)   Central European Journal of Geosciences 1: 2. 219-226  
Abstract: The Kopaida plain is a cultivated region of Eastern Greece, with specific characteristics related to the paleogeographic evolution and the changes in land use of the area. This study examines the geochemical conditions of the groundwater and soil, and the correlations between them. 70 samples (50 samples of groundwater and 20 samples of soil) were collected in order to asses the geochemical status and the major natural and manmade affecting processes in the region. Extended chemical analyses were carried out including the assessment of 28 parameters for groundwater and 13 for soil samples. The results revealed that groundwater geochemistry is influenced primary by natural processes such as the geological background, and secondary by manmade impact mainly deriving from the extended use of Nitrogen-fertilizers and the over-exploitation of boreholes. Soil geochemistry is influenced exclusively by natural processes, such as weathering of the prevailing geological formations. Chemical analyses and the statistical processing of data revealed that the major factor for the geochemical status of soils is the weathering of the karstic substrate, as well as the existing lateritic horizons and a weak sulfide mineralization.
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DOI 
Michael G Stamatakis, Evangelos P Tziritis, Niki Evelpidou (2009)  The geochemistry of Boron rich groundwater of the Karlovassi Basin, Samos Island, Greece   Central European Journal of Geosciences 1: 2. 207-218  
Abstract: The upper Miocene of Karlovassi Basin, Samos Island, Greece, contain continental evaporites such as colemanite, ulexite, celestite, gypsum and thenardite. These evaporites are related with volcanic tuffs, diagenetically altered in a saline-alkaline lake environment. The aim of the present paper is to: a) define the impact of the already known and possible buried borates and other evaporites to the geochemistry of the hydrogeological system of Karlovassi Basin, and; b) to assess the correlation between surface and underground evaporite deposits considering the spatial changes in the concentrations of the examined physicochemical parameters. Fieldwork, laboratory measurements and literature data revealed elevated boron values (2136-33012 μg/L) in the central part of Karlovassi Basin. In the same area, high amounts of strontium, sodium, lithium and sulfates also occur. It is proposed that these ions originate from the leaching of evaporites and authigenic minerals such as the Sr-rich clinoptilolite and the boron-bearing potassium feldspar. Boron values are abnormally high for freshwater aquifers, and are indicative of the presence of buried evaporites in the basin with unknown significance.
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DOI 
Akindynos Kelepertzis, Evangelos Tziritis, Eustratios Kelepertzis, Giorgos Leontakianakos, Kostas Pallas (2009)  Hydrogeochemical characteristics and genetic implications of Edipsos thermal springs, north Euboea, Greece   Central European Journal of Geosciences 1: 3. 241-250  
Abstract: Edipsos area, situated in northern Euboea, has been well known since ancient times for the existence of thermal springs. In order to assess the hydrogeochemical conditions, thermal and cold water samples were collected and analyzed by ICP method for major and trace elements. The results revealed the direct impact of seawater, a process which is strongly related to the major tectonic structures of the area. Seawater impact was confirmed by the Cl/Br and Na/Cl ionic ratios, as well as from statistical processing and graphical interpretation of the analytical results, which classified the sampled waters into three groups (two for cold waters and one for the thermal ones). Trace element ranges for thermal waters are: As (44-84 ppb), Pb (23-154 ppb), Ag (1-2 ppb), Mn (31-680 ppb), Cu (61-97 ppb), Cs (66-244 ppb), Se (0-76 ppb), Li (732-3269 ppb), Fe (0-1126 ppb), Sr (14000-34100 ppb), B (4300-9600 ppb). Compared with the chemical composition of other thermal springs from the Hellenic Volcanic Arc, Edipsos thermal waters are enriched in Ca2+, Na+, Cl−, SO42−, Li, B and K+, reflecting the influence from seawater. Cold waters are free of heavy metals compared with other natural waters and are characterized by good quality based on the major element chemistry. Finally, several geothermometers were applied in order to assess the reservoir temperatures, but none of them appear to be applicable, mainly due to the impact of seawater on the initial hydrogeochemistry of the geothermal fluids.
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2008

Book chapters

2009
2008

Conference papers

2008
2007
2005

Booklets

2008

Masters theses

2004

PhD theses

2008
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