| heal.abstract |
The area of north Evia and eastern central Greece is characterized by strong geomorphological contrast and is built up mainly of consolidated rocks. Unconsolidated young sediments of Pleistocene to Holocene age cover the valley and basin flats, forming the most productive aquifers in this area. However, two more types of aquifers can be distinguished within the consolidated rock area. The first one is associated with karstified limestones and the second with strongly tectonized ultramatic rocks. The schist-chert formation, with intercalations of shales and cherts, seals the ultramafic masses underneath. Surface and spring waters associated with ultramafic rocks in north Evia and eastern central Greece were studied. Two types of water can be distinguished: (1) high Mg2+ and SiO2, bicarbonate as the dominant anion, pH 7.4-9.2, temperature 9.5-16.3°C, low TDS (total dissolved solutes) (459-1037 mg 1), found both in peridotite and serpentinite areas, classified as Mg-HCO3 type; (2) high Ca2+, low Mg2+ and SiO2, hydroxyl ion as the major anion, pH 11.2, temperature 28°C, very low TDS (122 mg/l), found in peridotite areas, classified as Ca-OH type. The studied waters are highly supersaturated with respect to quartz, amorphous silica, brucite and most low temperature magnesium silicates (antigorite, sepiolite, talc, etc.). These waters show relatively narrow SiO2 concentration ranges and a trend parallel to the amorphous silica saturation surface. The silica supersaturated waters have the potential to precipitate silica and consequently could affect the people of the local communities that use it as drinking water, causing health problems (kidney stones).The area of north Evia and eastern central Greece is characterized by strong geomorphological contrast and is built up mainly of consolidated rocks. Unconsolidated young sediments of Pleistocene to Holocene age cover the valley and basin flats, forming the most productive aquifers in this area. However, two more types of aquifers can be distinguished within the consolidated rock area. The first one is associated with karstified limestones and the second with strongly tectonized ultramafic rocks. The schist-chert formation, with intercalations of shales and cherts, seals the ultramafic masses underneath. Surface and spring waters associated with ultramafic rocks in north Evia and eastern central Greece were studied. Two types of water can be distinguished: (1) high Mg2+ and SiO2, bicarbonate as the dominant anion, pH 7.4-9.2, temperature 9.5-16.3 °C, low TDS (total dissolved solutes) (459-1037 mg/l), found both in peridotite and serpentinite areas, classified as Mg-HCO3 type; (2) high Ca2+, low Mg2+ and SiO2, hydroxyl ion as the major anion, pH 11.2, temperature 28 °C, very low TDS (122 mg/l), found in peridotite areas, classified as Ca-OH type. The studied waters are highly supersaturated with respect to quartz, amorphous silica, brucite and most low temperature magnesium silicates (antigorite, sepiolite, talc, etc.). These waters show relatively narrow SiO2 concentration ranges and a trend parallel to the amorphous silica saturation surface. The silica supersaturated waters have the potential to precipitate silica and consequently could affect the people of the local communities that use it as drinking water, causing health problems (kidney stones). |
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