Akademik Veri Yönetim Sistemi
SCIENCE OF THE TOTAL ENVIRONMENT, cilt.312, sa.1-3, ss.155-166, 2003 (SCI-Expanded)
This study covers the geochemical investigations on water and stream sediments to evaluate the influence from the abandoned Kalecik Hg mine. The groundwater samples (S5, S8, S9, WW10) are neutral, slightly alkaline waters which have pH values varying between 7.3 and 7.5. Electrical conductivity (EC) values of groundwaters for spring samples are low (250-300 VLS/cm). However, groundwater obtained from a deep well has a higher EC value of 950 muS/cm. Hg concentrations of groundwater samples vary between 0.01 and 0.13 mug/l. Hg concentrations of other water samples taken from mining area from surface waters and adits are between 0.10 and 0.99 mug/l. Adit water (A4) collected at the mine has the highest Hg content of 0.99 mug/1 and a pH of 4.4. Trace element concentrations of mine water samples show variable values. As is observed only in MW1 (310 mug/l). A4 was enriched in Cd, Co and Cr and exceed the Turkish drinking water standards (Turk Standartlan Enstitusu, 1997). Cu concentrations vary between 6.0 and 150 mug/l and are below the Turkish water standards. Mn concentrations in mine waters are between 0.02 and 4.9 mg/l. Only for sample A4 Mn value (4.9 mg/1) exceeds the standard level. Ni was enriched for all of the mine water samples and exceeds the safe standard level (20 mug/l) for drinking water. Of the major ions SO4 shows a notable increase in this group reaching 650 mg/1 that exceeds the drinking water standards. Stream sediment samples have abnormally high values for especially Hg and As, Sb, Ni, Cr metals. With the exception of sample Ss6 of which Hg concentration is 92 mg/kg, all the other samples have Hg contents of higher than 100 mg/kg. Pollution index values are significantly high and vary between 69 and 82 for stream sediment samples. (C) 2003 Elsevier Science B.V. All rights reserved.