Toxic element contamination in waters from the massive sulfide deposits and wastes around Giresun, Turkey

This study assessed the quality of water polluted with mine drainage waters, some of which is used for drinking and agriculture, in the urban areas of the Giresun region, Turkey. A total of 40 water samples were collected from the main rivers and stream, spring, and drainage waters. All samples were analyzed for physical and chemical parameters. The tectonically controlled massive sulfide deposits hosted in the Maastrichtian-Eocene magmatic rocks are either active or have been abandoned. The main ore mineral assemblages are chalcopyrite, sphalerite, galena, and pyrite. The oxidation of the sulfide minerals in the deposits and wastes has caused acid mine drainage (AMD). Most of the spring, stream, and drainage waters have a strongly acidic pH and high sulfate content, and concentrations of Pb, Zn, Fe, and Cu can reach extremely high values. In addition to these elements, the concentrations of Cd, As, Mo, Se, Sb, Tl, and Bi are higher than the international and national drinking water guideline limits. Fe, Al, and Zn levels in stream, spring, and drainage waters are substantially higher than those in the rivers. The risk index values of hazardous elements in the river water show no or low risk, while most of the stream, spring, and drainage waters show high and/or extremely high risk values. The concentrations of the metals and pollution levels of most of the stream, spring, and drainage waters may pose great environmental risks through the changes they cause and disturbances brought to the living things in the area.

Toxic element contamination in waters from the massive sulfide deposits and wastes around Giresun, Turkey

This study assessed the quality of water polluted with mine drainage waters, some of which is used for drinking and agriculture, in the urban areas of the Giresun region, Turkey. A total of 40 water samples were collected from the main rivers and stream, spring, and drainage waters. All samples were analyzed for physical and chemical parameters. The tectonically controlled massive sulfide deposits hosted in the Maastrichtian-Eocene magmatic rocks are either active or have been abandoned. The main ore mineral assemblages are chalcopyrite, sphalerite, galena, and pyrite. The oxidation of the sulfide minerals in the deposits and wastes has caused acid mine drainage (AMD). Most of the spring, stream, and drainage waters have a strongly acidic pH and high sulfate content, and concentrations of Pb, Zn, Fe, and Cu can reach extremely high values. In addition to these elements, the concentrations of Cd, As, Mo, Se, Sb, Tl, and Bi are higher than the international and national drinking water guideline limits. Fe, Al, and Zn levels in stream, spring, and drainage waters are substantially higher than those in the rivers. The risk index values of hazardous elements in the river water show no or low risk, while most of the stream, spring, and drainage waters show high and/or extremely high risk values. The concentrations of the metals and pollution levels of most of the stream, spring, and drainage waters may pose great environmental risks through the changes they cause and disturbances brought to the living things in the area.

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Turkish Journal of Earth Sciences-Cover
  • ISSN: 1300-0985
  • Yayın Aralığı: Yılda 6 Sayı
  • Yayıncı: TÜBİTAK
Sayıdaki Diğer Makaleler

Reservoir characterization of the Burqan Formation sandstone from Midyan Basin, northwestern Saudi Arabia

Abdulaziz AL-LABOUN, Abdurrahman AL-QURAISHI, Haider ZAMAN, Mohammed BENAAFI

Toxic element contamination in waters from the massive sulfide deposits and wastes around Giresun, Turkey

Necati KARAKAYA, Muazzez ÇELİK KARAKAYA

Development of a numerical 2-dimensional beach evolution model

Cüneyt BAYKAL

Chemistry of magmatic and alteration minerals in the Chahfruzeh porphyry copper deposit, south Iran: implications for the evolution of the magmas and physicochemical conditions of the ore fuids

Morteza EINALI, Saeed ALIREZAEI, Federica ZACCARINI

Comparative geochemical study of soils developed on characteristic black and yellowpolymetallic massive sulfde deposits in Eastern Pontides (NE Turkey)

Nezihi KÖPRÜBAŞI, Cafer ÖZKUL, Necla KÖPRÜBAŞI, Sait CORDAN, Fatma TÜKEL ŞİŞMAN, Emin ÇİFTÇİ

Chemistry of magmatic and alteration minerals in the Chahfiruzeh porphyry copper deposit, south Iran: implications for the evolution of the magmas and physicochemical conditions of the ore fluids

Morteza EINALI, Saeed ALIREZAEI, Federica ZACCARINI

Terebella lapilloides Münster, 1833 from the Upper Jurassic-Lower Cretaceous İnaltı carbonates, northern Turkey: its taxonomic position and paleoenvironmental-paleoecological significance

Mustafa Yücel KAYA, Demir ALTINER

Terebella lapilloides Münster, 1833 from the Upper Jurassic Lower Cretaceous İnaltı carbonates, northern Turkey: its taxonomic position and paleoenvironmental-paleoecological signifcance

Demir ALTINER, Mustafa Yücel KAYA

Santonian-Campanian biostratigraphy of the Kalaat Senan area (West-Central Tunisia)

Zaineb ELAMRI, Dalila ZAGHBIB-TURKI

Comparative geochemical study of soils developed on characteristic black and yellow polymetallic massive sulfide deposits in Eastern Pontides (NE Turkey)

Nezihi KÖPRÜBAŞI, Emin ÇİFTÇİ, Sait CORDAN, Necla KÖPRÜBAŞI, Cafer ÖZKUL, Fatma Şişman TÜKEL