Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand

The presence of Cr(VI) in groundwater resources is governed by pH and Eh of water and its compounds are generally soluble and have more toxicicity and mobility in oxidizing environments. In this article, the Cr concentration in ophiolite units, in sediments, and in groundwater resources, and also it...

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Main Authors: Zahra Khaledi, Hossein Mohammadzadeh
Format: Article
Language:fas
Published: Ferdowsi University of Mashhad 2012-10-01
Series:Journal of Economic Geology
Subjects:
Online Access:http://econg.um.ac.ir/index.php/econg/article/view/16500
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author Zahra Khaledi
Hossein Mohammadzadeh
author_facet Zahra Khaledi
Hossein Mohammadzadeh
author_sort Zahra Khaledi
collection DOAJ
description The presence of Cr(VI) in groundwater resources is governed by pH and Eh of water and its compounds are generally soluble and have more toxicicity and mobility in oxidizing environments. In this article, the Cr concentration in ophiolite units, in sediments, and in groundwater resources, and also its potential to contaminate the environment have been investigated in southeast of Birjand. During sampling, 17 water samples (2 rain water samples and 15 groundwater samples), and 8 sediment samples were collected. The concentrations of cations (major cations and Cr) and anions in water samples were measured at Ottawa University, Canada using IC and ICP-AES methods, respectively. Cr concentrations of sediments were measured using XRF, and concentrations of Cr in collected Selective Sequential Extraction (SSE) fractions were measured using Atomic Absorption (AA) at Ferdowsi University of Mashhad, Iran. The average Cr concentrations in sediments and water resources are 627 and 0.026 ppm, respectively. According to the pH of sediments and Eh-pH of water samples, the Cr in water resources is as Cr(VI). Furthermore, the results of SSE show that the majority of Cr was found with residual matter, attached to the iron and manganese oxides, bound to carbonates, organic matter, and the soluble fractions, respectively. The hydrogeochemical properties of water resources show that the average values of EC, TDS and pH are 509 mg/l, 1045 µs/cm and 8.1, respectively, and the concentrations of Cl-, Na+, Mg2+ and SO42- ions are higher than the levels of WHO and Iran National Standard (1053). According to the WQI classification, while 20 percent of the water resources have excellent quality, 53 percent show good quality and 20 percent of water resources are poor in quality.
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spelling doaj.art-0588b21b7201443cad226c3c9cd072722022-12-22T00:10:42ZfasFerdowsi University of MashhadJournal of Economic Geology2008-73062012-10-0142335350Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of BirjandZahra Khaledi0Hossein Mohammadzadeh1Department of Earth Sciences, Ferdowsi University of Mashhad, Mashhad, IranGroundwater Research Center, Ferdowsi University of Mashhad, Mashhad, IranThe presence of Cr(VI) in groundwater resources is governed by pH and Eh of water and its compounds are generally soluble and have more toxicicity and mobility in oxidizing environments. In this article, the Cr concentration in ophiolite units, in sediments, and in groundwater resources, and also its potential to contaminate the environment have been investigated in southeast of Birjand. During sampling, 17 water samples (2 rain water samples and 15 groundwater samples), and 8 sediment samples were collected. The concentrations of cations (major cations and Cr) and anions in water samples were measured at Ottawa University, Canada using IC and ICP-AES methods, respectively. Cr concentrations of sediments were measured using XRF, and concentrations of Cr in collected Selective Sequential Extraction (SSE) fractions were measured using Atomic Absorption (AA) at Ferdowsi University of Mashhad, Iran. The average Cr concentrations in sediments and water resources are 627 and 0.026 ppm, respectively. According to the pH of sediments and Eh-pH of water samples, the Cr in water resources is as Cr(VI). Furthermore, the results of SSE show that the majority of Cr was found with residual matter, attached to the iron and manganese oxides, bound to carbonates, organic matter, and the soluble fractions, respectively. The hydrogeochemical properties of water resources show that the average values of EC, TDS and pH are 509 mg/l, 1045 µs/cm and 8.1, respectively, and the concentrations of Cl-, Na+, Mg2+ and SO42- ions are higher than the levels of WHO and Iran National Standard (1053). According to the WQI classification, while 20 percent of the water resources have excellent quality, 53 percent show good quality and 20 percent of water resources are poor in quality.http://econg.um.ac.ir/index.php/econg/article/view/16500OphioliteCr concentrationsedimentSSEmobility factorgroundwaterWQIBirjand
spellingShingle Zahra Khaledi
Hossein Mohammadzadeh
Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand
Journal of Economic Geology
Ophiolite
Cr concentration
sediment
SSE
mobility factor
groundwater
WQI
Birjand
title Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand
title_full Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand
title_fullStr Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand
title_full_unstemmed Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand
title_short Evaluation of Cr in ophiolite and groundwater and its potential to contaminate the environment in SE of Birjand
title_sort evaluation of cr in ophiolite and groundwater and its potential to contaminate the environment in se of birjand
topic Ophiolite
Cr concentration
sediment
SSE
mobility factor
groundwater
WQI
Birjand
url http://econg.um.ac.ir/index.php/econg/article/view/16500
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