Application of zeolitic volcanic rocks for arsenic removal from water

Natural zeolitic rocks consisting mainly of chabazite-phillipsite, clinoptilolite, and volcanic glass have been evaluated by means of batch methods to remove arsenic from waters with different mineralization degree (from deionized water to natural water with a specific conductivity of 1,600 μS cm −...

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Published inEngineering geology Vol. 101; no. 3; pp. 245 - 250
Main Authors Ruggieri, F., Marín, V., Gimeno, D., Fernandez-Turiel, J.L., García-Valles, M., Gutierrez, L.
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier B.V 17.10.2008
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Abstract Natural zeolitic rocks consisting mainly of chabazite-phillipsite, clinoptilolite, and volcanic glass have been evaluated by means of batch methods to remove arsenic from waters with different mineralization degree (from deionized water to natural water with a specific conductivity of 1,600 μS cm − 1 ). Arsenic was previously spiked in the studied waters at concentrations of about 100 µg l − 1 to simulate actual cases. The compositional range of natural waters is representative of large hydrogeochemical regions around the world. The experiments were focussed on the application of natural common zeolitic rocks to water treatment for human consumption. The removal efficiency observed rises, in the better cases, 60–80% for chabazite-phillipsite raw materials whereas is 40–60% for clinoptilolite-bearing ones. The arsenic removal tends to increase with water mineralization degree, independently of the zeolitic rock type. A large zeolitic content in the chabazite-phillipsite raw materials increase the removal. Instead, the inverse situation is observed in the clinoptilolite-bearing rocks. The relevance of the quantitative mineralogical analysis, determining also the content of volcanic glass, as well as the use of natural waters in the removal tests has been demonstrated.
AbstractList Natural zeolitic rocks consisting mainly of chabazite-phillipsite, clinoptilolite, and volcanic glass have been evaluated by means of batch methods to remove arsenic from waters with different mineralization degree (from deionized water to natural water with a specific conductivity of 1,600 mu S cm super(-) super(1)). Arsenic was previously spiked in the studied waters at concentrations of about 100 approximately equal to g l super(-) super(1) to simulate actual cases. The compositional range of natural waters is representative of large hydrogeochemical regions around the world. The experiments were focussed on the application of natural common zeolitic rocks to water treatment for human consumption. The removal efficiency observed rises, in the better cases, 60-80% for chabazite-phillipsite raw materials whereas is 40-60% for clinoptilolite-bearing ones. The arsenic removal tends to increase with water mineralization degree, independently of the zeolitic rock type. A large zeolitic content in the chabazite-phillipsite raw materials increase the removal. Instead, the inverse situation is observed in the clinoptilolite-bearing rocks. The relevance of the quantitative mineralogical analysis, determining also the content of volcanic glass, as well as the use of natural waters in the removal tests has been demonstrated.
Natural zeolitic rocks consisting mainly of chabazite-phillipsite, clinoptilolite, and volcanic glass have been evaluated by means of batch methods to remove arsenic from waters with different mineralization degree (from deionized water to natural water with a specific conductivity of 1,600 μS cm − 1 ). Arsenic was previously spiked in the studied waters at concentrations of about 100 µg l − 1 to simulate actual cases. The compositional range of natural waters is representative of large hydrogeochemical regions around the world. The experiments were focussed on the application of natural common zeolitic rocks to water treatment for human consumption. The removal efficiency observed rises, in the better cases, 60–80% for chabazite-phillipsite raw materials whereas is 40–60% for clinoptilolite-bearing ones. The arsenic removal tends to increase with water mineralization degree, independently of the zeolitic rock type. A large zeolitic content in the chabazite-phillipsite raw materials increase the removal. Instead, the inverse situation is observed in the clinoptilolite-bearing rocks. The relevance of the quantitative mineralogical analysis, determining also the content of volcanic glass, as well as the use of natural waters in the removal tests has been demonstrated.
Author Gimeno, D.
García-Valles, M.
Gutierrez, L.
Ruggieri, F.
Fernandez-Turiel, J.L.
Marín, V.
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Issue 3
Keywords Sorption
Chabazite
Arsenic
Natural zeolites
Removal
scanning electron microscopy
volcanic rocks
igneous rocks
Surface analysis
arsenic
sorption
Experimental result
zeolite
water treatment
silicates
framework silicates
characterization
Comparative study
applications
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SSID ssj0013007
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Snippet Natural zeolitic rocks consisting mainly of chabazite-phillipsite, clinoptilolite, and volcanic glass have been evaluated by means of batch methods to remove...
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SubjectTerms Applied sciences
Arsenic
Buildings. Public works
Chabazite
Crystalline rocks
Earth sciences
Earth, ocean, space
Exact sciences and technology
Experimental petrology
Natural zeolites
Sorption
Water supply. Pipings. Water treatment
Title Application of zeolitic volcanic rocks for arsenic removal from water
URI https://dx.doi.org/10.1016/j.enggeo.2008.06.006
https://search.proquest.com/docview/19386666
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