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2009
DOI: 10.1016/j.jhazmat.2008.12.124
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Adsorption of sulfur dioxide on natural clinoptilolite chemically modified with salt solutions

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Cited by 31 publications
(20 citation statements)
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References 37 publications
(71 reference statements)
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“…It was found that the adsorption capacity of SO 2 depended on the cation electronegativity and ionic potential. This is in agreement with previous papers (Sirkecioglu et al 1995;Ivanova and Koumanova 2009). A similar order for SO 2 adsorption was determined for cationic forms of Turkey clinoptilolite: H + > Na + > K + > Ca 2+ (Sirkecioglu et al 1995).…”
Section: Adsorptionsupporting
confidence: 92%
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“…It was found that the adsorption capacity of SO 2 depended on the cation electronegativity and ionic potential. This is in agreement with previous papers (Sirkecioglu et al 1995;Ivanova and Koumanova 2009). A similar order for SO 2 adsorption was determined for cationic forms of Turkey clinoptilolite: H + > Na + > K + > Ca 2+ (Sirkecioglu et al 1995).…”
Section: Adsorptionsupporting
confidence: 92%
“…A similar order for SO 2 adsorption was determined for cationic forms of Turkey clinoptilolite: H + > Na + > K + > Ca 2+ (Sirkecioglu et al 1995). Ivanova and Koumanova (2009) found that the adsorption capacity of the Na-form of natural clinoptilolite from Bulgaria was the highest. Capacity of clinoptilolites for SO 2 ranged from 2.083 mmol/g to 2.967 mmol/g in this study (Table 2).…”
Section: Adsorptionsupporting
confidence: 65%
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“…Among zeolites, clinoptilolite is the most common natural zeolite with a low Si/Al ratio, and large intersecting open channels of 8-and 10-member tetrahedral rings [20,21]. Its low cost and unique structure help clinoptilolite to be utilized as a cation exchange in adsorption of ammonia and heavy metals from waste waters and adsorption/ desorption of gases in gas treatment processes [22][23][24][25][26]. Furthermore, zeolite properties contribute to an extended field of catalytic processes [27,28].…”
Section: Introductionmentioning
confidence: 99%
“…It is well known that natural zeolites consist of aluminia and silica tetrahedra which, bound in a definite way, include crystal structure vacancies, channels and pores [1,2] . About 40 natural zeolites have been identified during the past 200 years; the most widespread are analcime, chabazite, clinoptilolite, erionite, ferrierite, heulandite, laumontite, mordenite, and phillipsite.…”
Section: Introductionmentioning
confidence: 99%