2003
DOI: 10.1016/s1387-1811(03)00367-6
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Dehydrogenation of propane over natural clinoptilolite zeolites

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Cited by 37 publications
(19 citation statements)
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“…The major mineral phase present in the studied samples is found to be HEU-type zeolite, with percentages varying from 42 wt.% (sample X1) to 67 wt.% (sample X4), with an average amount of 57 wt.%. These results are in good agreement with previous studies on the zeolitic tuffs of Metaxades Area, which report an average amount of 58 wt.% in HEU-type zeolite (Marantos et al, 1989;Tsirambides et al, 1989Tsirambides et al, , 1993Tsirambides, 1991;Misaelides et al, 1994aMisaelides et al, ,b, 1995aKoutles et al, 1995;Symeopoulos et al, 1996;Haidouti, 1997;Tserveni-Gousi et al, 1997;Sikalidis, 1998;Yannakopoulos et al, 1998;Vlessidis et al, 2001;Filippidis and Kassoli-Fournaraki, 2002;Katranas et al, 2003;Papadopoulos et al, 2004;Filippidis and Kantiranis, 2005;Kantiranis et al, 2006;Filippidis et al, 2007). In minor amounts plagioclase (5-21 wt.%), K-feldspar (4-19 wt.%), cristobalite (3-17 wt.%), quartz (3-8 wt.%), micas (3-4 wt.%) and clay minerals (4-11 wt.%), were also determined.…”
Section: Resultssupporting
confidence: 92%
“…The major mineral phase present in the studied samples is found to be HEU-type zeolite, with percentages varying from 42 wt.% (sample X1) to 67 wt.% (sample X4), with an average amount of 57 wt.%. These results are in good agreement with previous studies on the zeolitic tuffs of Metaxades Area, which report an average amount of 58 wt.% in HEU-type zeolite (Marantos et al, 1989;Tsirambides et al, 1989Tsirambides et al, , 1993Tsirambides, 1991;Misaelides et al, 1994aMisaelides et al, ,b, 1995aKoutles et al, 1995;Symeopoulos et al, 1996;Haidouti, 1997;Tserveni-Gousi et al, 1997;Sikalidis, 1998;Yannakopoulos et al, 1998;Vlessidis et al, 2001;Filippidis and Kassoli-Fournaraki, 2002;Katranas et al, 2003;Papadopoulos et al, 2004;Filippidis and Kantiranis, 2005;Kantiranis et al, 2006;Filippidis et al, 2007). In minor amounts plagioclase (5-21 wt.%), K-feldspar (4-19 wt.%), cristobalite (3-17 wt.%), quartz (3-8 wt.%), micas (3-4 wt.%) and clay minerals (4-11 wt.%), were also determined.…”
Section: Resultssupporting
confidence: 92%
“…Among them, Fe-mordenite and Fe-clinoptilolite have shown catalytic properties for the SCR of NO with ammonia, similar to that of Fe-ZSM-5 [172]. Natural zeolites [173] have also been used because they have a good combination of their crystalline structures and exhibit interesting physicochemical properties with various metal oxy-hydroxide phases that are naturally embedded inside their pores [174]. However, potential commercialization of natural zeolites as catalysts is not feasible due to the cost of homogenisation and purification of the zeolite-bearing tuffs [175].…”
Section: Selective Catalytic Reduction (Scr) Of No By H 2 or Nh 3 Or mentioning
confidence: 99%
“…Natural zeolites are widely applied in the construction and building materials industry, water and wastewater treatment, environmental remediation as well as agriculture, consumer products and medical applications. Clinoptilolite is the main zeolite used for commercial applications, while chabazite and mordenite are used in smaller quantities [11]. Zeolitic tuffs are used as additives in cement and concrete to neutralize excess lime, but can also be thermally expanded to form light weighed insulation materials [12].…”
Section: Introductionmentioning
confidence: 99%