Zsm 12 Synthesis Essay

Zeolites are microporous, aluminosilicateminerals commonly used as commercial adsorbents and catalysts.[1] The term zeolite was originally coined in 1756 by SwedishmineralogistAxel Fredrik Cronstedt, who observed that rapidly heating the material, believed to have been stilbite, produced large amounts of steam from water that had been adsorbed by the material. Based on this, he called the material zeolite, from the Greekζέω (zéō), meaning "to boil" and λίθος (líthos), meaning "stone".[2] The classic reference for the field has been Breck's book Zeolite Molecular Sieves: Structure, Chemistry, And Use.[3]

Zeolites occur naturally but are also produced industrially on a large scale. As of September 2016[update], 232 unique zeolite frameworks have been identified, and over 40 naturally occurring zeolite frameworks are known.[4][5] Every new zeolite structure that is obtained has to be approved by the International Zeolite Association Structure Commission and receives a three letter designation.[6]

Properties and occurrence[edit]

Zeolites have a porous structure that can accommodate a wide variety of cations, such as Na+, K+, Ca2+, Mg2+ and others. These positive ions are rather loosely held and can readily be exchanged for others in a contact solution. Some of the more common mineral zeolites are analcime, chabazite, clinoptilolite, heulandite, natrolite, phillipsite, and stilbite. An example of the mineral formula of a zeolite is: Na2Al2Si3O10·2H2O, the formula for natrolite.

Natural zeolites form where volcanic rocks and ash layers react with alkaline groundwater. Zeolites also crystallize in post-depositional environments over periods ranging from thousands to millions of years in shallow marine basins. Naturally occurring zeolites are rarely pure and are contaminated to varying degrees by other minerals, metals, quartz, or other zeolites. For this reason, naturally occurring zeolites are excluded from many important commercial applications where uniformity and purity are essential.

Zeolites are the aluminosilicate members of the family of microporous solids known as "molecular sieves" mainly consisting of Si, Al, O, and metals including Ti, Sn, Zn, and so on. The term molecular sieve refers to a particular property of these materials, i.e., the ability to selectively sort molecules based primarily on a size exclusion process. This is due to a very regular pore structure of molecular dimensions. The maximum size of the molecular or ionic species that can enter the pores of a zeolite is controlled by the dimensions of the channels. These are conventionally defined by the ring size of the aperture, where, for example, the term "8-ring" refers to a closed loop that is built from eight tetrahedrally coordinated silicon (or aluminium) atoms and 8 oxygen atoms. These rings are not always perfectly symmetrical due to a variety of effects, including strain induced by the bonding between units that are needed to produce the overall structure, or coordination of some of the oxygen atoms of the rings to cations within the structure. Therefore, the pores in many zeolites are not cylindrical.

Zeolites transform to other minerals under weathering, hydrothermal alteration or metamorphic conditions. Some examples:[7]


Industrially important zeolites are produced synthetically. Typical procedures entail heating aqueous solutions of alumina and silica with sodium hydroxide. Equivalent reagents include sodium aluminate and sodium silicate. Further variations include changes in the cations to include quaternary ammonium cations.[8]

Synthetic zeolites hold some key advantages over their natural analogues. The synthetic materials are manufactured in a uniform, phase-pure state. It is also possible to produce zeolite structures that do not appear in nature. Zeolite A is a well-known example. Since the principal raw materials used to manufacture zeolites are silica and alumina, which are among the most abundant mineral components on earth, the potential to supply zeolites is virtually unlimited.

Natural occurrence[edit]

Conventional open-pit mining techniques are used to mine natural zeolites. The overburden is removed to allow access to the ore. The ore may be blasted or stripped for processing by using tractors equipped with ripper blades and front-end loaders. In processing, the ore is crushed, dried, and milled. The milled ore may be air-classified as to particle size and shipped in bags or bulk. The crushed product may be screened to remove fine material when a granular product is required, and some pelletized products are produced from fine material.

As of 2016[update] the world's annual production of natural zeolite approximates 3 million tonnes. Major producers in 2010 included China (2 million tonnes), South Korea (210,000 t), Japan (150,000 t), Jordan (140,000 t), Turkey (100,000 t) Slovakia (85,000 t) and the United States (59,000 t).[9] The ready availability of zeolite-rich rock at low cost and the shortage of competing minerals and rocks are probably the most important factors for its large-scale use. According to the United States Geological Survey, it is likely that a significant percentage of the material sold as zeolites in some countries is ground or sawn volcanic tuff that contains only a small amount of zeolites. Some examples of such usage include dimension stone (as an altered volcanic tuff), lightweight aggregate, pozzolanic cement, and soil conditioners.[10]

Artificial synthesis[edit]

There are over 200 synthetic zeolites that have been synthesized by a process of slow crystallization of a silica-alumina gel in the presence of alkalis and organic templates. Many more such structures could theoretically be made.[11] In addition to variations in structures, zeolites can also be made with a variety of other atoms in them to make them chemically interesting and active. Some examples of the so-called heteroatoms that have been incorporated include germanium, iron, gallium, boron, zinc, tin, and titanium.[12] One of the important processes used to carry out zeolite synthesis is sol-gel processing. The product properties depend on reaction mixture composition, pH of the system, operating temperature, pre-reaction 'seeding' time, reaction time as well as the templates used. In sol-gel process, other elements (metals, metal oxides) can be easily incorporated. The silicalite sol formed by the hydrothermal method is very stable. The ease of scaling up this process makes it a favorite route for zeolite synthesis.

The zeolite conundrum[edit]

Computer calculations have predicted that millions of hypothetical zeolite structures are possible. However, only 232 of these structures have been discovered and synthesized so far, so many zeolite scientists question why only this small fraction of possibilities are being observed. This problem is often referred to as "the bottleneck problem". Currently there are a number of theories attempting to explain the reasoning behind this question.

  1. Zeolite synthesis research has primarily been concentrating on hydrothermal methods; however, new zeolites may be synthesized using alternative methods. Synthesis methods that have started to gain use include: microwave-assisted, post-synthetic modification, steam.
  2. Geometric computer simulations have shown that the discovered zeolite frameworks possess a behaviour known as "the flexibility window". This shows that there is a range in which the zeolite structure is "flexible" and can be compressed but retain the framework structure. It is suggested that if a framework does not possess this property then it cannot be feasibly synthesised.
  3. As zeolites are metastable, certain frameworks may be inaccessible as nucleation cannot occur because more stable and energetically favourable zeolites will form. Post-synthetic modification has been used to combat this issue with the ADOR method,[13] whereby frameworks can be cut apart into layers and bonded back together by either removing silica bonds or including them.


Zeolites are widely used as ion-exchange beds in domestic and commercial water purification, softening, and other applications. In chemistry, zeolites are used to separate molecules (only molecules of certain sizes and shapes can pass through), and as traps for molecules so they can be analyzed.

Zeolites are also widely used as catalysts and sorbents. Their well-defined pore structure and adjustable acidity make them highly active in a large variety of reactions.[14]

Zeolites have the potential of providing precise and specific separation of gases, including the removal of H2O, CO2 and SO2 from low-grade natural gas streams. Other separations include noble gases, N2, O2, freon and formaldehyde.

On-board oxygen generating systems (OBOGS) and Oxygen concentrators use zeolites in conjunction with pressure swing adsorption to remove nitrogen from compressed air in order to supply oxygen for aircrews at high altitudes, as well as home and portable oxygen supplies.[15]


Synthetic zeolites, as other mesoporous materials (e.g. MCM-41),are widely used as catalysts in the petrochemical industry, for instance in fluid catalytic cracking and hydrocracking. Zeolites confine molecules in small spaces, which causes changes in their structure and reactivity. The acidic forms of zeolites (prepared are often powerful solid-state solid acids, facilitating a host of acid-catalyzed reactions, such as isomerisation, alkylation, and cracking.

Catalytic cracking uses reactor and a regenerator. Feed is injected onto hot, fluidized catalyst where large gasoil molecules are broken into smaller gasoline molecules and olefins. The vapor-phase products are separated from the catalyst and distilled into various products. The catalyst is circulated to a regenerator where air is used to burn coke off the surface of the catalyst that was formed as a byproduct in the cracking process. The hot regenerated catalyst is then circulated back to the reactor to complete its cycle.

Zeolites have uses in advanced reprocessing methods, where their micro-porous ability to capture some ions while allowing others to pass freely, allowing many fission products to be efficiently removed from nuclear waste and permanently trapped. Equally important are the mineral properties of zeolites. Their alumino-silicate construction is extremely durable and resistant to radiation even in porous form. Additionally, once they are loaded with trapped fission products, the zeolite-waste combination can be hot pressed into an extremely durable ceramic form, closing the pores and trapping the waste in a solid stone block. This is a waste form factor that greatly reduces its hazard compared to conventional reprocessing systems. Zeolites are also used in the management of leaks of radioactive materials. For example, in the aftermath of the Fukushima Daiichi nuclear disaster, sandbags of zeolite were dropped into the seawater near the power plant to adsorb radioactive caesium which was present in high levels.[16]

The German group Fraunhofer e.V. announced that they had developed a zeolite substance for use in the biogas industry for long-term storage of energy at a density 4x more than water.[17] Ultimately, the goal is to be able to store heat both in industrial installations and in small combined heat and power plants such as those used in larger residential buildings.

Commercial and domestic[edit]

Zeolites can be used as solar thermal collectors and for adsorption refrigeration. In these applications, their high heat of adsorption and ability to hydrate and dehydrate while maintaining structural stability is exploited. This hygroscopic property coupled with an inherent exothermic (energy releasing) reaction when transitioning from a dehydrated to a hydrated form make natural zeolites useful in harvesting waste heat and solar heat energy. Zeolites are also used as a molecular sieve in cryosorption style vacuum pumps.[18]

The largest single use for zeolite is the global laundry detergent market. This amounted to 1.44 million metric tons per year of anhydrous zeolite A in 1992.[citation needed]

Non-clumping cat litter is often made of zeolite or diatomite.

Synthetic zeolites are used as an additive in the production process of warm mix asphalt concrete. The development of this application started in Germany in the 1990s. They help by decreasing the temperature level during manufacture and laying of asphalt concrete, resulting in lower consumption of fossil fuels, thus releasing less carbon dioxide, aerosols, and vapours. The use of synthetic zeolites in hot mixed asphalt leads to easier compaction and, to a certain degree, allows cold weather paving and longer hauls.

When added to Portland cement as a pozzolan they can reduce chloride permeability and improve workability. They reduce weight and help moderate water content while allowing for slower drying which improves break strength.[19] When added to lime mortars and lime-metakaolin mortars, synthetic zeolite pellets can act simultaneously as pozzolanic material and water reservoir.[20][21]


Thomsonites, one of the rarer zeolite minerals, have been collected as gemstones from a series of lava flows along Lake Superior in Minnesota and to a lesser degree in Michigan, U.S. Thomsonite nodules from these areas have eroded from basalt lava flows and are collected on beaches and by scuba divers in Lake Superior.

These thomsonite nodules have concentric rings in combinations of colors: black, white, orange, pink, purple, red, and many shades of green. Some nodules have copper inclusions and rarely will be found with copper "eyes". When polished by a lapidary the thomsonites sometimes display a "cat's eye" effect (chatoyancy).[22]


Research into and development of the many biochemical and biomedical applications of zeolites, particularly the naturally occurring species heulandite, clinoptilolite and chabazite has been ongoing.[23]

Zeolite-based oxygen concentrator systems are widely used to produce medical-grade oxygen. The zeolite is used as a molecular sieve to create purified oxygen from air using its ability to trap impurities, in a process involving the adsorption of nitrogen, leaving highly purified oxygen and up to 5% argon.

QuikClot brand hemostatic agent, which is used to stop severe bleeding,[24] contains a calcium-loaded form of zeolite found in kaolin clay.[25]

In agriculture, clinoptilolite (a naturally occurring zeolite) is used as a soil treatment. It provides a source of slowly released potassium. If previously loaded with ammonium, the zeolite can serve a similar function in the slow release of nitrogen. Zeolites can also act as water moderators, in which they will absorb up to 55% of their weight in water and slowly release it under the plant's demand. This property can prevent root rot and moderate drought cycles. Clinoptilolite has also been added to chicken food, the absorption of water and ammonia by the zeolite made the birds' droppings drier, less odoriferous and hence easier to handle.[26]

Pet stores market zeolites for use as filter additives in aquaria.[10] In aquaria, zeolites can be used to adsorb ammonia and other nitrogenous compounds. However, due to the high affinity of some zeolites for calcium, they may be less effective in hard water and may deplete calcium. Zeolite filtration is used in some marine aquaria to keep nutrient concentrations low for the benefit of corals adapted to nutrient-depleted waters.

Where and how the zeolite was formed is an important consideration for aquaria. Most Northern hemisphere natural zeolites were formed when molten lava came in contact with sea water, thereby "loading" the zeolite with Na (sodium) sacrificial ions. The mechanism is well known to chemists as ion exchange. These sodium ions will speciate with other ions in solution, thus the takeup of nitrogen in ammonia, with the release of the sodium. A deposit near Bear River in southern Idaho, (US) is a fresh water variety (Na < 0.05%). Southern hemisphere zeolites are typically formed in freshwater and have a high calcium content.[citation needed]

Zeolite filters ammonia effectively, but must be used with some care, especially with delicate tropical corals that are sensitive to water chemistry and temperature.

Zeolite mineral species[edit]

The zeolite structural group (Nickel-Strunz classification) includes:[4][7][27][28][29]

  • 09.GA. - Zeolites with T5O10 units (T = combined Si and Al) – the fibrous zeolites
  • 09.GB. - Chains of single connected 4-membered rings
  • 09.GC. - Chains of doubly connected 4-membered rings
    • Phillipsite framework (PHI): harmotome, phillipsite-series
    • Gismondine framework (GIS): amicite, gismondine, garronite, gobbinsite
    • Boggsite (BOG), merlinoite (MER), mazzite-series (MAZ), paulingite-series (PAU), perlialite (Linde type L framework, zeolite L, LTL)
  • 09.GD. - Chains of 6-membered rings – tabular zeolites
    • Chabazite framework (CHA): chabazite-series, herschelite, willhendersonite and SSZ-13
    • Faujasite framework (FAU): faujasite-series, Linde type X (zeolite X, X zeolites), Linde type Y (zeolite Y, Y zeolites)
    • Mordenite framework (MOR): maricopaite, mordenite
    • Offretite–wenkite subgroup 09.GD.25 (Nickel–Strunz, 10 ed): offretite (OFF), wenkite (WEN)
    • Bellbergite (TMA-E, Aiello and Barrer; framework type EAB), bikitaite (BIK), erionite-series (ERI), ferrierite (FER), gmelinite (GME), levyne-series (LEV), dachiardite-series (DAC), epistilbite (EPI)
  • 09.GE. - Chains of T10O20 tetrahedra (T = combined Si and Al)
  • Others

See also[edit]


  1. ^W. R. Grace & Co. Enriching Lives, Everywhere. – Zeolite StructureArchived February 15, 2009, at the Wayback Machine.. Grace.com. Retrieved on 2010-12-09.
  2. ^A.F. Cronstedt, Kongl Vetenskaps Academiens Handlingar Stockholm, 17, 1756, p. 120.
  3. ^Breck, Donald W. (1973-01-01). Zeolite molecular sieves: structure, chemistry, and use. Wiley. ISBN 9780471099857. 
  4. ^ abInternational Zeolite Association, Database of Zeolite Structures
  5. ^Webmineral Zeolites, Dana Classification
  6. ^"IZA Structure Commission". www.iza-structure.org. Retrieved 2017-01-23. 
  7. ^ abTschernich, Rudy W. (1992). Zeolites of the World. Geoscience Press. p. 563.  Note: 237 MB (PDF).
  8. ^Rollmann, L. D.; Valyocsik, E. W. (1995). Zeolite Molecular Sieves. Inorganic Syntheses. Inorganic Syntheses. 30. pp. 227–234. doi:10.1002/9780470132616.ch43. ISBN 9780470132616. 
  9. ^Zeolites (natural), USGS Mineral Commodity Summaries 2011
  10. ^ abRobert L. Virta Zeolites, USGS 2009 Minerals Yearbook (October 2010)
  11. ^Earl, David J.; Deem, Michael W. (2006-08-01). "Toward a Database of Hypothetical Zeolite Structures". Industrial & Engineering Chemistry Research. 45 (16): 5449–5454. doi:10.1021/ie0510728. ISSN 0888-5885. 
  12. ^Molecular Sieves - Principles of Synthesis and | Rosemarie Szostak | Springer. 
  13. ^Roth, Wieslaw J.; Nachtigall, Petr; Morris, Russell E.; Wheatley, Paul S.; Seymour, Valerie R.; Ashbrook, Sharon E.; Chlubná, Pavla; Grajciar, Lukáš; Položij, Miroslav (2013-07-01). "A family of zeolites with controlled pore size prepared using a top-down method". Nature Chemistry. 5 (7): 628–633. doi:10.1038/nchem.1662. ISSN 1755-4330. 
  14. ^Bhatia, Subhash (1989-12-21). Zeolite Catalysts: Principles and Applications. CRC Press. ISBN 9780849356285. 
  15. ^"On-Board Oxygen Generating System (OBOGS)." Honeywell.Archived September 10, 2011, at the Wayback Machine.
  16. ^Levels of Radioactive Materials Rise Near Japanese Plant. The Associated Press via NYTimes, April 16, 2011
  17. ^"Compact and flexible thermal storage". Fraunhofer-Gesellschaft. 1 June 2012. 
  18. ^Guglielmo Ventura; Lara Risegari (26 November 2007). The Art of Cryogenics: Low-Temperature Experimental Techniques. Surendra Kumar. pp. 17–. ISBN 978-0-08-044479-6. Retrieved 4 June 2012. 
  19. ^Jana, Dypayan (2007). "Clinoptilolite – a promising pozzolan in concrete"(PDF). A New Look at an Old Pozzolan. 29th ICMA Conference. Quebec City, Canada: Construction Materials Consultants, Inc. Retrieved 7 October 2013. 
  20. ^Andrejkovičová, Slávka; et al. (2012). "Air Lime Mortars with Incorporation of Sepiolite and Synthetic Zeolite Pellets"(PDF). Acta Geodynamica et Geomaterialia. 9: 79–91. 
  21. ^Ferraz, E.; et al. (2014). "Synthetic zeolite pellets incorporated to air lime–metakaolin mortars: mechanical properties". Construction & Building Materials. 69: 243–252. doi:10.1016/j.conbuildmat.2014.07.030. 
  22. ^Dietrich, R. V. (2005-07-14). "Thomsonite". Retrieved 2 October 2013. 
  23. ^Handbook of zeolite science and technology, Scott M. Auerbach, Kathleen A. Carrado, Prabir K. Dutta, eds. CRC Press, 2003, p. 16. ISBN 0-8247-4020-3
  24. ^Rhee P., Brown C., Martin M., et. al. (2008). "QuikClot use in trauma for hemorrhage control: case series of 103 documented uses". J. Trauma. 64 (4): 1093–9. doi:10.1097/TA.0b013e31812f6dbc. PMID 18404080. 
  25. ^Rowe, Aaron (24 April 2008). "Nanoparticles Help Gauze Stop Gushing Wounds". Wired.com. Retrieved 1 November 2013. 
  26. ^"Chapter VIII: Using Zeolites in Agriculture"(PDF). Retrieved 28 March 2014. 
  27. ^IMA Database of Mineral Properties
  28. ^Nickel-Strunz classification 10 ed, mindat.org
  29. ^First, E. L.; Gounaris, C. E.; Wei, J.; Floudas, C. A. (2011). "Computational characterization of zeolite porous networks: An automated approach". Physical Chemistry Chemical Physics. 13 (38): 17339–17358. doi:10.1039/C1CP21731C. PMID 21881655. 

Further reading[edit]

  • Zeolites in Sedimentary Rocks. Ch. in United States Mineral Resources, Professional Paper 820, 1973.
  • Natural and Synthetic Zeolites. U.S. Bureau of Mines Information Circular 9140, 1987.
  • Frederick A. Mumpton (1999). "La roca magica: Uses of natural zeolites in agriculture and industry". PNAS. 96 (7): 3463–3470. doi:10.1073/pnas.96.7.3463. PMC 34179. PMID 10097058. 
  • "Zeolite-water close cycle solar refrigeration; numerical optimisation and field-testing", Jean-Baptiste Monnier; Dupont, M. Proc. Annu. Meet. – Am. Sect. Int. Sol. Energy Soc.; Vol/Issue: 6 pp 181–185; American Solar Energy Society meeting; 1 June 1983; Minneapolis, MN, USA
  • Cheetham, A.K.; Peter Day (1992). Solid State Chemistry. Clarendon Press. 
  • Rhodes, Christopher J. (2007). "Zeolites: Physical Aspects and Environmental Applications". Annual Reports on the Progress of Chemistry, Section C. 103: 287–325. doi:10.1039/b605702k. 

External links[edit]

Wikimedia Commons has media related to Zeolite.

IMA–CNMNC / Nickel–Strunz IDs
Mineral categories (classes, subclasses, divisions)

"Special cases"
("native elements and organic minerals")
"Sulfides and oxides"
  • Sulfides (IDs 2.A–F)
  • Sulfosalts; sulfarsenites, sulfantimonites, sulfbismuthites (IDs 2.G)
  • Sulfosalts; sulfarsenates, sulfantimonates (IDs 2.K)
  • Other sulfosalts (IDs 2.H–J and 2.L–M)
  • Tellurium oxysalts
  • Vanadium oxides (IDs 4.H)
"Evaporites and similars"
"Mineral structures with tetrahedral units"
(sulfate anion, phosphate anion,
silicon, etc.)
  • Monomeric minerals (similar to nesosilicates)
  • Sulfates (IDs 7.A–E)
  • Thiosulphates (IDs 7.J)
  • Silicate frameworks, tectosilicates
  • Other tectosilicates (IDs 9.FA. and 9.FB.15, e.g. feldspars)
  • Other silicate frameworks
  • Ribbon or multiple chain inosilicates (IDs 9.D, e.g. amphiboles)
  • Other non monomeric minerals
  • Unclassified silicates (IDs 9.H)
Natural zeolite with a United States one-cent coin (penny) for scale
A form of thomsonite (one of the rarest zeolites) from India
A combination specimen of four zeolite species. The radiating natrolite crystals are protected in a pocket with associated stilbite. The matrix around and above the pocket is lined with small, pink-colored laumontite crystals. Heulandite is also present as a crystal cluster on the backside

1. Introduction

Different carbohydrates, exemplified by glucose, can be alkylated by long-chain alcohols over acid catalysts to yield non-ionic surfactants. Sulfonic acids are used as catalysts on an industrial scale, but the glycosidation process continues to be studied using different classes of catalysts. Thus, dealuminated Y type zeolites were screened in glycosidation reactions [1]. Extensive studies on the use of zeolites in the synthesis of alkyl glucosides were conducted by Corma et al. [2,3,4,5]. It was demonstrated that the highest activity in the synthesis of both C4 and long-chain alkyl glucosides was exhibited by H-Beta zeolite. Glycosidation of disaccharides with short- and long-chain alcohols over MCM-41 mesoporous molecular sieves was also studied [6].

On the other hand, perfluoroalkylglucosides comprise a very specific and important class of fluorosurfactants due to their potential applications [7]. A detailed account of these surface active agents was given by Reiss and Greiner [8,9,10]. Their particular importance stems from their application as emulsion stabilizers in biomedicine. Emulsions of fluorohydrocarbons are excellent oxygen carriers, and they are also used as contrasting media in diagnostics and various systems for other medical applications. Stabilization of such emulsions can be accomplished by fluorinated surfactants, especially those based on various carbohydrates. However, before application of such compounds certain conditions must be met: first, a structure should be well-defined, second, their biocompatibility should be assessed taking into account the required purity. The criteria mentioned above have determined the majority of synthesis methods, chosen in such a way as to yield particular compounds amenable for non-problematic purification.

One of synthesis paths yielding alkylglucosides with well-defined structures and free from contamination with higher oligomers is known as the Koenigs-Knorr method. In this method bromides of acetylated carbohydrates and a suitable alcohol are used as reagents (after deacetylation, a glucoside is obtained). However, when using fluorinated alcohols, an abnormal synthesis route ocurrs, and, instead of a glucoside, an orthoester is formed; detailed accounts of this phenomenon were given by Riess et al. [8]. As concluded by Riess, the very low nucleophilicity of perfluoroalcohols makes it difficult to substitute the C1 hydroxy group in the glucose molecule and form perfluoroalkyl glucosides using the Koenigs-Knorr route. High yields of O-fluoroalkylglucosides (>90%) were obtained when using this method. Its modification is based on formation of 1-O-alkylglucoside, which reacts further with a fluoroalkyl iodide to yield a iodoperfluoroglucoside. The latter compound can be conveniently transformed into a perfluoroalkylglucoside by zinc reduction.

The Mitsunobu reaction has gained wide acceptance as a versatile method in organic synthesis—it transforms hydroxyl groups into another groups which can be in turn displaced by nucleophiles [11]. Thus, O-fluoroalkylglucosides can be readily prepared according to this route. Synthesis of perfluoroalkylglucosides was carried out for the first time by Falck [12].

The methods described above have, however, limited application for laboratory use only. In this contribution we propose a useful method for the synthesis of perfluoroalkylglucosides by applying a Fischer reaction, that is, starting directly from glucose and the corresponding perfluoroalcohol (cf.Scheme 1). The results of glycosidation by the Fischer reaction over a variety of catalysts were described by Straathof et al., in particular, the acidic ion-exchange resins (Amberlyst 131, Purolite C122) proved to be especially good for this purpose [13].

Scheme 1. Synthesis of perfluoroalkylglucosides from glucose and alcohols by using the Fischer reaction.

Scheme 1. Synthesis of perfluoroalkylglucosides from glucose and alcohols by using the Fischer reaction.

The objective of the present work was to apply zeolite catalysts in the reaction visualized in Scheme 1. Four zeolites differing in structure, composition and pores architecture have been chosen: ZSM-5, ZSM-12, MCM-22 and Beta. Catalytic tests were performed in the liquid phase under the conditions relevant for practical implementation.

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