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Cu Y Zeolite

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionDec 14, 2025
Entity authorityQ19903892
Source-derived summary

Cu-Y zeolites (CuY, CuFAU, copper faujasite) are copper-containing high-silica derivatives of the faujasite mineral group which in turn is a member of the zeolite family. Cu-Y zeolites are synthesized through aqueous or gaseous ionic exchange unlike the naturally occurring faujasites: faujasite-Ca, faujasite-Mg, and faujasite-Na. The exchanged copper atom can vary in oxidation states, but the most studied Cu-Y zeolite variants include Cu(I) or Cu(II) cations. Due to their high catalytic potential, they are utilized as desulfurization agents and in the production of nitrogen gas from nitrogen monoxide.

History

Copper based type Y zeolites were first described as a means of hydrocracking in a patent filed in 1963, and were soon implemented in industrial hydrocracking processes. They eventually began to find use in other industries as the usage of zeolites increased as a whole, such as removal of carbon monoxide from gas. In 1972, a patent was filed describing the production of Cu-Y zeolites from sodium-based zeolites, helping to further spread its use in the industry. The first documented use of Cu-Y zeolites for desulfurization was in 1977, in which a variety of zeolites including the Cu-Y variant were used to remove hydrogen sulfide from gases. From then on, various methods were developed utilizing Cu-Y zeolites in desulfurization of hydrocarbons, reducing their environmental impact when used as fuel.

Properties

Many experiments have been done to understand the properties of Cu-Y zeolites.

Editorial summary

This brief starts where responsible research should: with the source description of “Cu Y Zeolite” as open-knowledge reference entry. Everything that follows is an evidence route, not borrowed authority.

Editorial reviewA concise reference frame for defining the subject, testing terminology and identifying the institution closest to the evidence. The current lead gives the account dated anchors—1963, 1972, 1977—that can be checked directly. The selected authority fields contribute no independent date. The account is most persuasive where Zeolite, Open-knowledge and entry can be independently traced.
Editorial analysis

Why this record matters

The subject matters to the general reference register because the source frames it as open-knowledge reference entry. Its deeper value depends on whether names, dates, institutions and citations support that framing.

Evidence profile

Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Dec 14, 2025. The linked authority identifier is Q19903892. None of the 0 selected statements returned an explicit reference. The first chronological checks are 1963, 1972 and 1977.

Critical limits

Overview language is designed for orientation and should not be treated as a substitute for the evidence cited beneath it. The lead is largely declarative, so disagreement and counter-evidence require a deliberate search beyond the opening account. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Use the entry as an orientation point, then follow its citations and revision history. Names, dates and institutional relationships should be checked against the original record.

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  2. Expand the search: follow Cu Y Zeolite primary sources, Cu Y Zeolite archive and Zeolite research across catalogues and specialist indexes.
  3. Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.

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Source & attribution

This entry incorporates text from Cu Y Zeolite” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.