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(K4Li4)Al8Ge8O 32·8H2O: An Li+-exchanged potassium aluminogermanate with the zeolite gismondine (GIS) topology

  • Aaron J. Celestian
  • , John B. Parise
  • , Akhilesh Tripathi
  • , Åke Kvick
  • , Gavin M.B. Vaughan
  • Stony Brook University
  • Texas A&M University
  • European Synchrotron Radiation Facility

Research output: Contribution to journalArticlepeer-review

1 Scopus citations

Abstract

The title compound, lithium potassium dialuminium digermanium octaoxide dihydrate, (K,Li)-(Al,Ge)-GIS (GIS is gismondine), is the result of a 50% Li+ exchange into the K-(Al,Ge)-GIS structure. The (K,Li)-(Al,Ge) -GIS structure was determined from a 4 × 4 × 2 μm octahedral single crystal at the ESRF synchrotron X-ray source. The ion exchange results in a symmetry transformation from I2/a for K-(Al,Ge)-GIS to C2/c for (K,Li)-(Al,Ge)-GIS. The structural change is due to disordering of K + ions with Li+ ions along the [001] channel and ordering of water molecules in the [101] channels. The distance between sites partially occupied by K+ ions increases from 2.19 (3) Å in K-(Al,Ge)-GIS to 2.94 (3) Å in (K,Li)-(Al,Ge)-GIS. The Li+ ions occupy positions along the twofold axis at the intersection of the eight-membered-ring channels in a twofold coordination with water molecules. For the four closest framework O2- anions, the Li⋯O distances are 3.87 (4) Å.

Original languageEnglish
Pages (from-to)i74-i76
JournalActa Crystallographica Section C: Crystal Structure Communications
Volume59
Issue number8
DOIs
StatePublished - Aug 2003

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