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Complexation behavior of a previously described heteroditopic cryptand L 1 and a newly synthesized cryptand L 2 toward transition metal ions is described. The cryptands readily accept a transition metal ion like Cu(II) or Ni(II) at the N 4 end of the cavity forming mononuclear cryptates. The Cu(II)-cryptate of L 1 further accepts a water molecule to form [Cu( L 1 )(OH 2 )]·(picrate) 2 ·(H 2 O), i.e., C 45 H 53 N 11 O 19 Cu. This molecule crystallizes in the monoclinic space group C 2/ c with a = 34.199(8) Å, b = 12.286(5) Å, c = 23.289(7) Å, β = 93.12(4)°, Z = 8. The O atom of the water molecule is strongly bonded to the Cu(II) ion, while its H atoms are H-bonded to the nearest benzene rings. The UV−vis spectral and magnetic studies of the complexes are consistent with the mononuclear nature of the cryptates. Cryptand L 1 undergoes diprotonation upon treatment with a mineral acid like HCl or HClO 4 . This diprotonated cryptand is found to be a good host for two molecules of water inside the cavity. The diperchlorate salt, [H 2 L 1 ⊂(H 2 O) 1.5 ]·(ClO 4 ) 2 ·(H 2 O) 0.75, i.e., C 33 H 51.5 Cl 2 N 5 O 13.25, crystallizes in the monoclinic space group P 2 1 / c with a = 12.204(1) Å, b = 11.465(1) Å, c = 28.537(3) Å, β = 91.98(2)°, Z = 4. The cryptand has an ellipsoidal cavity with both the bridgehead N atoms adopting an endo-endo conformation in the solid state. The water O atoms O(1w) and O(2w) lie in the pseudo 3-fold axis joining the two bridgehead N atoms. Occupancy of O(2w) is found to be 0.5 while that of O(1w) is unity. The water molecules are held inside the cavity through H-bonding with an ice-like structure. The FAB-mass spectral data and the bond distances involving the water oxygens suggest that both the water molecules are tightly held inside the cavity. The present cryptate is the first X-ray crystallographically characterized complex with two water molecules inside the cavity of a cryptand.
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Chand et al. (1998) studied this question.
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