Journal of Physical Chemistry B, Vol.111, No.7, 1759-1768, 2007
UV-visible and H-1 or C-13 NMR spectroscopic studies on the specific interaction between lithium ions and the anion from tropolone or 4-isopropyltropolone (Hinokitiol) and on the formation of protonated tropolones in acetonitrile or other solvents
The specific interaction between lithium ions and the tropolonate ion (C7H5O2-: L-) was examined by means of UV-visible and H-1 or C-13 NMR spectroscopy in acetonitrile and other solvents. On the basis of the electronic spectra, we can propose the formation of not only coordination-type species (Li+(L-)(2)) and the ion pair (Li+L-) but also a "triple cation" ((Li+)(2)L-) in acetonitrile and acetone; however, no "triple cation" was found in N,N-dimethylformamide (DMF) and in dimethylsulfoxide (DMSO), solvents of higher donicities and only ion pair formation between Li+ and L- in methanol of much higher donicity and acceptivity. The H-1 NMR chemical shifts of the tropolonate ion with increasing Li+ concentration verified the formation of (Li+)(2)L- species in CD3CN and acetone-d(6), but not in DMF-d(6) or CD3OD. With increasing concentration of LiClO4 in CD3CN, the H-1 NMR signals of 4-isopropyltropolone (HL') in coexistence with an equivalent amount of Et3N shifted first toward higher and then toward lower magnetic-fields, which were explained by the formation of (Li+)(Et3NH+)L'(-) and by successive replacement of Et3NH+ with a second Li+ to give (Li+)(2)L'(-). In CD3CN, the 1,2-C signal in the C-13 NMR spectrum of tetrabutylammnium tropolonate (n-Bu4NC7H5O) appeared at an unexpectedly lower magnetic-field (184.4 ppm vs TMS) than that of tropolone (172.7 ppm), while other signals of the tropolonate showed normal shifts toward higher magnetic-fields upon deprotonation from tropolone. Nevertheless, with addition of LiClO4 at higher concentrations, the higher and lower shifts of magnetic-fields for 1,2-C and other signals, respectively, supported the formation of the (Li+)(2)L- species, which can cause redissolution of LiL precipitates. All of the data with UV-visible and H-1 and C-13 NMR spectroscopy demonstrated that the protonated tropolone (or the dihydroxytropylium ion), H2L+, was produced by addition of trifluoromethanesulfonic or methanesulfonic acid to tropolone in acetonitrile. The order of the 5-C and 3,7-C signals in C-13 NMR spectra of the tropolonate ions was altered by addition of less than an equivalent amount of H+ to the tropolonate ion in CD3CN. Theoretical calculations satisfied the experimental C-13 NMR chemical shift values of L-, HL, and H2L+ in acetonitrile and were in accordance with the proposed reaction schemes.