Reich and Whipple
1583
obligatory intermediate), and as a reactive partner in its own
right in donating a thienyl anion to iodothiophene (eq. [3]).
The latter observation suggests that ate complexes may be
reactive partners in reactions when lithium reagents are pre-
pared by Li–I exchange. The fact that solutions of iodide
and lithium reagent are stable in samples where upwards of
109 Li–I exchanges have occurred during an experiment pro-
vides a strong argument that single electron transfer reac-
tions involving aryl radical intermediates play no role in the
reaction, since cage effects of this magnitude would seem
impossible.
Rate of Li–I exchange for the dimer (k4)
7
The observation that the Li NMR signal of the dimer 4D
could be decoalesced from the averaged signal comprising
the lithiums of 4M and 5 in Fig. 6B shows that the dimer is
not undergoing Li–I exchange (eq. [4]) under conditions
7
where exchange of monomer is rapid. The Li NMR signal
of 4D at –102 °C is 60 Hz wide. At the same temperature
the 13C NMR signal of 4D in a sample containing only 4 is
80 Hz (Fig. 2), so there is no detectable broadening assign-
able to the Li–I exchange of dimer, the k4 process. If we es-
timate that no more than 10 Hz of the 60 Hz line width of
the lithium signal could be due to the k4 process, then the
NMR rate constant kDA ≤ 31 s–1 (π∆ν), and the physical rate
constant k4 = kDA/[6] ≤ 670 s–1 (mol/L)–1. Since the rate of
exchange of the iodide with monomer (k2) is 6.7 × 106 s–1
(mol/L)–1 at –102 °C (see eq. [2]), reaction of dimer with the
iodide is at least a factor of 1000 slower than reaction of the
monomer. Although many reactivity effects of organolithium
reagents have been ascribed to aggregation phenomena, de-
termination of quantitative and qualitative differences be-
tween reactivity of different aggregates of an organolithium
species under the same conditions has rarely been reported
(24, 25). This result shows that the common assumption that
higher aggregates are less reactive than lower ones holds
well in this monomer–dimer case, and that the differences
can be quite large.
Experimental section
General
All glassware was dried in an oven at 110 °C for at least
2 h and flushed with N2 for at least 5 min. All reactions
were performed under an atmosphere of dry nitrogen.
Instrumentation
GC analyses were performed using a 12 m × 0.32 mm
SE-30 capillary column, with He pressure of 6.0 psi (1 psi =
6.894 757 kPa), column flow rate (split ratio 300:1) of
3 mL/min, and column temperature of 90 °C. Retention times
and response factors with respect to n-undecane are as fol-
lows: 2-iodo-5-methylthiophene (2.77 min, 2.39), 2-(methylthio)-
5-methylthiophene (2.87 min, 1.99), n-undecane (2.67 min,
1.00). For a 1:1 molar solution of compound: C11H24, the re-
sponse factor = (peak area C11H24)/(peak area compound).
Summary
A DNMR investigation of 2-lithio-5-methylthiophene (4)
showed this lithium reagent to be a mixture of monomer and
4-center dimer in THF–ether (3:2). Solutions of 4 and the
corresponding iodide 6 undergo Li–I exchange on the NMR
timescale. The ate complex 5, a probable intermediate in the
exchange, is formed with a high association constant at low
temperature (–130 °C), but is largely dissociated at tempera-
tures above –70 °C. A variable-temperature DNMR kinetic
analysis showed that three exchange processes occurred on
the NMR timescale, the monomer dimer exchange (eq. [1]),
the Li–I exchange of the monomeric lithium reagent
(eq. [2]), and direct exchange between the ate complex and
the iodide (eq. [3]). The ate complex 5 is comparable in re-
activity to the monomeric lithium reagent 4M in the Li–I ex-
change process. The data obtained also allowed an estimate
of the upper limit of a fourth process, the Li–I exchange of
the dimer (eq. [4]). The bimolecular rate constants at –102 °C
are shown in the following:
7
6
13C, Li, and Li NMR spectra were obtained on a Bruker
AM-360 spectrometer operating at 90.56, 139.96, and
53.00 MHz, respectively. The NMR spectra were acquired
unlocked and in non-deuterated solvents unless otherwise
stated. For 13C NMR, a 30° pulse of 5 µs repeated every
2.9 s was used. An exponential line broadening of 2–5 Hz
was used, and a 64 K transform was carried out over a spec-
tral width of 20 800 Hz. 13C NMR chemical shifts are re-
ported in ppm relative to TMS (δ 0.0), using THF as an
7
internal reference. Li NMR spectra were recorded over a
spectral width of 1400 Hz (8K data points) using a 10 µs
pulse and 6Li NMR spectra over a spectral width of 2907 Hz
(8K data points) with a pulse width of 10 µs and a recycle
7
6
delay of 4 s. Both Li and Li NMR chemical shifts were
referenced to external 0.30 mol/L LiCl in MeOH (δ 0.0 ≈
–100 °C) (19c). n-Bu-6Li (95.5% enriched) was prepared by
literature procedures (7l).
Probe temperatures were measured (decoupler turned off)
by replacing the sample with an open tube containing the
same solvent and the sensor of a RTD (platinum resistance)
thermometer, which was designed to measure temperatures
from –150 °C to 50 °C, and was calibrated using ice water
(0.01 °C) and CO2 (–78.5 °C). The accuracy of the resis-
tance thermometer was checked with the melting points of
toluene (–95.00 °C) and methylcyclohexane (–126.6 °C) and
were found to be within 0.4 °C of the reported value. Sam-
ples were allowed to equilibrate for at least 8 min in the
probe prior to tuning the spectrometer and acquiring the
spectrum. Probe temperatures were confirmed following the
acquisition of each spectrum.
Rate constant
k ((mol/L)–1 s–1)
krel
1/100
1.0
1.9
<1/1000
6.8×103
6.7×105
1.3×106
<6.6×102
k1 (eq. [1])
k2 (eq. [2])
k3 (eq. [3])
k4 (eq. [4])
The lithium iodine exchange reaction has been mechanis-
tically controversial since its discovery in 1938. The present
DNMR investigation, together with other related papers (7a–
7c), places aryl iodine ate complexes (5) firmly into the
mechanistic picture in two roles: as a permissible intermedi-
ate in the exchange itself (our results do not make it an
DNMR simulations were performed with the Binsch
DNMR program (26) and with WINDNMR (7m).
© 2005 NRC Canada