and 12 was observed, the major product being alkylated at
the nitrogen closer to the tert-butyl group. The regiochemistry
of the products 11b-g was assigned on the basis that their
CHAHBPh groups display diastereotopic signals (due to slow
rotation about an Ar-N axis14) and confirmed for 11g by
X-ray crystal structure (Figure 2), for 11h by comparison
with an authentic sample of the alternative regioisomer (see
Scheme 3), and for 12j and 12k by NOE studies. Presumably,
Scheme 4. Lithiation of Unsymmetrically Methylated Ureas
11h with 2.5 equiv of sec-BuLi in THF at -78 °C and
allowing the mixture of dilithiourea 15 and electrophile to
warm to -40 °C before aqueous quench of excess base.
Other bases (n-BuLi, t-BuLi, sec-BuLi in the presence of
TMEDA) generally gave lower yields. A range of electro-
philes reacted with 15, as shown in Table 2, providing ureas
16a-g. In every case, regioselectivity was complete, with
the newly introduced electrophile occupying the 6-position
on the 2-alkylated ring, the left-hand ring of 16.15 No
lithiation was observed on the right-hand phenyl ring.
Figure 2. X-ray crystal structure of 11g.
Table 2. Regioselective Ortholithiation
the twist in the Ar-N bond imposed by the steric require-
ments of a substituent in the ortho position prevents
delocalization of the anion 13 into the more hindered ring,
increasing electron density and reactivity at the nearer
nitrogen atom, despite its more crowded environment.
The alternative N-alkylated regioisomer 12h was available
simply by addition of N-methylaniline to isocyanate 14
(Scheme 3). Regioisomers 11h and 12h were clearly different
by NMR.
entry
E+
E
product 16 yield of 16 (%)
1
2
3
4
5
6
7
MeI
Me
16a
16b
16c
16d
16e
16f
65
80
93
95
81
66
83a
BrCH2CH2Br Br
I2
I
Me2S2
SMe
Me3SiCl
Me2NCHO
PhCHO
SiMe3
CHO
CH(OH)Ph
16g
a Product formed as a separable mixture of two diastereoisomeric
atropisomers.
Scheme 3. Alternative Regioisomer
Two structural features differentiate the two rings: the ring
tert-butyl substituent and the N-methyl group, and we wanted
to know which was governing this remarkable regioselec-
tivity. We therefore made the two isomeric ureas 17a and
17b and lithiated them under our optimized conditions,
quenching with trimethylsilyl chloride to determine regio-
With the regioselectively alkylated ureas 11 in hand, we
proceeded to study their ortholithiation. Optimum conditions
were established by treating 11h with at least 2 equiv of
organolithium base and quenching with an electrophile
(Scheme 4 and Table 2) to yield the functionalized ureas
16. We found that the best yields resulted from lithiating
(14) An Ar-N axis rotating slow enough to indicate chirality on the
NMR time scale is possible only if the nitrogen is fully substituted and the
Ar group is unsymmetrically functionalized (Adler, T.; Bonjoch, J.; Clayden,
J.; Font-Bardia, M.; Pickworth, M.; Solans, X.; Sole´, D.; Vallverdu´, L. Org.
Biomol. Chem., in press. These conditions are not met in compounds 12,
which cannot show chirality on the NMR time scale.
(15) Regioselectivity was assigned by analysis of coupling patterns in
the aromatic region of the 1H NMR spectra of 16, and for 16g by NOE
indicating proximity of NMe and PhCH. Alcohol 16g was isolated as two
separable diastereoisomers: a future publication will report our observations
on atropisomerism in related N,N′-diarylureas.
(10) Monodeuteration was indicated by a 1/6 decrease in the intergral
of the NMe peaks of the 1H NMR spectrum, but the regioselectivity remains
unassigned.
(11) Beak, P.; Reitz, D. B. Chem. ReV. 1978, 78, 275.
(12) See ref 8 for a discussion.
(16) Remainder is starting material. Urea 19 exists as an inseparable
mixture of diastereoisomeric conformers. Compare ref 15.
(13) No diastereotopic signals were seen for 11a (see ref 14), but we
cannot be sure whether this is due to fast Ar-N rotation resulting from the
small size of the fluoro substituent or because electronegative F induces a
reversal of reactivity in the two monoanion tautomers 13.
(17) (a) Clark, R. D.; Jahangir, A. Org. React. 1995, 47, 1. (b) Clayden,
J. Organolithiums: SelectiVity for Synthesis; Pergamon: Oxford, 2002;
Chapter 2.4, p 73. Lateral lithiation of ureas was, to our knowledge,
previously unknown.
Org. Lett., Vol. 7, No. 15, 2005
3149