REPORTS
R
R
and insertion of the Ru atom are expected to be favored
at the C-2 carbon of indene. Previously, we also observed
the formation free benzene molecule in the reactions
catalyzed by 1 (12, 16).
Fig. 4. Proposed mechanism of the alkyl-
R'CH2OH
R
2
ation of an alkene (CH2=CHR) with an al-
cohol (R′CH2OH). rds, rate-determining step.
R = R′ = alkyl, aryl.
[Ru]
HO
1
[Ru]
22
-C6H6, -PCy3
H2O
R
R'
R
19. R. M. Roberts, A. A. Khalaf, Friedel-Crafts Alkylation
Chemistry: A Century of Discovery (Dekker, New York,
1984).
[Ru] = Ru(CO)L
[Ru] = Ru(CO)Ln
rds
L = alkene, alconhol
L = alkene, alcohol
R'
20. G. A. Olah, R. Krishnamurti, G. K. S. Prakash, in
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OH
[Ru]
OH
[Ru]
23
H
R
R
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be a key intermediate in C–H bond activation chemistry.
For representative examples, see (32, 33).
26. The formation of a free benzene molecule (2%) is
detected after heating the reaction mixture at 70°C for
15 min using 5 mol % of 1. Previously, we observed
similar results in the reactions catalyzed by 1 (12, 16).
27. Y. Feng et al., J. Am. Chem. Soc. 127, 14174 (2005).
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2010).
for the alkylation reaction. We (23) and others
(24) observed similar carbon isotope effects in
ruthenium-catalyzed C–H insertion reactions,
where C–C bond formation has been proposed
as the rate-limiting step.
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indene is most consistent with the vinyl C−H activation
mechanism. The selective deuterium incorporation on the
C-1 and C-3 carbons of indan can readily be explained
from regioselective insertion of indene to Ru−D, followed
by reductive elimination with the hydride formed from
the vinyl C−H activation of another indene molecule. Due
to steric hindrance from the arene hydrogen, metalation
On the basis of these results, we propose a
mechanism involving a cationic Ru-alkenyl spe-
cies 22, which is initially formed from the re-
action of 1 with two equivalents of the olefin
substrate via the vinylic C–H activation and an
alkane elimination step (Fig. 4) (25). As support-
ing evidence for the Ru-alkenyl species, we have
been able to detect the formation of indan and
free benzene molecules from the crude reaction
mixture of indene with 4-methoxybenzyl alcohol
(26). Though the exact mechanism of the C–O
cleavage step is not clear at the present time, one
possible pathway involves the oxidative addition
of the C–O bond to form a cationic Ru(IV)-
alkenyl-alkyl species, from which reductive elim-
ination proceeds to yield the alkylation product
and a cationic Ru-hydroxo complex 23. Notably,
Ru-hydroxo complexes have been shown to ex-
hibit high activity for both C–H and H–H bond
activation reactions (27, 28). The carbon iso-
tope effect study provides strong support for a
turnover-limiting C–C bond formation step. A
few electrophilic ruthenium complexes have been
found to mediate the C–O bond cleavage re-
action of alcohols and acetals (29–31). The
subsequent vinylic C–H activation and water
elimination is envisaged for the regeneration of
the Ru-alkenyl species 22. Extensive hydrogen-
deuterium exchange between indene and 2-
propanol-d8 substrates suggests that the vinylic
C–H bond activation step is facile and reversible
under the catalytic conditions.
Our catalytic alkylation method exhibits a
broad substrate scope, as well as a high degree of
regio- and chemoselectivity without requiring any
co-catalysts or additives, and generates no wasteful
by-products other than water. Whereas chlorinated
solvents such as CH2Cl2 and C6H5Cl generally
give the best results, nonchlorinated solvents such
as toluene and tetrahydrofuran can be used in most
cases without sacrificing product yields or selec-
tivity (though they require a longer reaction time).
We anticipate that the catalytic method will con-
tribute substantially to the development of next-
generation “green” catalytic processes.
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Acknowledgments: We thank the NSF for financial support
(grant CHE-1011891).
Supporting Online Material
SOM Text
Figs. S1 to S3
Tables S1 to S3
References (34–38)
24 May 2011; accepted 3 August 2011
10.1126/science.1208839
Soil Nitrite as a Source of
Atmospheric HONO and OH Radicals
Hang Su,1*† Yafang Cheng,2,3*† Robert Oswald,1 Thomas Behrendt,1 Ivonne Trebs,1
Franz X. Meixner,1,4 Meinrat O. Andreae,1 Peng Cheng,2 Yuanhang Zhang,2 Ulrich Pöschl1†
Hydroxyl radicals (OH) are a key species in atmospheric photochemistry. In the lower atmosphere,
up to ~30% of the primary OH radical production is attributed to the photolysis of nitrous acid
(HONO), and field observations suggest a large missing source of HONO. We show that soil nitrite
can release HONO and explain the reported strength and diurnal variation of the missing source.
Fertilized soils with low pH appear to be particularly strong sources of HONO and OH. Thus, agricultural
activities and land-use changes may strongly influence the oxidizing capacity of the atmosphere.
Because of the widespread occurrence of nitrite-producing microbes, the release of HONO from soil
may also be important in natural environments, including forests and boreal regions.
eterogeneous reactions of NO2 have NO2, however, atmospheric aerosols have too
been suggested to be a missing source little surface area to account for the measured
of nitrous acid (HONO) to the atmo- HONO production rates (7, 8). Thus, recent studies
H
sphere (1–4), and photoenhanced reactions on suggested that the reduction of N(IV) in NO2 to
the surface of soot and other aerosol particles N(III) in HONO may proceed on ground surfaces
have been proposed to explain the observed en- (7, 8), and field data indicate that HONO is in-
hancement of HONO production rates during the deed released from the ground (10, 11).
The dominant sources of N(III) in soil, how-
(5–9). Because of low uptake coefficients for ever, are biological nitrification and denitrifica-
References and Notes
1. G. A. Olah, A. Molnár, Hydrocarbon Chemistry
(Wiley, New York, 2003).
daytime [up to 5 parts per billion (ppb) hour–1]
1616