Dr. Kanaya of the Atmospheric
Composition Research Program, Frontier Research Center for
Global Change, received the Chemical Society of Japan Award
For Young Chemists for FY2004. The Chemical Society of Japan,
a 36,000-member organization with a history of 127 years,
gives the award every year to 10 or less young researchers
(limited to those aged less than 35) for their outstanding
research accomplishment in fundamentals and applications of
chemistry. His receiving is based upon the "Elucidation
of the Tropospheric Chemistry Mechanism by Measuring the OH
and HO2 Radical Concentration in the
Atmosphere". In the troposphere, the OH radical is the
most important "cleansing agent", whose chemical
reactions initiate the transformation of many trace gases
(NOx and hydrocarbons etc.) into water-soluble
species, which are then easily removed from the atmosphere.
Simultaneously, the OH radical is essential in controlling
the atmospheric burden of methane and O3,
both of which are the important greenhouse gases. Despite
these key roles, its very low concentrations in the atmosphere
had kept us away from characterizing its behavior through
direct observations. Kanaya started developing a laser-induced
fluorescence instrument for measuring both OH and its reservoir
HO2 in the atmosphere as a graduate
student in the University of Tokyo and completed it in JAMSTEC.
In the last stage of the development, much effort was put
in optimizing the fluorescence detector and finally, the detection
limit of as low as 2x105 cm-3
(mixing ratio of 0.008 pptv, with 1-min.
integration) was achieved. This performance is comparable
to or even higher than those of the similar instruments developed
by other research groups in the US, UK, and Germany.
The instrument was set up at clean remote islands (Oki, Okinawa,
and Rishiri) and in Tokyo, where the OH and HO2
concentrations were observed to study their chemical production
and loss processes in detail. The observed concentration levels
were compared with those predicted by a photochemical box
model employing a tropospheric chemistry mechanism. At Oki
and Rishiri Islands, the model significantly overpredicted
the daytime HO2 levels by up to a factor
of 2, suggesting that some important processes were still
missing from our current knowledge of the tropospheric chemical
reactions.
Kanaya has proposed several hypotheses possibly explaining
the discrepancy, including that the HO2
radical is lost on the aerosol surfaces by heterogeneous reactions
and that the OH and HO2 radical concentrations
are influenced by halogen chemistry. Particularly, IO radical,
if produced via the photolysis of organoiodine species emitted
from marine ecosystem (mainly by seaweeds) into the atmosphere,
could react with HO2 rapidly, influencing
the concentrations of OH and HO2. The
hypothesis regarding the iodine chemistry has recently been
verified by the observations in Ireland.
During the observations, it was also found that the OH and
HO2, believed to be present only during
daytime when the sun provides UV photon fluxes, could be present
even in the nighttime at measurable concentrations, due to
the dark reactions of O3 with olefins
such as monoterpenes (C10H16),
a class of hydrocarbons mainly emitted from coniferous forests.
It is exciting to find that both marine and terrestrial ecosystems
could affect the radical chemistry near the Earth's surface.
Since an observational program for atmospheric composition
has not started in IORGC, the above works were conducted within
FRCGC mostly supported by outside grants including "Grant-in-aid
for Scientific Research" and "Research Revolution
2002"by MEXT. Kanaya mentions, "Although the atmospheric
chemistry mechanisms have recently been integrated into global
model simulations to predict future global warming, many parts
of them are still highly uncertain. For better prediction,
more observational studies are necessary to test and improve
the mechanisms, especially for those related to aerosol chemistry
and physics whose importance in the Earth's radiative budget
has widely been recognized."
