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Appl Environ Microbiol, May 1998, p. 1864-1870, Vol. 64, No. 5
Institute for the Study of Earth, Oceans and
Space, University of New Hampshire, Durham, New Hampshire
03824,1 and
Center for Chemical and
Environmental Physics, Aerodyne Research Inc., Billerica, Massachusetts
018212
Received 28 October 1997/Accepted 5 March 1998
A dynamic dilution system for producing low mixing ratios of methyl
bromide (MeBr) and a sensitive analytical technique were used to study
the uptake of MeBr by various soils. MeBr was removed within minutes
from vials incubated with soils and ~10 parts per billion by volume
of MeBr. Killed controls did not consume MeBr, and a mixture of the
broad-spectrum antibiotics chloramphenicol and tetracycline inhibited
MeBr uptake by 98%, indicating that all of the uptake of MeBr was
biological and by bacteria. Temperature optima for MeBr uptake
suggested a biological sink, yet soil moisture and temperature optima
varied for different soils, implying that MeBr consumption activity by
soil bacteria is diverse. The eucaryotic antibiotic cycloheximide had
no effect on MeBr uptake, indicating that soil fungi were not involved
in MeBr removal. MeBr consumption did not occur anaerobically. A
dynamic flowthrough vial system was used to incubate soils at MeBr
mixing ratios as low as those found in the remote atmosphere (5 to 15 parts per trillion by volume [pptv]). Soils consumed MeBr at all
mixing ratios tested. Temperate forest and grassy lawn soils consumed
MeBr most rapidly (rate constant [k] = 0.5 min
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Rapid Consumption of Low Concentrations of Methyl
Bromide by Soil Bacteria
1), yet sandy temperate, boreal, and tropical forest
soils also readily consumed MeBr. Amendments of CH4 up to
5% had no effect on MeBr uptake even at CH4:MeBr ratios of
107, and depth profiles of MeBr and CH4
consumption exhibited very different vertical rate optima, suggesting
that methanotrophic bacteria, like those presently in culture, do not
utilize MeBr when it is at atmospheric mixing ratios. Data acquired
with gas flux chambers in the field demonstrated the very rapid in situ consumption of MeBr by soils. Uptake of MeBr at mixing ratios found in
the remote atmosphere occurs via aerobic bacterial activity, displays
first-order kinetics at mixing ratios from 5 pptv to ~1 part per
million per volume, and is rapid enough to account for 25% of the
global annual loss of atmospheric MeBr.
*
Corresponding author. Present address: Department of
Biological Sciences, University of Alaska Anchorage, 3211 Providence Dr., Anchorage, AK 99508. Phone: (907) 786-7762. Fax: (907) 786-4607. E-mail: afmeh{at}uaa.alaska.edu.
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