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Abstract - Issue Mar 2013, 34 (2) Back
nstantaneous and historical temperature effects on a-pinene
Carbon
isotope fractionation studies of bacterial strain
Rhodococcus
rhodochrous MTCC 291
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M.A.
Rasheed*, M. Lakshmi, P.L.S. Rao, M.S. Kalpana, D.J. Patil and A.M. Dayal
Microbiology
Laboratory, National Geophysical Research Institute, CSIR, Hyderabad-500 007,
India
*Corresponding
Author email : drrasheedmicro@gmail.com
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Publication
Data
Paper received:
30 August 2011
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Revised received:
05 April 2012
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Accepted:
26 May 2012
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Abstract
Carbon
isotope fractionation associated with the aerobic consumption of propane (C3)
were determined using Rhodococcus rhodochrous MTCC 291 bacterial
strain to estimate the amount of hydrocarbon oxidized using GC, fractionation
of δ13C
carbon isotopes of propane and CO2 using GC-C-IRMS and growth of bacteria by
UV-Visible Spectrophotometer. The initial δ13C isotopic value of propane
was -34 ‰ and after incubation the changes of the isotopic values have been
determined on 6th,
10th, 14th, and 17th days. The propane
isotopic fractionation value was found to be maximum of -38.0 ‰ with an
average value of -36.5 ‰ and a standard deviation of -1.22 ‰. The initial δ13C isotopic value of CO2 was -19.601 ‰. The CO2 isotopic fractionation
value was found to be maximum of -29.153 ‰ with an average value of -26.859 ‰
and a standard deviation of -28.338 ‰. The consumption of propane gas was
estimated using Gas Chromatograph. The initial concentration of propane in
control was found to be 53 ppm. On incubation, the consumption of the propane
gas was observed to be of 26 ppm. The carbon isotope fractionation presented
here may be applied to estimate the extent of C1-C4 oxidation in natural gas
samples, and should prove useful in further studying the microbial oxidation
of these compounds in the natural environment.
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Key words
Carbon
Isotope, Propane–oxidation, GC-C-IRMS, Rhodococcus rhodocrous MTCC 291
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