nstantaneous and historical temperature effects on a-pinene
Characterization of light gaseous
hydrocarbons of the
surface soils of Krishna-Godavari basin, India
Author Details
M.Lakshmi
(Corresponding author)
Microbiology
Laboratory, National Geophysical Research Institute (CSIR), Uppal Road,
Hyderabad - 500 007, India
e-mail: lakshmi.kirla1220@gmail.com
M.A.Rasheed
Microbiology
Laboratory, National Geophysical Research Institute (CSIR), Uppal Road,
Hyderabad - 500 007, India
T.Madhavi
Microbiology
Laboratory, National Geophysical Research Institute (CSIR), Uppal Road,
Hyderabad - 500 007, India
M. S.Kalpana
Microbiology
Laboratory, National Geophysical Research Institute (CSIR), Uppal Road,
Hyderabad - 500 007, India
D.J.
Patil
Microbiology
Laboratory, National Geophysical Research Institute (CSIR), Uppal Road,
Hyderabad - 500 007, India
A.M.
Dayal
Microbiology
Laboratory, National Geophysical Research Institute (CSIR), Uppal Road,
Hyderabad - 500 007, India
Publication Data
Paper received:
25
September 2010
Revised
received:
13
January 2011
Accepted:
05 February 2011
Abstract
Several techniques are used
for the exploration of hydrocarbons, of which; the geochemical techniques
involving the microbiological technique use the principle of detecting the
light hydrocarbon seepage activities for indication of sub-surface petroleum
accumulations. A survey was carried out to characterize the light gaseous
hydrocarbons seeping in oil and gas fields of Krishna-Godavaribasin of Andhra Pradesh. A set of 50 sub-soil
samples were collected at depths of about 3 m for geochemical analyses and 1m
for microbiological analysis. The microbial prospecting
studies showed the presence of high bacterial population for methane 2.5 x 102
to 6.0 x 106 cfu g-1, propane
1x102 to 8.0 x 106 cfu g-1 in soil samples. The adsorbed
soil gas analysis showed the presence of moderate to low concentrations of
methane (26? to 139 ppb), ethane (0 to
17 ppb), propane (0 to 8 ppb),? butane
(0 to 5 ppb) and pentane (0 to 2 ppb) in the soil samples of the study area.
Carbon isotope analysis for methane (?13C1) ranging
from-36.6 to -22.7?? Pee Dee Belemnite (PDB) suggests
these gases are of thermogenic origin.
Geo-microbial prospecting method coupled with adsorbed soil gas and carbon
isotope ratio analysis have thus shown good correlation with existing oil/
gas fields of? Krishna-Godavari basin.
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