Tn. Nazina et al., MICROBIOLOGICAL AND GEOCHEMICAL CHARACTERIZATION OF CARBONATE OIL COLLECTORS OF TATARSTAN, Microbiology (New York), 67(5), 1998, pp. 575-581
Regularities in the distribution of microorganisms were studied in the
carbonate oil collectors of the Romashkinskoe and Bavlinskoe oil fiel
ds differing in hydrochemical conditions. In the Turneiskii stratum of
the Bavlinskoe oil field flooded with fresh river water, the greatest
diversity and activity of microflora were observed in the near-bottom
zone of injection wells. In this zone, anaerobic microflora was repre
sented by fermentative (10(4) cells/ml), sulfate-reducing (10(4) to 10
(5) cells/ml), and methanogenic (10(2) to 10(4) cells/ml) bacteria; th
e number of aerobic bacteria was low. The sulfate reduction rate reach
ed 237.5 mu g H2S/(1 day). Analysis of samples of oil-water emulsion f
rom producing wells showed a scarce microbial population in the Turnei
skii stratum. In the Serpukhovskoi stratum (bed 303) of the Romashkins
koe oil field, which has been exploited without flooding, the reduced
environment prevented the development of aerobic microorganisms: sapro
trophs growing on nutrient agar were detected only in two out of nine
samples; hydrocarbon oxidizers were absent. Among anaerobes, most nume
rous were fermentative (10-10(4) cells/ml) and sulfate-reducing (10(2)
-10(4) cells/ml) bacteria. In bed 303, we recorded contemporary proces
ses of sulfate reduction and methanogenesis. The sulfate reduction rat
e did not exceed 17.1 mu g S2-/(1 day). Methane was produced mainly fr
om bicarbonate (0.009-0.199 mu g CH4/(1 day). Methanogenesis from acet
ate was detected in only two water samples, where its rate was 0.004 a
nd 0.023 mu g CH4/(1 day). Thus, the carbonate collectors studied cont
ained fermentative microflora, and this is a factor calling for the em
ployment of microbiological methods for the enhancement of oil recover
y.