Proceedings of European Petroleum Conference 1988
DOI: 10.2523/18368-ms
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Studies on the Thermophilic Sulfate-Reducing Bacteria From a Souring North Sea Oil Field

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Cited by 9 publications
(14 citation statements)
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“…The optimum temperature for sulfate reduction in colder sediments was around 30°C. 88il°8 Cochrane et al 19 observed that the presence and growth of thermophilic SRB at temperatures greater than 60°C was a major source of sulfide production in a North Sea oil field. None of the presently known sulfate reducers is able to grow at extremely high temperatures near 100°C or below -5°C.…”
Section: Temperaturementioning
confidence: 99%
“…The optimum temperature for sulfate reduction in colder sediments was around 30°C. 88il°8 Cochrane et al 19 observed that the presence and growth of thermophilic SRB at temperatures greater than 60°C was a major source of sulfide production in a North Sea oil field. None of the presently known sulfate reducers is able to grow at extremely high temperatures near 100°C or below -5°C.…”
Section: Temperaturementioning
confidence: 99%
“…Samples for microbial analysis were collected in 500 ml sterilised glass Duran bottles after 0, 2, 6, 12, 30, 48, 60, 78 and 96 h backXowing from well A-42 and after ¡0. 5,1,4,8,24,36,54,72 and 95 h backXowing from well B-26. The sample collected at the time ¡0.5 h contained water that had reached well-bottom but not the reservoir.…”
Section: Samplingmentioning
confidence: 99%
“…The introduction of sea water alters the physical and chemical conditions in the reservoir as sulphate-rich sea water gradually cools the reservoir formation [1,2] and blends with the warm (60-200°C) indigenous reservoir water (formation water) which is low in sulphate and rich in organic acids [3][4][5]. The cooling of the reservoir formation creates a new biotope for mesophilic sea water bacteria in the near injector area.…”
Section: Introductionmentioning
confidence: 99%
“…Mesophilic, thermophilic and hyperthermophilic SRB´s can grow at different temperatures and therefore colonize different parts of the reservoir. (5) However, in most situations the reservoir harsh environment does not support expressive microbiological activity unless the cool-, deareated-, rich in sulfate-, and SRB-containing-seawater is allowed to penetrate the reservoir and create a moving front (interface) with the formation fluid. In fact, the cooling of the reservoir fluid and the drop in salinity promoted by the mixing of the two waters, the existence of low molecular weight fatty acids and the anaerobic conditions found in the reservoir, are the factors that can bring about a window for BRS colonies to settle downhole.…”
Section: How Does H 2 S Form? • Anthropogenic Souringmentioning
confidence: 99%
“…So, if the bisulfite dosage is well controlled it is very unlikely that it ends up being a major source of sulfate in the reservoir, although sulfite ions are more easily reduced than sulfate ions (to sulfide ions) by SRB. (5) On the Use of Mass Spectrometry Analysis to Identify the H 2 S Genesis MS is a useful analytical tool used to identify and quantify known chemical compounds. Detection of chemical species in very small quantities is one of the amazing features presented by this technique.…”
Section: Hso 3 -+ ½ O 2 So 4 = + H +mentioning
confidence: 99%