| Literature DB >> 28620357 |
Navreet Suri1, Johanna Voordouw1, Gerrit Voordouw1.
Abstract
The injection of nitrate is one of the most commonly used technologies to impact the sulfur cycle in subsurface oil fields. Nitrate injection enhances the activity of nitrate-reducing bacteria, which produce nitrite inhibiting sulfate-reducing bacteria (SRB). Subsequent reduction of nitrate to di-nitrogen (N2) alleviates the inhibition of SRB by nitrite. It has been shown for the Medicine Hat Glauconitic C (MHGC) field, that alkylbenzenes especially toluene are important electron donors for the reduction of nitrate to nitrite and N2. However, the rate and extent of reduction of nitrate to nitrite and of nitrite to nitrogen have not been studied for multiple oil fields. Samples of light oil (PNG, CPM, and Tundra), light/heavy oil (Gryphon and Obigbo), and of heavy oil (MHGC) were collected from locations around the world. The maximum concentration of nitrate in the aqueous phase, which could be reduced in microcosms inoculated with MHGC produced water, increased with the toluene concentration in the oil phase. PNG, Gryphon, CPM, Obigbo, MHGC, and Tundra oils had 77, 17, 5.9, 4.0, 2.6, and 0.8 mM toluene, respectively. In incubations with 49 ml of aqueous phase and 1 ml of oil these were able to reduce 22.2, 12.3, 7.9, 4.6, 4.0, and 1.4 mM of nitrate, respectively. Nitrate reduced increased to 35 ± 4 mM upon amendment of all these oils with 570 mM toluene prior to incubation. Souring control by nitrate injection requires that the nitrate is directed toward oxidation of sulfide, not toluene. Hence, the success of nitrate injections will be inversely proportional to the toluene content of the oil. Oil composition is therefore an important determinant of the success of nitrate injection to control souring in a particular field.Entities:
Keywords: nitrate; nitrate-reducing bacteria; oil fields; souring control; toluene
Year: 2017 PMID: 28620357 PMCID: PMC5450463 DOI: 10.3389/fmicb.2017.00956
Source DB: PubMed Journal: Front Microbiol ISSN: 1664-302X Impact factor: 5.640
Physicochemical properties of oil samples used in this study.
| Oil | Field information; location | API gravity | Viscosity (cP) at 20°C∗ | Designation |
|---|---|---|---|---|
| PNG | Conventional oil field; Papua New Guinea | 46° | 9.4 | Light |
| CPM | Shale oil field in the Bakken formation; Saskatchewan, Canada | 41° | 10.8 | Light |
| Tundra | Shale oil field in the Bakken formation; Manitoba, Canada | 38° | 11.8 | Light |
| Gryphon | Shale oil field; Alberta, Canada | 31° | 16.6 | Light/Heavy |
| Obigbo | Obigbo field; Nigeria | 21° | 50.9 | Light/Heavy |
| MHGC | Conventional oil reservoir; Medicine Hat, Alberta, Canada | 16° | 2471 | Heavy |
Maximum concentrations of nitrate reduced and nitrite produced at the end of incubations in serum bottles with 2% (v/v) of oil and in Hungate tubes with 6.7% (v/v) of oil.
| Oil | 2% (v/v) of oil | 6.7% (v/v) of oil | Fold increase in nitrate reduced | ||||||
|---|---|---|---|---|---|---|---|---|---|
| Nitrate reduced (mM) | Nitrite formed (mM) | Theoretical maximum toluene contribution (%) | N | Nitrate reduced (mM) | Nitrite formed (mM) | Theoretical maximum toluene contribution (%) | |||
| PNG | 6 | 22.2 ± 1.1 | 9.5 ± 7.3 | 68 | 2 | 80.0 ± 0ˆ* | 39.7 ± 3.2 | 66 | 3.6 |
| Gryphon | 6 | 12.3 ± 1.6 | 3.9 ± 2.7 | 25 | 4 | 41.7 ± 5.2 | 32.3 ± 6.4 | 37 | 3.4 |
| CPM | 8 | 7.9 ± 0.6 | 2.6 ± 0.7 | 13 | 4 | 27.7 ± 0.8 | 23.2 ± 2.2 | 21 | 3.5 |
| Obigbo | 8 | 4.6 ± 0.7 | 1.4 ± 0.2 | 15 | 6 | 16.2 ± 3.4 | 14.8 ± 1.9 | 26 | 3.2 |
| MHGC | 8 | 4.0 ± 1.5 | 0.7 ± 0.2 | 11 | 6 | 12.5 ± 2.1 | 8.7 ± 1.3 | 17 | 2.2 |
| Tundra | 8 | 1.4 ± 0.6 | 0.4 ± 0.1 | 10 | 8 | 6.9 ± 3.2 | 1.2 ± 1.1 | 6 | 4.9 |
Microbial community compositions of hNRB enrichments.
| Cluster I | Cluster II | |||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| #Taxonomy (Class; Order; Family; Genus) | Average | Tundra_N3 | Gryphon_N3 | CPM_N3 | PNG_N3 | Obigbo_N3 | MHGC_N3 | PNG_N2 | Gryphon_N1 | CPM_N1 | Tundra_0 | Obigbo_0 | MHGC_0 | Gryphon_0 | PNG_0 | CPM_0 |
| Betaproteobacteria; Rhodocyclales; Rhodocyclaceae; Thauera | ||||||||||||||||
| Gammaproteobacteria; Pseudomonadales; Pseudomonadaceae; Pseudomonas | 0.4 | 0.3 | ||||||||||||||
| Sphingobacteriia; Sphingobacteriales; WCHB1-69 | 0.7 | 0.5 | 0.6 | 0.4 | 0.3 | |||||||||||
| Methanomicrobia; Methanosarcinales; Methanosaetaceae; Methanosaeta | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.1 | 0.0 | 0.0 | ||||||
| Methanomicrobia; Methanomicrobiales; Methanomicrobiales-Incertae-Sedis; Methanocalculus | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.4 | 0.0 | ||||||||
| Deferribacteres; Deferribacterales; Deferribacteraceae | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.1 | 0.0 | 0.3 | 0.9 | 0.5 | ||||
| Bacteroidia; Bacteroidales; Porphyromonadaceae; Proteiniphilum | 0.7 | 0.4 | 0.1 | 0.2 | ||||||||||||
| Anaerolineae; Anaerolineales; Anaerolineaceae | 0.3 | 0.2 | 0.1 | 0.0 | 0.6 | |||||||||||
| Clostridia; Clostridiales; Eubacteriaceae; Acetobacterium | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.1 | ||||
| Deltaproteobacteria; Syntrophobacterales; Syntrophaceae; Smithella | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.6 | 0.0 | 0.5 | ||||
| Methanomicrobia; Methanomicrobiales; Methanomicrobiaceae; Methanoculleus | 0.4 | 0.1 | 0.5 | 0.0 | 0.0 | 0.2 | 0.3 | 0.7 | 0.1 | 0.4 | ||||||
| Clostridia; Clostridiales; Peptococcaceae | 0.0 | 0.0 | 0.0 | 0.0 | 0.1 | 0.0 | 0.0 | 0.1 | 0.0 | 0.8 | 0.2 | 0.0 | ||||