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001 | 661637 | ||
005 | 20231030041753.0 | ||
035 | _a(RuTPU)RU\TPU\network\32335 | ||
090 | _a661637 | ||
100 | _a20200123a2018 k y0engy50 ba | ||
101 | 0 | _aeng | |
105 | _aa z 100zy | ||
135 | _adrcn ---uucaa | ||
181 | 0 | _ai | |
182 | 0 | _ab | |
200 | 0 |
_aBiodegradation in the Nkh 3-4 reservoir at Vankor Field (West Siberia Basin, Russia) is strongly controlled by rock properties _fN. V. Oblasov, I. V. Goncharov, V. V. Samoilenko (Samoylenko), V. G. G. Vidzhnandus |
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203 |
_aText _celectronic |
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300 | _aTitle screen | ||
320 | _a[References: 33 tit.] | ||
330 | _aThe Vankor Field, located in the West Siberia Basin, Russia, contains oils at various levels of biodegradation. A study of reservoir oils and rock extracts from the Lower Cretaceous sandstones in the Nkh 3-4 interval reveals that increasing biodegradation when moving from the gas-oil contact (GOC) towards the oil-water contact (OWC) is strongly controlled by rock properties. Biodegradation is most advanced where the OWC is located in the high permeability reservoir interval. High permeability rocks also allow for more extensive upward mixing of biodegraded oil. Changes in the oil and gas fractions due to biodegradation also affect the gas-oil ratio as dry gas is less soluble in heavy oil. This explains the presence of reservoir oil saturated with gas near the OWC. The latter also can be partly due to the admixture of methane through methanogenic processes at the OWC. Upward movement of microbial gas bubbles enhances the mixing of biodegraded oil in the high permeability reservoir intervals. | ||
333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
461 |
_tOrganic Geochemistry _d1977- |
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463 |
_tVol. 119 _v[P. 36-49] _d2018 |
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610 | 1 | _aтруды учёных ТПУ | |
610 | 1 | _aэлектронный ресурс | |
610 | 1 | _aVankor Field | |
610 | 1 | _aFluid properties | |
610 | 1 | _aBiodegradation | |
610 | 1 | _aPermeability | |
610 | 1 | _aGas-oil ratio | |
610 | 1 | _aOil saturation | |
610 | 1 | _aжидкости | |
610 | 1 | _aбиологическое разложение | |
610 | 1 | _aводопроницаемость | |
610 | 1 | _aнефтенасыщенность | |
701 | 1 |
_aOblasov _bN. V. _cgeologist _clead engineer of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences _f1981- _gNikolay Vladimirovich _2stltpush _3(RuTPU)RU\TPU\pers\34011 |
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701 | 1 |
_aGoncharov _bI. V. _cgeologist _cprofessor of Tomsk polytechnic university (TPU), doctor of geological and mineralogical sciences (DSc) _f1947- _gIvan Vasilyevich _2stltpush _3(RuTPU)RU\TPU\pers\30093 |
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701 | 1 |
_aSamoilenko (Samoylenko) _bV. V. _cgeochemist _cLeading engineer of Tomsk Polytechnic University, Candidate of geological-mineralogical sciences _f1981- _gVadim Valerievich _2stltpush _3(RuTPU)RU\TPU\pers\33274 |
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701 | 1 |
_aVidzhnandus _bV. G. G. _gVan Graas Gerardus |
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712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет _bИнженерная школа природных ресурсов _bОтделение геологии _h8083 _2stltpush _3(RuTPU)RU\TPU\col\23542 |
801 | 2 |
_aRU _b63413507 _c20200713 _gRCR |
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856 | 4 | _uhttps://doi.org/10.1016/j.orggeochem.2018.02.005 | |
942 | _cCF |