Golikov N.A.
golikovna@ipgg.sbras.ru
Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch Russian Academy of Sciences; Novosibirsk state university; Novosibirsk state technical university.Stratigraphy and lithology
| Article # 8_2025 | submitted on 11/12/2024 displayed on website on 02/24/2025 |
| 19 p. | Shumskayte M.Y., Yanushenko T.A., Golikov N.A. |
| Study of permafrost rocks of the Bykov peninsula by laboratory methods of dielectric spectroscopy and nuclear magnetic resonance | |
| The complex permittivity of sedimentary rocks mainly depends on the porosity and water saturation. For frozen rocks, the complex permittivity is also determined by the state of water in the pores. This is due to the difference in permittivity and electrical conductivity of free water and ice in the pores of the rock. In fine-porous rocks, the influence of bound water is great, the properties of which differ from the properties of free water. A study of the granulometric composition and specific electrical resistance of rocks was carried out on samples of permafrost rocks, and measurements were also made using the nuclear magnetic resonance method. Nuclear magnetic resonance is widely used in geological and geophysical studies to determine the filtration-capacitive properties of rocks and the rheological properties of formation fluids. It was found that the transformation of water into ice with a decrease in temperature does not occur at a certain temperature, but in a certain range of negative temperatures. It was found that the dielectric constant changes by approximately 6 for different wells. According to NMR data, a connection was established between water saturation and granulometric composition and the dependence of the transverse relaxation time on the degree of mineralization and temperature of rocks. Keywords: complex permittivity, NMR relaxometry, permafrost rock, Bykov peninsula. |
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| article citation | Shumskayte M.Y., Yanushenko T.A. Golikov N.A. Izuchenie mnogoletnemerzlykh porod Bykovskogo poluostrova laboratornymi metodami dielektricheskoy spektroskopii i yadernogo magnitnogo rezonansa [Study of permafrost rocks of the Bykov peninsula by laboratory methods of dielectric spectroscopy and nuclear magnetic resonance]. Neftegazovaya Geologiya. Teoriya I Praktika, 2025, vol. 20, no. 1, available at: https://www.ngtp.ru/rub/2025/8_2025.html EDN: OORYLZ |
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Dzhafarov I.S., Syngaevskiy P.E., Khafizov S.F. Primenenie metoda yadernogo magnitnogo rezonansa dlya kharakteristiki svoystva i raspredeleniya plastovykh flyuidov [Nuclear magnetic resonance application for reservoir fluids distribution and properties characterization]. Moscow: Khimiya, 2002, 439 p. (In Russ.).
Epov M.I., Savin I.V., Mironov V.L. Dielektricheskaya temperaturnaya model' vlazhnykh neftesoderzhashchikh porod v diapazone chastot ot 0,5 do 15 GGts [Dielectric temperature model of wet oil-bearing rocks in the frequency range from 0.5 to 15 GHz]. Geologiya i geofizika, 2012, no. 7, pp. 912-919. (In Russ.). DOI: 10.1016/j.rgg.2012.05.008
Fleury M., Deflandre F., Godefroy S. Validity of permeability prediction from NMR measurements. Comptes Rendus de l'Académie des Sciences, Chemistry, 2001, no. 4, pp. 869-872. DOI: 10.1016/S1387-1609(01)01343-3
Freedman R., Heaton N. Fluid characterization using nuclear magnetic resonance logging. Petrophysics, 2004, no. 45, pp. 241-250.
Freedman R., Heaton N., Flaum M., Hirasaki G, Flaum C, Hurlimann M. Wettability saturation and viscosity from NMR measurements. SPE Journal, 2003, no. 8, pp. 317-327. DOI: 10.2118/87340-PA
Repin A.V., Bobrov P.P., Golikov N.A. Dielectricheskaya pronicaemost’ neftevodonasyshchennykh kernov bazhenovskoy svity [Dielectric constant of oil-saturated cores of the Bazhenov Formation]. Aktualnye problemy geologii nefti I gaza Sibiri: materialy Vserossiyskoy nauchnoy konferencii molodykh uchenykh I studentov, posvyashch. 80-letiyu akad. A.E. Kontorovicha (Novosibirsk, 10-15 Feb 2014). INGG SO RAN: Novosibirsk, 2014, pp. 228-231. (In Russ.).
Shumskayte M., Junasheva A., Eltsov T., Golikov N. Electrophysical parameters and NMR-characteristics of cryogel. IOP Conference Series: Earth and Environment Science, 2016, vol. 43, Paper 012021, 7 p. DOI: 10.1088/1755-1315/43/1/012021
Shumskayte M.Y., Glinskikh V.N. Analiz vliyaniya ob"emnogo soderzhaniya i tipa glinistykh mineralov na relaksatsionnye kharakteristiki peschano-alevritovykh obraztsov kerna [Analysis of the effect of volumetric content and the type of clay minerals on relaxation characteristics of sandy-aleuritic core samples]. Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2015, no. 7, pp. 35-38 (In Russ.). EDN: UAPYRX
Shumskayte M.Y., Glinskikh V.N. Eksperimental'noe issledovanie zavisimosti YAMR-kharakteristik ot udel'noy poverkhnosti i udel'nogo elektricheskogo soprotivleniya peschano-alevritoglinistykh obraztsov [Relation of NMR parameters with specific surface and resistivity of shaly sandstone and siltstone samples: experimental study]. Geologiya i geofizika, 2016, vol. 57, no. 10, pp. 1911-1918. (In Russ.). DOI: 10.15372/GiG20161009
Sudakova M.S., Vladov M.L. Experimentalnoe issledovanie akusticheskikh svoystv vodonasyshchennogo peska v interval temperatury ot –20 до +20ᵒС [Experimental study of the acoustic properties of water-saturated sand in the temperature range from –20 до +20ᵒС]. Vestnik Moskovskogo universiteta. Seriya 4. Geologiya, 2019, no. 4, pp. 55-62. (In Russ.). DOI: 10.33623/0579-9406-2019-4-55-62
Tabarin V.A., Dem’yanceva S.D. Opredelenie soderzhaniya svyazannoy vody v kernakh na SVCh [Determination of bound water content in cores using microwave]. Neftegazovoe delo, 2009, vol. 7, no. 1, pp. 1-28. (In Russ.).