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Manifestation of the low-frequency dispersion of the earth electromagnetic properties in transient measurements for marine waters up to 100 m deep

https://doi.org/10.21285/2686-9993-2019-42-4-461-475

Abstract

The article presents a study of the low-frequency dispersion of the geological formations’ electromagnetic properties in transient measurements for the offshore areas with a depth of not more than 100 m. The research methods include calculation and analysis of the transient signal change, the finite difference of the transient signal, and the ratio of the two as a function of the electrical probe immersion depth. The probe consists of a source (a horizontal grounded electric line 500 m long) and a receiver (a three-electrode electric line 500 m long). The study has compared the values obtained at the submerged probes with those obtained at the surface probes. The values for the conducting and polarizable conducting models, obtained at the probes located at the same depth, have been also compared. The base polarizability has been included by introducing frequency-dependent electrical resistivity by the Cole-Cole formula. The calculations have shown a uniform distribution of the transient electric field in the conducting medium at the late stage, the transient signal being the same for the probes located at different depths. For a polarizable model base, the distribution of the transient signal at the late stage is non-uniform, the non-uniformity being a function of the distance to the base. Based on the calculations, it can be argued that with the sea depth of up to 100 m, the low-frequency dispersion of the geological formations for the given model is manifested at the electrical probe with the source length of 500 m on the entire depth range.

About the Authors

E. N. Vodneva
Limnological Institute, Siberian Branch of the Russian Academy of Sciences
Russian Federation

Lead Engineer

3 Ulan-Batorskaya St., Irkutsk 664033, Russia



E. V. Ageenkov
Irkutsk National Research Technical University
Russian Federation

Cand. Sci. (Geol. & Mineral.), Associate Professor, Department of Geology, Geophysics and Geoinformation Systems, Institute of Subsoil Use

83 Lermontov St., Irkutsk 664074, Russia



A. A. Sitnikov
Siberian Geophysical Research and Production Company
Russian Federation

CEO

9 Shapova St., Irkutsk 664044, Russia



References

1. of the Arctic States on the continental shelf of the Arctic. Yuridicheskii vestnik Dagestanskogo gosudarstvennogo universiteta = Law Нerald of Dagestan State University. 2017;24(4):104–108. (In Russ.)

2. Leont'ev OK. Ocean floor. Moscow: Mysl'; 1968. 320 p. (In Russ.)

3. Malovitskii YaP, Gagel'gants AA, Kogan LI, et al. Marine geophysical survey. Moscow: Nedra; 1977. 375 p. (In Russ.)

4. Edwards RN, Law LK, Wolfgram PA, Nobes DC, Bone MN, Trigg DF, et al. First results of the MOSES experiment: sea sediment conductivity and thickness determination, Bute Inlet, British Columbia, by magnetometric offshore electrical sounding. Geophysics. 1985;50(1):153–160.

5. Barsukov P, Fainberg E, Singer B. A method for hydrocarbon reservoir mapping and apparatus for use when performing the method. International patent WO 2007/053025; 2007.

6. Holten T, Flekkøy EG, Singer B, Blixt EM, Hanssen A, Måløy KJ. Vertical source, vertical receiver, electromagnetic technique for offshore hydrocarbon exploration. First Break. 2009;27(5):89–93.

7. Sitnikov AA, Ageenkov EV, Ivanov SA, Zhugan PP, Maltsev SKh. Equipment, devices and surveying systems to solve the proЬlems of oil and gas exploration and engineering geology in water areas with application of DNME and NDEMS electrical prospecting methods. Pribory i sistemy razvedochnoi geofiziki = Devices and Systems of Exploration Geophysics. 2017;60(2):42–49. (In Russ.)

8. Chave AD, Constable SC, Edwards RN. Electrical exploration methods for the seafloor. In: Nabighian MN (eds.). Electromagnetic Methods in Applied Geophysics. Tulsa: Society of Exploration Geophysicists; 1991. p.931–966.

9. Eidesmo T, Ellingsrud S, Macgregor LM, Constable S, Sinha MC, Johansen SE, et al. Sea bed logging (SBL), a new method for remote and direct identification of hydrocarbon filled layers in deepwater areas. First Break. 2002;20(3):144–152.

10. Constable S, Srnka LJ. An introduction to marine controlled source electromagnetic methods for hydrocarbon exploration. Geophysics. 2007;72(2):WA3–WA12. https://doi.org/10.1190/1.2432483

11. Veeken PCH, Legeydo PJ, Davidenko YuA, Kudryavceva EO, Ivanov SA, Chuvaev A. Benefits of the induced polarization geoelectric method to hydrocarbon exploration. Geophysics. 2009;74(2):B47–B59. https://doi.org/10.1190/1.3184802

12. Sidorov VA. Pulse inductive electrical exploration. Moscow: Nedra; 1985. 192 p. (In Russ.)

13. Vishnyakov AE, Lisitsyn ED, Yanevich MYu. The influence of IP time parameters of hydrocarbon deposits on the transient processes of the electromagnetic field. In: Rzhevskii NN, Kholmyanskii MA (eds.). Tekhnika i metodika geofizicheskikh issledovanii Mirovogo okeana = Technique and procedure of geophysical research on the World Ocean. Leningrad: Production geological association “Sevmorgeologiya”; 1988. p.124–132. (In Russ.)

14. Petrov AA. The potential of TEM for hydrocarbon exploration in shelf zones. Geofizika = Russian Geophysics. 2000;5:21–26. (In Russ.)

15. Legeido PYu, Mandel'baum MM, Rykhlinskii NI. Differential-normalized electrical survey method in direct hydrocarbon exploration. Geofizika = Russian Geophysics. 1995;4:42–45. (In Russ.)

16. Legeido PYu, Mandel'baum MM, Rykhlinskii NI. Selfdescriptiveness of differential methods of electrical survey in polarizable medium research. Geofizika = Russian Geophysics. 1997;3:49–56. (In Russ.)

17. Ageenkov EV, Sitnikov AA, Pesterev IYu. Display of induce polarization different types in electromagnetic measurements by the line. Geofizika = Russian Geophysics. 2018;2:37–43. (In Russ.)


Review

For citations:


Vodneva E.N., Ageenkov E.V., Sitnikov A.A. Manifestation of the low-frequency dispersion of the earth electromagnetic properties in transient measurements for marine waters up to 100 m deep. Earth sciences and subsoil use. 2019;42(4):461-475. (In Russ.) https://doi.org/10.21285/2686-9993-2019-42-4-461-475

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