1887
image of Review paper: Instrumentation for marine magnetotelluric and controlled source electromagnetic sounding

Abstract

ABSTRACT

We review and describe the electromagnetic transmitters and receivers used to carry out magnetotelluric and controlled source soundings in the marine environment. Academic studies using marine electromagnetic methods started in the 1970s but during the last decade these methods have been used extensively by the offshore hydrocarbon exploration industry. The principal sensors (magnetometers and non‐polarizing electrodes) are similar to those used on land but magnetotelluric field strengths are not only much smaller on the deep sea‐floor but also fall off more rapidly with increasing frequency. As a result, magnetotelluric signals approach the noise floor of electric field and induction coil sensors (0.1 nV/m and 0.1 pT) at around 1 Hz in typical continental shelf environments. Fluxgate magnetometers have higher noise than induction coils at periods shorter than 500 s but can still be used to collect sea‐floor magnetotelluric data down to 40–100 s. Controlled source transmitters using electric dipoles can be towed continuously through the seawater or on the sea‐bed, achieving output currents of 1000 A or more, limited by the conductivity of seawater and the power that can be transmitted down the cables used to tow the devices behind a ship. The maximum source‐receiver separation achieved in controlled source soundings depends on both the transmitter dipole moment and on the receiver noise floor and is typically around 10 km in continental shelf exploration environments. The position of both receivers and transmitters needs to be navigated using either long baseline or short baseline acoustic ranging, while sea‐floor receivers need additional measurements of orientations from compasses and tiltmeters. All equipment has to be packaged to accommodate the high pressure (up to 40 MPa) and corrosive properties of seawater. Usually receiver instruments are self‐contained, battery powered and have highly accurate clocks for timekeeping, even when towed on the sea‐floor or in the water column behind a transmitter.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.2012.01117.x
2013-01-29
2024-04-24
Loading full text...

Full text loading...

References

  1. BeckerK., VonHerzenR.P., FrancisT.J.G., AndersonR.N., HonnorezJ. and AdamsonA.C. et al. 1982. In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica Rift. Nature 300, 594–598.
    [Google Scholar]
  2. BrownT.F. and CoxC.S.1973. Design of light, cylindrical pressure cases. Engineering Journal 2, 35–37.
    [Google Scholar]
  3. CheesmanS.J., LawL.K. and St. LouisB.1993. A porosity mapping survey in Hecate Straight using a seafloor electro‐magnetic profiling system. Marine Geology 110, 245–256.
    [Google Scholar]
  4. ConstableS.C.1990. Marine electromagnetic induction studies. Surveys in Geophysics 11, 303–327.
    [Google Scholar]
  5. ConstableS. and CoxC.S.1996. Marine controlled source electromagnetic sounding 2. The PEGASUS experiment. Journal of Geophysical Research 101, 5519–5530.
    [Google Scholar]
  6. ConstableC.G. and ConstableS.C.2004. Satellite magnetic field measurements: Applications in studying the deep Earth. In: The State of the Planet: Frontiers and Challenges in Geophysics, Geophysical Monograph 150 , (eds R.S.J.Sparks and C.T.Hawkesworth ), pp. 147–159. American Geophysical Union.
    [Google Scholar]
  7. ConstableS. and HeinsonG.2004. Hawaiian hot‐spot swell structure from seafloor MT sounding. Tectonophysics 389, 111–124.
    [Google Scholar]
  8. ConstableS., HeinsonG., AndersonG. and WhiteA.1997. Seafloor electromagnetic measurements above Axial Seamount, Juan de Fuca Ridge. Journal of Geomagnetism and Geoelectricity 49, 1327–1342.
    [Google Scholar]
  9. ConstableS., KeyK. and LewisL.2009. Mapping offshore sedimentary structure using electromagnetic methods and terrain effects in marine magnetotelluric data. Geophysical Journal International 176, 431–442.
    [Google Scholar]
  10. ConstableS., OrangeA., HoverstenG.M. and MorrisonH.F.1998. Marine magnetotellurics for petroleum exploration Part 1. A sea‐floor instrument system. Geophysics 63, 816–825.
    [Google Scholar]
  11. ConstableS. and SrnkaL.J.2007. An introduction to marine controlled source electromagnetic methods for hydrocarbon exploration. Geophysics 72, WA3–WA12.
    [Google Scholar]
  12. ConstableS. and WeissC.J.2005. Mapping thin resistors (and hydrocarbons) with marine EM methods: Insights from 1D modeling. Geophysics 71, G43–G51.
    [Google Scholar]
  13. CorwinR.F.1973. Offshore Application of Self‐potential Prospecting . PhD thesis, University of California, Berkeley (available as Scripps Institution of Oceanography Library, Paper 22, http://repositories.cdlib.org/sio/lib/22).
  14. CoxC.S.1980. Electromagnetic induction in the oceans and inferences on the constitution of the earth. Geophysical Surveys 4, 137‐156.
    [Google Scholar]
  15. CoxC.S., ConstableS.C., ChaveA.D. and WebbS.C.1986. Controlled source electromagnetic sounding of the oceanic lithosphere. Nature 320, 52–54.
    [Google Scholar]
  16. CoxC.S., DeatonT.K. and PistekP.1981. An active source EM method for the seafloor . Scripps Institution of Oceanography Technical Report, http://escholarship.org/uc/item/7dr96489, accessed 25 May 2010.
    [Google Scholar]
  17. CoxC.S., FillouxJ.H. and LarsenJ.C.1971. Electromagnetic studies of ocean currents and electrical conductivity below the ocean floor. In: The Sea , Vol. 4Part I, (ed. A.E.Maxwell ), pp. 637–693. Wiley–Interscience, New York .
    [Google Scholar]
  18. CronaL., FristedtT., LundbergP. and SigrayP.2001. Field tests of a new type of graphite‐fiber electrode for measuring motionally induced voltages. Journal of Atmospheric and Oceanic Technology 18, 92–99.
    [Google Scholar]
  19. EllingsrudS., EidesmoT., JohansenS., SinhaM.C., MacGregorL.M. and ConstableS.2002. Remote sensing of hydrocarbon layers by seabed logging (SBL): Results from a cruise offshore Angola. The Leading Edge 21, 972–982.
    [Google Scholar]
  20. EvansR.L.2007. Using CSEM techniques to map the shallow section of seafloor: From the coastline to the edges of the continental slope. Geophysics 72, WA105–WA116.
    [Google Scholar]
  21. EvansR.L., ConstableS.C., SinhaM.C. and CoxC.S.1991. Upper crustal resistivity structure of! the East Pacific Rise near 13°N. Geophysical Research Letters 18, 1917–1920.
    [Google Scholar]
  22. EvansR.L., TaritsP., ChaveA.D., WhiteA., HeinsonG., FillouxJ.H. et al.1999. Asymmetric electrical structure in the mantle beneath the East Pacific rise at 17 degrees S. Science 286, 752–756.
    [Google Scholar]
  23. FillouxJ.H.1967. An ocean bottom, D component magnetometer. Geophysics 6, 978–987.
    [Google Scholar]
  24. FillouxJ.H.1974. Electric field recording on the sea floor with short span instruments. Journal of Geomagnetism and Geoelectricity 26, 269–279.
    [Google Scholar]
  25. FillouxJ.H.1987. Instrumentation and experimental methods for oceanic studies. In: Geomagnetism , (ed. J.A.Jacobs ), pp. 143–248. Academic Press.
    [Google Scholar]
  26. GoldmanM., LeviE., TezkanB. and YogeshwarP.2011. The 2D coastal effect on marine time domain electromagnetic measurements using broadside dBz/dt of an electrical transmitter dipole. Geophysics 76, F101–F109.
    [Google Scholar]
  27. GotoT., KasayaT., MachiyamaH., TakagiR., MatsumotoR., OkudaY. et al.2008. A marine deep‐towed DC resistivity survey in a methane hydrate area, Japan Sea. Exploration Geophysics 39, 52–59.
    [Google Scholar]
  28. HeinsonG., ConstableS. and WhiteA.1996. Seafloor magnetotelluric sounding above Axial seamount. Geophysical Research Letters 23, 2275–2278.
    [Google Scholar]
  29. HeinsonG., ConstableS. and WhiteA.2000. Episodic melt transport at a mid‐ocean ridge inferred from magne‐ totelluric sounding. Geophysical Research Letters 27, 2317–2320.
    [Google Scholar]
  30. HeinsonG.S., WhiteA., LawL.K., HamanoY., UtadaH., YukutakeJ. et al.1993. EMRIDGE: The electromagnetic investigation of the Juan de Fuca Ridge. Marine Geophysical Researches 5, 77–100.
    [Google Scholar]
  31. HoehnG.L. and WarnerB.N.1983. Magnetotelluric measurements in the Gulf of Mexico at 20 m ocean depths. In: CRC Handbook of Geophysical Exploration at Sea , (ed. R.A.Geyer ), pp. 397–416. CRC Press, Boca Raton.
    [Google Scholar]
  32. HoverstenG.H., ConstableS. and MorrisonH.F.2000. Marine magnetellurics for base salt mapping: Gulf of Mexico field‐test at the Gemini structure. Geophysics 65, 1476–1488.
    [Google Scholar]
  33. IronsH.R. and SchweeL.J.1972. Magnetic thin‐film magnetometers for magnetic‐field measurement. IEEE Transactions on Magnetics , MAG‐8, 61–65.
    [Google Scholar]
  34. JegenM. and EdwardsR.N.1998. The electrical properties of a 2D conductive zone under the Juan de Fuca Ridge. Geophysical Research Letters 25, 3647–3650.
    [Google Scholar]
  35. JosephE.J., TohH., FujimotoH., IyengarR.V., SinghB.P., UtadaH. and SegawaJ.2000. Seafloor electromagnetic induction studies in the Bay of Bengal. Marine Geophysical Researches 21, 1–21.
    [Google Scholar]
  36. KeyK.W.2003. Application of Broadband Marine Magnetotelluric Exploration to a 3D Salt Structure and a Fast‐Spreading Ridge . PhD thesis, University of California San Diego.
  37. KeyK.2009. 1D inversion of multicomponent, multifrequency marine CSEM data: Methodology and synthetic studies for resolving thin resistive layers. Geophysics 74, F9–F20.
    [Google Scholar]
  38. KeyK.W., ConstableS.C. and WeissC.J.2006. Mapping 3D salt using 2D marine MT: Case study from Gemini Prospect, Gulf of Mexico. Geophysics 71, B17–B27.
    [Google Scholar]
  39. KeyK. and LockwoodA.2010. Determining the orientation of marine CSEM receivers using orthogonal Procrustes rotation analysis. Geophysics 75, F63–F70.
    [Google Scholar]
  40. KnappeS., GerginovV., SchwindtP.D.D., ShahV., RobinsonH.G., HollbergL. and KitchingJ.2005. Atomic vapor cells for chip‐scale atomic clocks with improved long‐term frequency stability. Optics Letters 30, 2351–2353.
    [Google Scholar]
  41. LawL.K.1978. An ocean bottom magnetometer: Design and first deployment near the Explorer Ridge (abstract). Eos Transactions of the AGU 59, 235.
    [Google Scholar]
  42. LawL.K. and GreenhouseJ.P.1981. Geomagnetic‐variation sounding of the asthenosphere beneath the Juan‐de Fuca Ridge. Journal of Geophysical Research 86, 967–978.
    [Google Scholar]
  43. LuX. and SrnkaL.J.2005. Logarithmic spectrum transmitter waveform for controlled‐source electromagnetic surveying. United States Patent 7539279.
  44. MattssonJ., LundL., LimaJ., EngelmarkF. and McKayA.2010. Case study: A towed EM test at the Peon discovery in the North Sea. Contributed paper at EAGE Meeting, pages 1–5.
  45. MittetR., AakervikO.M., JensenH.R., EllingsrudS. and StovasA.2007. On the orientation and absolute phase of marine CSEM receivers. Geophysics 72, F145–F155.
    [Google Scholar]
  46. MittetR. and Schaug‐PettersenT.2008. Shaping optimal transmitter waveforms for marine CSEM surveys. Geo- physics 73, F97–F104.
    [Google Scholar]
  47. MüllerH., vonDobeneck T., HilgenfeldtC., SanFilipoB., ReyD. and RubioB.2012. Mapping the magnetic susceptibility and electric conductivity of marine surficial sediments by benthic EM profiling. Geophysics 77, E43–E56.
    [Google Scholar]
  48. MüllerH., vonDobeneck T., NehmizW. and HamerK.2011. Near‐surface electromagnetic, rock magnetic, and geochemical fingerprinting of submarine freshwater seepage at Eckernforde Bay (SW Baltic Sea). Geo-Marine Letters 31, 123–140.
    [Google Scholar]
  49. MyerD., ConstableS. and KeyK.2011. Broad‐band waveforms and robust processing for marine CSEM surveys. Geophysical Journal International 184, 689–698.
    [Google Scholar]
  50. MyerD., ConstableS. and KeyK.2012. Marine CSEM survey of the Scarborough gas field, Part 1: Experimental design and data uncertainty. Geophysics 77, E281–E299.
    [Google Scholar]
  51. OrangeA., KeyK. and ConstableS.2009. The feasibility of reservoir monitoring using time‐lapse marine CSEM. Geophysics 74, F21–F29.
    [Google Scholar]
  52. PerkinR.G. and WalkerE.R.1972. Salinity calculations from in situ measurements. Journal of Geophysical Research 77, 6618–6621.
    [Google Scholar]
  53. PoehlsK.A. and VonHerzen R.P.1976. Electrical resistivity structure beneath the North‐west Atlantic Ocean. Geophysical Journal of the Royal Astronomical Society 47, 331–346.
    [Google Scholar]
  54. RipkaP.1992. Review of fluxgate sensors. Sensors and Actuators A 33, 129–141.
    [Google Scholar]
  55. RosaE.B.1908. The Self and Mutual Inductances of Linear Conductors. Bulletin of the Bureau of Standards 4, 301.
    [Google Scholar]
  56. SchwalenbergK. and EngelsM.2011. Marine controlled source electromagnetic methods for gas hydrate assessment: New instrumentation and first field applications. Contributed paper at Proceedings of the 7th International Conference on Gas Hydrates, Edinburgh, UK, July, pp. 17–21.
  57. SchwalenbergK., HaeckelM., PoortJ. and JegenM.2010. Evaluation of gas hydrate deposits in an active seep area using marine controlled source electromagnetics: Results from Opouawe Bank, Hikurangi Margin, New Zealand. Marine Geology 272, 79–88.
    [Google Scholar]
  58. SchwalenbergK., WilloughbyE., MirR. and EdwardsR.N.2005. Marine gas hydrate electromagnetic signatures in Cascadia and their correlation with seismic blank zones. First Break 23, 57–63.
    [Google Scholar]
  59. SegawaJ. and TohH.1992. Detecting fluid circulation by electric‐field variations at the Nankai Trough. Earth and Planetary Science Letters 109, 469–476.
    [Google Scholar]
  60. SinhaM.C., NavinD.A., MacGregorL.M., ConstableS., PeirceC., WhiteA. et al.1996. Evidence for accumulated melt beneath the slow‐spreading mid‐Atlantic ridge. Philosophical Transactions A Royal Society 355, 233–253.
    [Google Scholar]
  61. SinhaM.C., PatelP.D., UnsworthM.J., OwenT.R.E. and MacCormackM.R.J.1990. An active source EM sounding system for marine use. Marine Geophysical Research 12, 59–68.
    [Google Scholar]
  62. SpiessF.N. and MudieJ.D.1970. Small‐scale topographic and magnetic features. In: The Sea , Vol. 4 Part I (ed. A.E.Maxwell ), pp. 637–693. Wiley–Interscience, New York .
    [Google Scholar]
  63. SpiessF.N. and TyceT.C.1973. Marine Physical Laboratory Deep Tow Instrument System. Scripps Institution of Oceanography Reference 73–74, 37 pp.
  64. SundeE.D.1949. Earth Conduction Effects in Transmission Systems . D. Van Nostrand, New York .
    [Google Scholar]
  65. TohH., GotoT. and HamanoY.1998. A new seafloor electromagnetic station with an Overhauser magnetometer, a magnetotelluric variograph and an acoustic telemetry modem. Earth, Planets and Space 50, 895–903.
    [Google Scholar]
  66. TumanskiS.2007. Induction coil sensors – A review. Measurement Science and Technology 18, R31–R46.
    [Google Scholar]
  67. WebbS.C., ConstableS.C., CoxC.S. and DeatonT.K.1985. A sea‐floor electric field instrument. Geomagnetism and Geoelectricity 37, 1115–1129.
    [Google Scholar]
  68. WeitemeyerK.A.2008. Marine Electromagnetic Methods for Gas Hydrate Characterization . PhD thesis, University of California, San Diego (available as Scripps Institution of Oceanography Technical Report, http://repositories.cdlib.org/sio/techreport/91.
  69. WeitemeyerK. and ConstableS.2010. Mapping shallow geology and gas hydrate with marine CSEM surveys. First Break 28, 97–102.
    [Google Scholar]
  70. WeitemeyerK.A., ConstableS.C., KeyK.W. and BehrensJ.P.2006. First results from a marine controlled‐source electromagnetic survey to detect gas hydrates offshore Oregon. Geophysical Research Letters 33, L03304, doi:10.1029/2005GL024896.
    [Google Scholar]
  71. WheelerH.A.1928. Simple inductance formulas for radio coils. Proceedings of the Institute of Radio Engineering , 16, 1398–1400.
    [Google Scholar]
  72. WhiteA.1979. A sea floor magnetometer for the continental shelf. Marine Geophysical Researches 4, 105–114.
    [Google Scholar]
  73. WorzewskiT., JegenM., KoppH., BrasseH. and CastilloW.T.2011. Magnetotelluric image of the fluid cycle in the Costa Rican subduction zone. Nature Geoscience 4, 108–111.
    [Google Scholar]
  74. YuanJ. and EdwardsR.N.2000. The assessment of marine gas hydrates through electrical remote sounding: Hydrate without a BSR? Geophysical Research Letters 27, 2397–2400.
    [Google Scholar]
  75. ZiolkowskiA., ParrR., WrightD., NocklesV., LimondC., MorrisE. and LinfootJ.2010. Multi‐transient electromagnetic repeatability experiment over the North Sea Harding field. Geophysical Prospecting 58, 1159–1176.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.2012.01117.x
Loading
/content/journals/10.1111/j.1365-2478.2012.01117.x
Loading

Data & Media loading...

  • Article Type: Research Article
Keywords: Magnetotelluric ; Magnetometers ; Electromagnetic
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error