Electromagnetic surveying for hydrocarbon reservoirs
AssigneeStatoil ASA
InventorsLucy M MacGregor, Martin C Sinha
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AssigneeStatoil ASA
InventorsLucy M MacGregor, Martin C Sinha
Estimating the term…
An electromagnetic survey method for surveying an area previously identified as potentially containing a subsea hydrocarbon reservoir, comprising obtaining first and second survey data sets with an electromagnetic source aligned end-on and broadside relative to the same or different receivers. The invention also relates to planning a survey using this method, and to analysis of survey data taken in combination allow the galvanic contribution to the signals collected at the receiver to be contrasted with the inductive effects, and the effects of signal attenuation, which are highly dependent on local properties of the rock formation, overlying water and air at the survey area. This is very important to the success of using electromagnetic surveying for identifying hydrocarbon reserves and distinguishing them from other classes of structure.
An electromagnetic survey method for surveying an area previously identified as potentially containing a subsea hydrocarbon reservoir, comprising:
An electromagnetic survey method for surveying an area previously identified as potentially containing a subsea hydrocarbon reservoir, comprising:
A method of planning an electromagnetic survey of an area identified as potentially containing a subsea hydrocarbon reservoir, comprising:
A method of planning an electromagnetic survey of an area identified as potentially containing a subsea hydrocarbon reservoir, comprising:
A computer program product bearing machine readable instructions for implementing a method of planning an electromagnetic survey of an area identified as potentially containing a subsea hydrocarbon reservoir, comprising:
A computer apparatus loaded with machine readable instructions for implementing a method of planning an electromagnetic survey of an area identified as potentially containing a subsea hydrocarbon reservoir, comprising:
A computer program product bearing machine readable instructions for implementing a method of planning an electromagnetic survey of an area identified as potentially containing a subsea hydrocarbon reservoir, comprising:
A computer apparatus loaded with machine readable instructions for implementing a method of planning an electromagnetic survey of an area identified as potentially containing a subsea hydrocarbon reservoir, comprising:
Dependencies are inferred from the claim text.
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Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation: operating with…
Operating with magnetic or electric fields produced or modified by objects or geological structures or by detecting devices: controlled source…
Technologies having an indirect contribution to adaptation to climate change: assessment of water resources
Geophysics
Term ended 29 Sep 2023 (estimated)
This application is a national phase of International Application No. PCT/GB02/05355 filed Nov. 28, 2002 and published in the English language.
The invention relates to seafloor electromagnetic surveying for oil and other hydrocarbon reserves.
Determining the response of the sub-surface strata within the earth's crust to electromagnetic fields is a valuable tool in the field of geophysical research. The geological processes occurring in thermally, hydrothermally or magmatically active regions can be studied. In addition, electromagnetic sounding techniques can provide valuable insights into the nature, and particularly the likely hydrocarbon content, of subterranean reservoirs in the context of subterranean oil exploration and surveying.
For a better understanding of the invention and to show how the same may be carried into effect reference is now made by way of example to the accompanying drawings.
FIG. 1 shows a schematic representation of an exploratory EM sounding survey.
FIG. 2A is a graph showing the modelled electric field strength as a function of distance from, and along the axis of, the EM source. This is shown for several frequency components. The modelled sea depth is 750 m.
FIG. 1 of the accompanying drawing shows schematically a surface vessel 14 undertaking EM sounding of subterranean rock strata 8 within which a hydrocarbon reservoir 12 is located. The surface vessel 14 floats on the surface 2 of the sea 4. A deep-towed vehicle 18 is attached to the surface vessel 14 by an umbilical cable 16 which provides an electrical, optical and mechanical connection between the deep-towed vehicle 18 and the surface vessel 14. The deep-towed vehicle 18 is towed by the surface vessel 14 such that it remains consistently close to the seafloor 6. This is facilitated by an echo-location package 20 which relays information about the height of the deep-towed vehicle 18 above the seafloor 6 to the surface vessel 14. The deep-towed vehicle 18 receives electrical power from the ship's on-board power supply via the umbilical cable 16.
A cycloconverter unit 30 generates the chosen waveform to be supplied to an EM source in the form of a transmitting antenna 22 which is towed by the deep-towed vehicle 18. The transmitting antenna 22 broadcasts the EM signal into the sea 4, and this results in a component passing through the rock strata 8. One or more remote instrument packages 26 record the signal received by receiving antennae 24 in response to the transmitted EM signal. If the separation of the transmitting antenna 22 and the receiving antenna 24 is greater than a few hundred meters, the highly conductive seawater strongly attenuates the direct signal between them. The components of the EM signal that have travelled through the rock strata 8 and the reservoir 12 dominate the received signal and provide information about the electrical properties of these regions. At the end of the sounding experiment, a remotely operable release system allows the instrument package 26 to be detached from a ballast weight (not shown) so that an in-built flotation device 28 can carry the instrument package 26 to the surface 2 for recovery and retrieval of data for inversion analysis.
The transmitting antenna 22 emits signals that propagate outwards both into the overlying water column 4 and downwards into the seafloor 6 and the underlying strata 8, 12. In both cases, at practical frequencies for this method and given the typical resistivity of the media 4, 8, 12, propagation occurs by diffusion of electromagnetic fields. The rate of decay in amplitude and the phase shift of the signal are controlled both by geometric spreading and by skin depth effects. Because in general the underlying strata 8, 12 are more resistive than seawater 4, skin depths in the underlying strata 8, 12 are longer. As a result, electric fields measured at the seafloor 6 by a receiving antenna 24 at a suitable horizontal range are dominated by the components of the source fields which have propagated downwards through the seafloor 6, along within the underlying strata 8, 12, and back up to the receiving antenna 24. Both the amplitude and the phase of the received signal depend on the resistivity structure of the underlying strata 8, 12—and so, in principal, a survey consisting of many transmitter (source) and receiver (detector) locations can provide a multi-dimensional image, by geophysical inversion, of sub-seafloor resistivity.