Patent Grant
8593910
1. Field of the Invention
The present invention relates to permanent seismic wave emission systems and more particularly to a permanent seismic wave emission device based on magnetostrictive materials.
2. Description of the Prior Art
Several types of seismic sources for emitting seismic waves in wells are known. These sources are of different types and involve
either an explosion which may be a point or elongated charge with detonating cord wound helically around a rigid mandrel, etc.;
an electric spark which is a breakdown between electrodes in water, a wire explosion under the effect of an electric discharge, etc.,
a vertical mechanical shock of a mass impacting an anvil secured to a packer that produces, on the well wall, a vertical shear for mainly generating S waves,
or a horizontal shock, in a radial direction, of a mass radially driven by hydraulic or electromagnetic a mechanism that contact the well wall at one point.
Seismic waves are also created in wells using controlled vibratory sources of piezoelectric type which are coupled (or not) to the well wall and which emit monofrequencies or codes or frequency modulated signals through a ramp.
These permanently buried seismic sources provide advantages of stability of the source coupling conditions due to the fact that the source is permanently cemented in a dedicated well; insensitivity to the climatic variations of the altered zone when the source is installed below the altered zone; ease of implementation of the source for each acquisition survey; and proximity of the source in relation to the seismic objective to be imaged.
The main drawback of these buried permanent seismic sources is the high installation cost, mainly because a well dedicated to these sources is required. Furthermore, their efficiency is affected by the stiffness of the casing that limits the stress applied to the surrounding medium.
A device for emitting radial elastic waves in a material medium, based on the principle of magnetostriction, is also known. The emission of radial waves is essentially obtained by radially expanding the metallic casing of the well in contact with the material medium under the effect of a magnetic pressure generated by electromagnetic induction with elastic waves being created in the medium under the effect of the radial expansion. The magnetic pressure is obtained by connecting a coil placed in line with the tube to a current generator, a shock generator or a variable frequency generator. The winding pitch of the coil can be constant or variable. The tube can for example be added into a well or a hole, or it can be a tube portion of a cased well. It can also be the lateral wall of a sealed enclosure that is immersed in water for producing acoustic or seismic waves therein.
However, for this type of source, the elongation of the material making up the casing is tens of parts per million. The seismic wave generated is thus very weak and the efficiency of this type of source is therefore not satisfactory enough to be properly used in the industry.
The present invention overcomes one or more of the drawbacks of the prior art by providing a permanent seismic source that can be installed below the altered zone and that does not require drilling of a well specifically dedicated to seismic prospecting, and having an efficiency compatible with 4D seismic surveys.
The invention provides a system for emitting seismic waves in an underground formation traversed by a well comprising a casing, including a casing seal allowing passage of a magnetic field, an active part generating seismic waves, made up of magnetic-field active elements, disposed outside the casing seal, and a mobile magnetic field induction source disposed inside the casing seal.
The active elements of the seismic wave emission system are made of magnetostrictive materials.
The active elements are bars which are evenly distributed over the circumference of the casing seal and parallel to the casing axis. The ends of each bar rest on two rings mechanically coupled with the formation.
According to an embodiment of the invention, the number of bars ranges between 3 and 10.
According to an embodiment of the invention, the bars are straight.
According to another embodiment of the invention, the bars are curved, have the shape of the stave of a cask with two ends resting upon two rings through two stops fastened to the casing seal.
Circulation of the magnetic field occurs through windows provided in the casing seal at the level of the rings.
According to another embodiment of the invention, circulation of the magnetic field occurs through the two stops.
The zone of the casing seal located between the two rings had magnetic materials.
Mechanical coupling of the rings with the formation is achieved with cement.
The invention also relates to a method using the seismic wave emission system, which activates active elements arranged outside the casing of a well, with a magnetic field emitted by a mobile magnetic field induction source within the casing of the well which passes through the casing of the well.
The invention has application for seismic prospecting or monitoring operations in the subsoil. Seismic prospecting generally emits seismic waves in the subsoil, by one or more seismic sources emits seismic waves and records the reflected waves formation discontinuities with seismic receivers (geophones, hydrophones), for forming seismograms, which are processed to extract therefrom useful information relative to the subsoil geology. The device can be used for example to generate seismic waves within cased wells.
Other features and advantages of the invention will be clear from reading the non-limitative description hereafter, illustrated by the accompanying figures wherein:
The seismic wave emission system according to the invention is described in connection with
The seismic wave emission system according to the invention is integrated in a well or any other cavity of the same type to be equipped with seismic sources. The well comprises a set of casing seals (1) making up casing (10) that is included in the completion of the well. The system is thus integrated at the level of one of these casing seals (1).
The system according to the invention comprises an active part generating the seismic waves, which is activated by a mobile magnetic field induction source (8).
The active part of the device has active elements generating the seismic waves, made up of several bars (4) arranged parallel to the casing axis (A). These bars have a cross-section of any shape. The bars are evenly arranged over the circumference of casing seal (1) and outside casing seal (1). The device comprises 3 to 10 bars, preferably 4 to 8 bars and more preferably 4, 6 or 8 bars.
The materials used for these bars are magnetostrictive materials, GMMs (Giant Magnetostrictive Materials), such as Terfenol-D produced by the ETREMA® Company (United States). When they are subjected to a magnetic field, these materials can elongate by 1500 ppm. According to the invention, the source can comprise yet more effective materials such as the MSM magnetic shape memory materials, for example the Ni—Mn—Ga alloy marketed by the AdaptaMat Company (Finland). When they are subjected to a magnetic field, these materials can elongate by 100,000 ppm.
The ends of each bar (4) rest on two rings (2) and (6) fastened with cement (11), reinforcing the well, between casing seal (1) and formation (12) or medium (12) surrounding the well. Rings (2) and (6) are thus mechanically coupled to formation (12) by cement (11). Any other equivalent material can be used in place of cement to fasten the rings.
In a first embodiment of the invention, bars (4) are straight and they preferably have a circular cross-section. Rings (2) and (6) are embedded in cement and therefore are held in place in cement (11) along casing seal (1). In order to facilitate setting of the device upon well construction, one (2) of the rings can be fastened to the casing seal. Thus, when pouring the cement around the formation, active elements (4) are held in place.
Thus, when bars (4) made of active material are subjected to magnetic field (13), generated by a mobile induction source (8), they elongate. The elongation of the bars depends on the type of magnetostrictive material used. This elongation exerts a longitudinal pressure with respect to the casing axis (A) on the rings, which thus causes stresses in cement (11) surrounding the casing. These stresses then generate seismic waves that propagate in cement (11) and in surrounding medium (12). The seismic wave propagation mechanism is known in the art. In this variant, the deformation of the bars thus causes longitudinal stresses with respect to the casing axis in cement (11). The seismic waves which are generated are recorded by seismic pickups and will be used by geophysicists to detect, among other things, the hydrocarbon level variations in the reservoirs or the gas volumes in CO2 storage sites.
The inducing tool, which has a coil (8) and of an electrocarrying linking cable (9) connecting it to the surface, induces a magnetic field (13) used to cause expansion of the active material bars. Coil (8) is lowered into the well, by means of cable (9), only during seismic acquisition surveys. The rest of the time, the inside of the casing is free for other uses, production, logging, etc.
The method implementing the system according to the invention thus activates active elements (4) of the seismic wave emission system arranged outside casing seal (1), with a mobile source located within casing seal (1) during seismic measuring operations, through well casing (1).
Coupling of the mobile induction source (8), temporarily located within casing seal (1), with the permanent part of the device located outside casing seal (1), is performed through the wall of casing seal (1) that allows passage of the magnetic field. Circulation of the magnetic field induced by the coil thus occurs through windows (7) provided in casing seal (1) and arranged at the level of rings (2) and (6).
Casing seal (1), that supports the source, is generally made of steel and it can be optimized to improve the magnetic coupling between coil (8) and active material bars (4). The steel of the casing seal is therefore replaced, at the level of bars (4), by a zone (5) made of a magnetic materials (relative permeability close to 1) known to persons skilled in the art to avoid any magnetic flux loss in the casing. Similarly, in order to limit losses, the magnetic circuit can be optimized through the use of materials of high magnetic permeability for rings (2) and (6) arranged at both ends of bars (4), and for windows (7) integrated to casing seal (1), which belong to the magnetic circuit of the seismic source.
In a second embodiment of the invention, the active elements or bars made of magnetostrictive materials are curved in the shape of bent plates or cask staves (4′) illustrated in
These elements rest on rings (2) and (6) through stops (3) fastened to casing seal (1). Rings (2) and (6) and stops (3) are embedded in the cement surrounding the well.
When magnetic field (13) induced by coil (8) flows through the stave-shaped elements, the latter elongate through magnetostrictive effect. The elongation being limited by stops (3), active element (4) deforms perpendicularly to the casing axis due to its concave shape. Thus, unlike the first variant, the deformation of the bars causes radial stresses, with respect to the casing axis, in the cement.
In this variant, magnetic field (13) circulates either through windows (7) or through stops (3) as illustrated in
The deformation is transmitted to cement (11) and then to soil (12) which generates a seismic wave that can be used as a source for seismic acquisitions.
The active elements having the shape of plates or of cask staves (4′) can be a bimetallic strip made up of an inner supporting plate (41), made of titanium for example, and of an outer layer (42) made up of prismatic elements made of magnetostrictive material which are attached together and attached onto the titanium supporting plate.
In another variant of the invention, several devices can be integrated in the completion of one well at different depths and can be used alternately while lowering the inducing source into the well or the formation.
The permanent seismic emission device can for example be integrated in the casing of production or observation wells provided in the development plan of oil reservoirs or the storage of hydrocarbons under observation by means of the 4D seismic method since the mobile induction source is set within the well only during seismic prospecting or monitoring operations.
It is clear that the present invention is not limited to the details given above and that it allows embodiments in many other specific forms without departing from the field of application of the invention. The present embodiments should therefore be considered by way of illustration and they can be modified without however departing from the scope defined by the accompanying claims.
| Number | Date | Country | Kind |
|---|---|---|---|
| 07 07934 | Nov 2007 | FR | national |
| Filing Document | Filing Date | Country | Kind | 371c Date |
|---|---|---|---|---|
| PCT/FR2008/001569 | 11/6/2008 | WO | 00 | 5/6/2010 |
| Publishing Document | Publishing Date | Country | Kind |
|---|---|---|---|
| WO2009/092919 | 7/30/2009 | WO | A |
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