Patent Application
20200124760
The present invention relates to a method and a device for measuring the burial depth of a line of the kind that are being laid increasingly under a soil surface on land and in water in the form of conduits and pipelines and energy supply and/or data cables.
In order to protect such lines from external mechanical influences, but also from an intensely fluctuating influence of temperatures and thus to achieve the most constant possible maintenance of an intrinsic temperature, lines of the above-mentioned type are laid in the ground underneath a soil surface. In this connection, a certain depth below the soil surface is specified, which in the case of a line that is as a rule laid in a slot-shaped trench, is also referred to as the burial depth.
On land, a sufficient identification of such line routes and a possible placement of additional protective structures over the respective line is required in order to provide the greatest possible prevention of damage or excavation of the burial depth, for example as part of earth-moving operations. DE 196 14 707 A1 has also proposed applying corresponding warning signals in the form electromagnetic waves to these cables so that when a receiver comes close to them, a corresponding warning can be received.
When using buried underground lines of the above-mentioned type in bodies of water and particularly under a sea bed, additional problems arise. For identification, line routes can in fact be included in nautical charts. Also, additional protection can be provided for sections in line routes that are particularly threatened by shipping or icebergs. Lines, for example in the form of undersea cables, in order to protect them from mechanical damage of the kind that can be caused, for example, by anchors, are laid a particular minimum depth below the sea bed. Tides and currents, however, can reduce this depth to the point where the line is swept bare. As a result, this type of covering as protection could therefore prove to be insufficient, particularly against large anchors.
A covering of the lines that is as a rule composed of sand and/or gravel, however, will be moved and changed by the motion of waves as well as by tides and/or currents in the adjacent water layer. A sea bed is consequently anything but static. Due to tides and sea currents, the sea bed is continuously in motion, particularly in the vicinity of estuaries. As a result, even a specified minimum burial depth of a line can be fallen below within a short period of time. Lines can also be swept completely bare and/or altered in their position by the effects mentioned above by way of example.
Consequently, a covering layer that that extends, for example, as a cover for a so-called export or transport cable from an offshore wind farm to a collection point on the coast and is usually protected with a thickness or layer thickness of approximately 3 m, can be swept completely bare of the covering over the course of a few months due to the effects of currents. At least part of this line is then directly exposed to the mechanical forces of the water. But temperature differences in the water along longer stretches and differing dissipation of a self-heating produce regionally different elongations and compressions of the line, which can cause the line to be displaced or even buck in any direction in space. A temperature that is as uniform as possible due to a sufficient burial depth is very important with many lines, particularly in the case of high-voltage cables because they are very sensitive to thermal overloading. Excessively high thermal loads occurring in some regions can cause unwanted aging effects particularly in the insulation, but also in connection sleeves, etc. and can thus curtail the service life, resulting in premature failures and can thus reduce the availability of a network. By the same token, such heating phenomena, in addition to changing environmental conditions, also set individual capacity limits on the affected lines.
As part of a collection, in particular from offshore systems, there is the requirement it is necessary to be able to furnish proof of a correspondingly sufficient coverage of all lines. In addition, it is necessary to perform an annual inspection of the burial depths of the respective lines. To this end, there are known approaches, among others the one in DE 25 30 598 A1, in which on the one hand, a distance between a measuring point and a conduit composed of a magnetic material must first be located and then, with the aid of an electromagnetic alternating current method, a secondary field signal injected into a conduit is then measured in a detector cell in order to determine a distance and on the other hand, a sonar measurement is used as a basis for determining a distance between the detector cell and a respective surface of the sea bed as the surface of the covering. Based on a simple difference measurement, this makes it possible to determine a thickness of the covering layer.
In addition, GB 2 419 956 B has disclosed a method for detecting undersea cables and other electrically conductive bodies underneath a sea bed or ocean bed using pulsed electromagnetic fields.
The object of the present invention is to modify a method and corresponding device by increasing the measurement precision.
According to the invention, this is achieved by the features of the independent claims in that a method for measuring a burial depth of a line in which a detector cell transmits an electromagnetic pulse as a primary signal and a secondary signal is received and at the same time, a height of the detector cell above the bottom is measured, characterized in that more than one excitation coil extending in an xy plane is used, the excitation coils are positioned next to one another in an orientation essentially perpendicular to a center axis of the line and are moved essentially over the line, along this center axis being parallel to the y-axis of a Cartesian coordinate system. The excitation coils transmit electromagnetic pulses in a time-lagged fashion as a primary signal. This produces a kind of transmitting bar, which is moved in an essentially perpendicularly aligned direction over the line to be investigated. In addition, receiver coils that are equally distributed in the xy plane across the entire array of transmission coils and that carry out measurements in at least two axis, x and z axes of said Cartesian coordinate system, oriented orthogonally to one another and to the elongation of the line as well as the direction of propagation. All of such transmission coils measure the secondary signals in reaction to the transmission of a primary pulse by the transmission coils. Consequently, across the arrangement of transmission coils, a kind of array of receiver coils is used to pick up secondary signals from different respective positions. Because of spatial arrangement of magnetic fields, the receiver coils that are situated in a distributed fashion in the xy plane detect a secondary signal, possibly always with spatial components that differ in their magnitude. It is thus possible to draw better inferences as to a depth position of the line to be investigated. Since distance determinations of a height above the sea bed carried out, for example, based on sonar measurements are very precise today, it is possible, based on the difference between the distance between the line and the detector cell on the one hand and a height of the detector cell above the sea bed on the other, it is possible to very reliably determine a thickness of a covering of the line.
This object is also attained by means of a device that includes an array of more than one excitation coil extending in an xy plane; the excitation coils extending essentially perpendicular to a center axis of the line are arranged for being moved essentially along this center axis of the line; the coils are embodied for transmitting time-lagged electromagnetic pulses; and equally distributed across the entire array of transmitting coils in pairs of at least two receiver coils carry out measurements in at least two axes oriented orthogonally to one another respectively, all of which are embodied to execute measurements of a secondary signal in reaction to the transmission of primary pulses by the transmission coils. As long as there are two receiver coils used as a pair, the respective two axes are oriented orthogonally to center axis of the line and the direction of propagation.
Advantageous modifications are the subject of the respective independent claims. According to them, the receiver coils measure secondary signals as a reaction to the primary pulse over a certain time span only after a fixed time lag relative to a transmission of an electromagnetic pulse or primary pulse by the transmission coils e.g. in terms of evaluation. This time lag between the transmission of a primary pulse and a measurement of secondary signals is, for example, in a range of 400 up to 550 μs, and preferably approximately 498 μs for use in marine or salt-water. this range of time during the measurement span varies depending on different variables such as e.g. a line diameter, line depth, conductivity of the water, respectively.
In an embodiment of the present invention it is preferred that the measurement of the secondary signals is carried out for a time span of up to about 10 ms. In an embodiment of the invention signals have faded out after 10 ms and that is why the measurement has stopped resulting in said time span as a rule of thumb. However, there are cases imaginable for instance when the cable is heavier and thicker or the cable is buried at a lower depth, where the signal fades out after more than 10 ms, for instance after 15 ms. In such a case it is desirable to keep on measuring until all the relevant signals have faded out enhancing said time span up to about 15 ms.
A time span at the beginning is left out in terms of evaluation to cut away the influence of a number of side effects like e.g. reflections cause by marine water or salt-water and the like. In an alternative method, a correction regarding the influence of the salt water is carried out by first measuring the secondary signals obtained from the salt-water only and subsequently subtracting this from the secondary signals received during analysis of the burial depth of the line. By doing so the result is just the secondary signal originating from the line.
In an embodiment it is preferred that said arrangements or pairs of receiver coils are provided as receiver units, which are embodied like small cubes inside the array composed of the transmission coils or a plane parallel to said array. However, in an alternative embodiment, receiver units are located in a xy plane parallel to the array composed of the transmission coils. However, keeping in mind the effective size of receiver units in real life, the person skilled in the art certainly understands, that even a somewhat staggered positioning of receiver units is regarded to be a location of receiver units in a xy plane.
Preferably, the transmission coils and receivers or receiver units are affixed to a wing-shaped support composed of an electrically nonconductive material. Such a design can be embodied in a flow-optimized way in order to also be positionally stable at a nominal speed of an apparatus as described above under water with a reasonable flow resistance. Using known means and methods, the detector cell embodied in this way can also be changed in its position, in particular relative to a line, by means of a control. In addition to controllable rudders, small screws driven by electric motors or compressed air motors can be used like the ones that are known from mini-submarines or remotely operated underwater vehicles (ROVs).
Other features and advantages of embodiments according to the invention will be described in greater detail below in conjunction with exemplary embodiments based on the drawings. In the drawings:
Throughout the different figures of the drawings, the same reference numerals are consistently used for the same elements. Further, a Cartesian coordinate system is used throughout all figures modelling an ideal situation of application, where the center axis of a line as well as a direction of motion of a device according to the present invention are parallel to the y-axis of said Cartesian coordinate system.
Because of the growing importance of so-called offshore wind farms for the production of renewable energy, it is very important to protect, monitor, and/or inspect a line network that is to be constructed and maintained for these wind farms. Without restricting a use field of the present invention, only on an inspection of such lines will be discussed below. Basically, related and alternative use fields in the realm of archeology, prospecting for natural resources, or locating pipelines and the like are not precluded from a use of the method and devices according to the invention.
The illustration in
As shown in more detail in
These pulses B, B′, B″ also penetrate the sea bed surface BO of the indicated sea bed and excite the flow of induced currents in the electrically conductive material of the line extending 2. These currents decay and in turn generate secondary electromagnetic signals Br.
Distributed in the xy plane across the array of transmission coils 3, 3′, 3″ is an arrangement of receiver coils 4 for receiving the secondary electromagnetic signals Br. In a manner not shown in the drawing, two respective receiver coils 4 are combined with two axes or center axes extending in x and z of the Cartesian coordinate system respectively. Thus, two receiver coils 4 are combined as a pair extending orthogonally to one another to form a cube-like receiver unit 5. As a matter of the fact that the line 2 under a sea bed surface BO as the target is lying parallel to the y-axis of said Cartesian coordinate system changes in this direction may be neglected in this embodiment of the invention.
In this embodiment, there are five cube-like receiver units 5 used distributed in a more or less equidistant manner within each of the transmission coils 3, 3′, 3″ and beyond. Receiver units 5′ shown in dashed lines are cube-like receiver units in a somewhat staggered configuration, which still is regarded as a xy-plane configuration within the scope of the present invention reduce to deviations in real life showing very little effect to the method described in here. Thus, all cube-like receiver units 5 are regarded to be equal even in case of a deviation of their respective position. Said receiver units 5 are made to measure only the secondary signals Br in the receiver coils 4 of the receiver units 5 for evaluation after a specified time lag Δt from the transmission of primary pulses by the transmission coils 3, 3′, 3″. This may be achieved by switching means not further disclosed here. Approximately 498 μs is used as the time lag Δt.
The illustration in
The excitation coils 3, 3′, 3″ all lie in an xy plane and transmit electromagnetic pulses that are time-lagged relative to one another as a primary signal, as indicated by the different field lines B, B′, and B″ in
The illustration in
Across the array of transmission coils 3, 3′, 3″, distributed in the xy plane, receiver units 5 are provided, which all measure the secondary signals Br, not shown in detail here, that are generated in response to the transmission of each primary pulse by one of the transmission coils 3, 3′, 3″. Since the receiver units 5 each have receiver coils 4 that measure in two axes x and z extending orthogonal to one another, reception signals are picked up simultaneously at different points of the detector cell 1 that are slightly offset from one another. For simple reasons of geometry, the receiver units 5 according to
This effect may be used to reduce the influence of e.g. noise. Due to the longitudinal extension of the line 2 and a resulting form of the fields, the evaluation of response signals Br in this extension axis y is hardly informative. This means that measurement and calculation efforts can be saved here. In an exemplary embodiment, each transmission coil 3, 3′, 3″ is embodied as a rectangle with the edge lengths of approximately 1.5 m*approximately 1.41 m with a winding at a nominal current of approximately 170 A and a voltage between about 10 V to less than about 25 V. It can be shown, that in case of deviation regarding an axial offset as well as a coverage thickness Δ the amplitudes clearly decrease from a situation with a low coverage thickness Δ and a measurement position exactly over the center axis M of the line. Basically, however, the curve of an x component is always essentially point-symmetrical to the origin 0,0, the y component remains at about 0 due to symmetry of the line 2 and the detector cell 1 being torn at least parallel to the y-axis, while the z component has a curve that is axially symmetrical to the zero point.
Finally, a time decay at maximum amplitude for three different diameters of cables has been measured within the same field. Certainly, the best and strongest response is given from the cable having the largest diameter. However, over the measurements it was found that a response signal may be used up to 10 ms after switching of the primary signal. A time lag Δt in a range of 400 up to 550 μs cutting away by appropriate switching means analysis of the data derived from a respective measurement still gives the chance to receive a strong and reliable result for measuring a thickness Δ of a covering over the line 2 under examination.
| Number | Date | Country | Kind |
|---|---|---|---|
| 10 2017 210 672.7 | Jun 2017 | DE | national |
| Filing Document | Filing Date | Country | Kind |
|---|---|---|---|
| PCT/EP2018/065902 | 6/14/2018 | WO | 00 |
