The present invention relates to sensors which exploit a change in phase of an interrogation signal to determine a sensed parameter, and particularly, but not exclusively to fibre optic interferometric sensing. The present invention finds particular application in the filed of seismic surveying.
Fibre optic sensors employ a length of optic fibre arranged in such a way that a sensed parameter causes a strain to be imposed on the fibre. Typically the fibre is arranged in a coil, although other arrangements are possible. Such strain causes a change in phase of optical signal propagation in that fibre, which change can be detected by interferometric techniques. A variety of different arrangements for this type of transducer have previously been proposed, many of which have the coil of optic fibre wound on a deformable core or mandrel, which undergoes radial expansion or contraction in response to the sensed parameter, such as sensed vibration.
Such fibre optic sensors can exhibit extremely high sensitivities, and have the advantage of being completely passive, employing no power at the sensing transducer. Such sensors have also proved popular in applications where large arrays of sensors are required, on account of the relative ease with which they can be multiplexed.
An example of such an application is seismic surveying in the oil and gas exploration industry, where large time multiplexed arrays comprising hundreds or even thousands of vibration sensors and/or hydrophones can be used to sense reflections of an incident pulse from geological formations beneath the sea bed. Sampling such an array at regular periods provides 3D time lapsed data on existing or potential new reserves.
A problem experienced with this approach to sensing is that, for a given sampling rate, signals above a certain amplitude threshold cause the phase based sensed information to become distorted, and can cause failure of the demodulation process. This effect, commonly referred to as overloading or overscaling is dependent on the frequency of the measured signal. In seismic systems this can cause a particular problem with the direct arrival of the incident pulse, especially when that pulse has been generated close to the sensors (usually by an airgun towed from a surface vessel as it passes over the array). It is desirable to be able to record this incident pulse without the distortion that overscale can produce.
It is therefore an object of the present invention to provide improved sensing methods and apparatus.
According to a first aspect of the present invention there is provided a method of interrogating a phase based transducer, said transducer providing a change in phase of signal propagation in response to a sensed parameter, said method comprising receiving a signal propagated through said transducer, comparing the signal at a point representing the state of the transducer at a first time, and at a point representing the state of the transducer at a second time, and determining from said comparison a measure of the rate of change of phase with time of said signal.
The rate of change, or derivative of the phase change typically has a much smaller amplitude than the signal itself since the difference between the two times at which the signal is measured will usually be much less than the period of the signal being measured. Thus even if the transducer experiences a stimulus which causes the normal signal to overscale, the derivative signal is likely to be unaffected. The derivative signal or measurement can therefore be thought of as a low sensitivity measurement, which can be obtained severally and independently, to be used instead of or in combination with the normal signal measurement having higher sensitivity. For a signal with the majority of its energy centred at approximately 800 Hz, for example, the derivative of that signal will typically be attenuated by 60 dB with a period between the two measurement times of 200 ns.
In one embodiment, comparing the signal comprises combining a delayed version and an undelayed version of the received signal, preferably using an output interferometer. Alternatively the signal could be sampled at multiple different times and an algorithmic or signal processing approach employed to determine the derivative of the sensed parameter.
The actual value of the sensed parameter can be reconstructed by integrating the measured derivative value. However, if the noise floor is determined by system noise, then the noise floor is substantially the same for both the phase information and its derivative, the derivative signal suffers from a lower SNR. Considering then that overscaling may only occur infrequently in response to certain high amplitude inputs, such as the first break of an airgun used in geophysical surveying, it is beneficial in certain embodiments to measure both the derivative, and the actual value of the sensed parameter directly. Examples of such embodiments are described below and it will be appreciated that an adaptive system could be employed which measures the signal directly in a default state, and reverts to a signal integrated from a derivative measurement on detecting an overscale condition. For example, it would be possible to use a threshold value for the amplitude of the derivative signal to identify periods in which the normal signal was overloaded.
It has been found however, that by careful consideration of overscaling and its effect on the phase information produced by the transducer, that during overscaling, although a direct measurement of the phase value representative of the sensed parameter may be distorted, such a phase value can be used in conjunction with the derivative signal to produce a re-constructed value. In certain embodiments therefore a measure of phase from said received signal is derived in addition to the measure of the rate of change of phase. In particular embodiments the two measures (phase, and rate of change of phase) are obtained severally, in that each can be obtained without recourse to the other, and can be obtained substantially simultaneously.
As will be described below in greater detail, overloading occurs when the instantaneous frequency of the output of the transducer (which depends on the rate of change of phase) falls outside of the Nyquist frequency range determined by the rate at which this signal is sampled. Any instantaneous frequency that falls outside the Nyquist range will be folded about the limits of the range back into it. Depending on the amplitude and frequency of the sensed signal, the information may be folded or wrapped about the Nyquist frequency limits multiple times. The present inventors have found that the derivative information measured in embodiments of the present information can be used to determine how many times the information has been wrapped, or the factor by which the information exceeds the Nyquist limit. This then allows the directly measured parameter value to be corrected to provide a signal having an improved SNR to that provided by integrating the measured derivative signal.
The invention extends to methods, apparatus and/or use substantially as herein described with reference to the accompanying drawings.
Any feature in one aspect of the invention may be applied to other aspects of the invention, in any appropriate combination. In particular, method aspects may be applied to apparatus aspects, and vice versa.
Preferred features of the present invention will now be described, purely by way of example, with reference to the accompanying drawings, in which:
Referring to
Referring to
If φ(t) is the sensed parameter, then the signal obtained from a photodetector used to measure a series of pulses returning from a sensor of the type described above can be written as cos(ωct+φ(t)) i.e. the sensed information is represented as a phase change superimposed on a carrier signal of frequency ωc. Techniques that are well known to those skilled in the art can then be used to demodulate the phase signal from the carrier. The carrier frequency is typically chosen to be half of the Nyquist frequency, which is in turn half of the sampling frequency. It is usual for one sample to be made in each returning optical pulse and so the sampling frequency is the rate at which pulse pairs are transmitted into the array. By way of an example, the sampling frequency could be approximately 320 KHz, giving a Nyquist frequency of approximately 160 KHz and a carrier frequency of approximately 80 KHz. The sampling frequency will typically have a practical upper limit dependent upon the type and arrangement of sensor or sensors, amongst other factors.
An overscale condition occurs when the instantaneous frequency of the phase modulated carrier falls outside the Nyquist band i.e. when
or when
where ωN and ωc are the Nyquist and carrier frequencies respectively. In practice this results in aliasing of instantaneous frequency back into the Nyquist band by folding or wrapping around one of its limits in frequency space. Depending on the magnitude and frequency of the sensed parameter, the instantaneous frequency can be wrapped back multiple times. If the sensed parameter is modelled approximately as ω(t)=φ0 cos ωmt, then the condition for overscale not occurring, for the usual condition of ωN=2ωc is sometimes expressed as
Referring now to
The output series of pulses is tapped off at junction 406, passed through an isolator 408, and to output interferometer designated by 410. In the scheme of
or the instantaneous frequency of the returned signal.
Considering the combined output pulse centred at t=1, it will be understood that this represents the combination of two pulse having been reflected from mirror B, ie having passed through sensing loop AB, at two different times. The derivative of the parameter sensed by coil AB is therefore contained within and can be determined from this pulse. In a similar way, the pulse output from the interferometer at t=2 will be a combination of pulses, both of which have made double passes of sensing loops AB and BC. Once the derivative value is extracted from this pulse then, by subtracting the derivative value of sensing loop AB (obtained above) the derivative value of sensing loop BC is obtained. In this way, the derivative values for each of the sensing loops in package 402 can be obtained.
It is noted that the reflection from fibre coupled mirror A is not affected by the derivative, or rate of change of phase of any of the sensing loops of the arrangement explained above with respect to
Turning to
It can be seen that pulse trains 604 and 606 are substantially the same as trains 502 and 504 of
Therefore, in the arrangement described, both directly sensed (high sensitivity) values and derivative (low sensitivity) values can be obtained independently from interleaved sets of output pulses, resulting from the same input pulse pair. It can be seen that in the example of
The operation of the arrangement of
Interferometer 706 of
It will be noted that the component pulses making up signals 708 and 710 will have passed through the sensor package with a greater time separation than in previously described embodiments. This results in the derivative signal being more sensitive than for a shorter input pulse separation. For a 2 μs input pulse delay, approximately 10 times more phase is accumulated over the derivative sampling time than if a 200 ns delay had been employed. Considering the ‘direct’ measurement of phase, since the two samples being combined in interferometer 706 represent instances at the sensor having a relatively large time separation, then the measure of the derivative of phase obtained from interferometer 704 can be used to provide a correction if necessary.
In the embodiment of
An alternative method to achieve an increase in the time separation between the pulses that generate the derivative signal is to keep the pulse separation at 200 ns but then mix reflections that were from different transmitted pulse pairs. In such an embodiment the time separation between respective pairs of pulses is determined by the length of fibre in the sensors in one segment of the array, but a value of around 5 μs would be typical.
Since the delay imposed by the delay coil (5.2 μs) is 200 ns longer than the time separation between pulse pairs, the combination of pulses takes the same general form as if the delay imposed by the coil had been 200 ns (as per
It can be shown that it is possible (in the embodiment described above) to use any delay time of the form [5NR+2(ND+1)0.2] μs, where the 5 μs is the time between pulse pairs and NR is a positive integer. The number 0.2 corresponds to the time in μs between pulses in a pair and is dictated by the sensor length. ND is also a positive integer. The derivative of a time varying signal will tend to be proportional to the frequency of the signal. Actual interferometer response observes this relationship at low frequencies, but tails off slightly at high frequencies. In the low frequency range of approximately 0-250 Hz (useful in seismic applications), the amplitude of the derivative signal can therefore be correspondingly low, and can suffer from low SNR. Using a longer delay however causes the interferometer sensitivity to be greatly increased, and to produce correspondingly increased output amplitudes.
Although the arrangement shown in
Referring to
The pulse of
Considering
S
1
=A cos(ωcntp+φ1)
where A is the signal amplitude into the demodulation system, n is the nth sample after some arbitrary start, and φi is the phase associated with the sample at the first sampling position S1. The second sample S2 is simply modelled by
S
2
=A cos(ωc(ntp+τs)+φ2)
where φ2 is the phase associated with the signal at the second sampling position.
It is possible to employ an algorithm using the two samples S1 and S2, to extract the instantaneous phase change Δφ=(φ2−φ1) which can take the form:
This is the differential phase acquired over the sampling period τs within a pulse. Assuming τs is significantly smaller than the carrier period tp, the change in phase Δφ is small, but this can correspond to a very large instantaneous frequency over the said sampling time.
The above algorithm which operates on two sampling positions on the pulse may provide an adequate solution in certain applications, but has been found to suffer from a degree of data dropout under certain conditions. While a limited amount of data dropout may be acceptable, it is possible to use a third sample S3 (labelled as 1010) from the pulse to improve the estimate of Δφ.
By taking a third sample, a second phase change value Δφ2 (corresponding to the phase change over time τs between S2 and S3) is obtained. The difference between the two phase changes Δφ1 and Δφ2 is assumed to be small in comparison to either one value, and by taking the maximum of the absolute value between the two phase measurements i.e. max (|Δφ1|, |Δφ2|) data dropout can be substantially eliminated up to a maximum ratio of Fs/Fp (Fs=1/τs) allowing an accurate reconstruction of a wrapped instantaneous frequency signal. The reconstruction process is typically carried out at the sampling rate Fp, but may be decimated to other rates after reconstruction.
Using this technique, signals having instantaneous frequency values up to 500 times greater than the ‘normal’ overscaling limit can be reconstructed over a wide range of frequencies, for typical sampling frequencies of 160 kHz.
Where the change in phase Δφ is itself wrapped, this will happen between Fp/2 and dc, bearing in mind that the centre of the instantaneous frequency change is at the carrier frequency.
A frequency unwrapping algorithm to unfold the instantaneous frequency operates by finding the time positions where the instantaneous frequency reaches zero and changing the sign of the signal between every other pair of zero crossings. The instantaneous frequency is finally integrated or used to reconstruct the lost phase information in the normal sensitive signal.
It will be understood that the present invention has been described above purely by way of example, and modification of detail can be made within the scope of the invention.
Although a fibre optic sensor package suitable for seismic surveying has been described, it will be appreciated by the skilled person that the invention is equally applicable to other types of phase based transducers employed in alternative applications. Examples include uses of fibre optic hydrophones in active sonar systems and measurements of surface vibration using a free space optical interferometer.
Each feature disclosed in the description, and (where appropriate) the claims and drawings may be provided independently or in any appropriate combination.
Number | Date | Country | Kind |
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0705240.0 | Mar 2007 | GB | national |
Filing Document | Filing Date | Country | Kind | 371c Date |
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PCT/GB08/00830 | 3/10/2008 | WO | 00 | 8/31/2009 |