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M.M.K. Al Hasani
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1
Distributed Acoustic Sensing (DAS) is a versatile dynamic strain sensing method that has been adopted for a wide range of seismic applications. In DAS, optical fibres are interrogated and used as sensors, where a strain or strain-rate measurement is made along a specific length of the fibre, called the gauge length. Its main appeal is the spatially dense data over long distances. The main limitations of DAS, however, are that it is mainly sensitive along the axial direction of the fibre and that the signal-to-noise ratio is worse than that of standard geophones. The first issue limits its adoption in surface reflection seismic when the fibre is deployed horizontally. Also, due to the very nature of the measurement (i.e. elongation and contraction of the fibre), it is commonly considered as a single-component measurement, therefore it lacks the information from the other components.
This thesis studies the potential of obtaining multi-component information from DAS as well as investigating the use of combined fibre configurations for surface-seismic applications. We approach this by examining several fibre-shaping approaches with static and dynamic strain measurements. First, the concept of the sinusoidally shaped fibre is examined to make a directional strain sensor in a direction other than the fibres’ axial direction using a static-strain approach. Secondly, the combined use of straight and helically wound fibres for obtaining multi-component information from DAS data as well as assessing the usefulness of using such a combination is investigated in a surface-seismic setting.'
Using the sinusoidally shaped fibre, two approaches are investigated. The first approach involves the use of the sinusoidally shaped fibre embedded in a homogenous material. An analytical model is presented to describe what happens to the deformed fibre in three main directions, which was validated via a finite-element model. Along with the model, loading experiments were performed on a sinusoidally shaped fibre embedding in a polyurethane-type (i.e. called Conathane®) strip in the following directions: in-line (i.e. transversal in-plane with the sinusoidal fibre), broadside (i.e. perpendicular to the sinusoidal fibre), and along-strip (i.e. along the strip’s longest dimension). We saw that the fibre is mainly sensitive to the in-line and broadside directions, and it is slightly more sensitive in the in-line direction relative to the broadside direction. We also saw that the geometrical parameters of the fibre, as well as the mechanical properties of the embedding material, affect its directional sensitivity. This is exploited in the second approach where the embedding material is now adapted to a low Poisson’s ratio metamaterial as well as further adaptations in the geometry of the fibre, aiming to create a unidirectional strain sensor. Experimental results showed improvements in the sensitivity but not as much as predicted by the analytical or numerical modelling.
Using DAS in field settings, multiple configurations of straight (SF) and helically wound fibres (HWF) with different wrapping angles (α) were buried in a 2-m trench in farmland in the province of Groningen in the Netherlands. Significant amplitude differences are observed between the straight and helically wound fibres. It is observed that shaping the fibre into a helix dampens the amplitude inside the surface wave significantly. Also, a polarity flip is observed with the use of HWF with a wrapping angle of 30◦. This hints that there is a contribution of the vertical component on the response measured by the HWF as also supported by the theoretical models. The reflection response is also examined using a set of engineered SF and HWF fibres. The main seismic reflections are present in both fibres with higher amplitude in SF compared to HWF, contrary to what was expected. Also, using post-stack images we see that the SF and HWF provide reflection structural images comparable to surface-deployed geophones but with an (expected) lower signal-to-noise ratio. We show that the combined use of SF and HWF is useful, as reflections were better shown for the shallow section, unlike HWF which provided better reflections in deeper sections. Furthermore, we discuss the effect of gauge length on the retrieval of surface waves along with the use of different fibre shapes using active and passive sources.
With the active-source data, we show that the gauge length plays an essential role in the retrieval of surface waves depending on their wavelength range, as it might cause distortions in the waveform which appears as notches in the (frequency, horizontal-wavenumber)–domain, as well as complicates picking the dispersion curves of these waves. On the other hand, the helically wound fibres might require a longer gauge length to retrieve the surface wave properly. This decreased sensitivity of the helically wound fibres is also shown from virtual shots obtained by passive interferometry as well as a recorded earthquake in the area.
...
Distributed Acoustic Sensing (DAS) is a versatile dynamic strain sensing method that has been adopted for a wide range of seismic applications. In DAS, optical fibres are interrogated and used as sensors, where a strain or strain-rate measurement is made along a specific length of the fibre, called the gauge length. Its main appeal is the spatially dense data over long distances. The main limitations of DAS, however, are that it is mainly sensitive along the axial direction of the fibre and that the signal-to-noise ratio is worse than that of standard geophones. The first issue limits its adoption in surface reflection seismic when the fibre is deployed horizontally. Also, due to the very nature of the measurement (i.e. elongation and contraction of the fibre), it is commonly considered as a single-component measurement, therefore it lacks the information from the other components.
This thesis studies the potential of obtaining multi-component information from DAS as well as investigating the use of combined fibre configurations for surface-seismic applications. We approach this by examining several fibre-shaping approaches with static and dynamic strain measurements. First, the concept of the sinusoidally shaped fibre is examined to make a directional strain sensor in a direction other than the fibres’ axial direction using a static-strain approach. Secondly, the combined use of straight and helically wound fibres for obtaining multi-component information from DAS data as well as assessing the usefulness of using such a combination is investigated in a surface-seismic setting.'
Using the sinusoidally shaped fibre, two approaches are investigated. The first approach involves the use of the sinusoidally shaped fibre embedded in a homogenous material. An analytical model is presented to describe what happens to the deformed fibre in three main directions, which was validated via a finite-element model. Along with the model, loading experiments were performed on a sinusoidally shaped fibre embedding in a polyurethane-type (i.e. called Conathane®) strip in the following directions: in-line (i.e. transversal in-plane with the sinusoidal fibre), broadside (i.e. perpendicular to the sinusoidal fibre), and along-strip (i.e. along the strip’s longest dimension). We saw that the fibre is mainly sensitive to the in-line and broadside directions, and it is slightly more sensitive in the in-line direction relative to the broadside direction. We also saw that the geometrical parameters of the fibre, as well as the mechanical properties of the embedding material, affect its directional sensitivity. This is exploited in the second approach where the embedding material is now adapted to a low Poisson’s ratio metamaterial as well as further adaptations in the geometry of the fibre, aiming to create a unidirectional strain sensor. Experimental results showed improvements in the sensitivity but not as much as predicted by the analytical or numerical modelling.
Using DAS in field settings, multiple configurations of straight (SF) and helically wound fibres (HWF) with different wrapping angles (α) were buried in a 2-m trench in farmland in the province of Groningen in the Netherlands. Significant amplitude differences are observed between the straight and helically wound fibres. It is observed that shaping the fibre into a helix dampens the amplitude inside the surface wave significantly. Also, a polarity flip is observed with the use of HWF with a wrapping angle of 30◦. This hints that there is a contribution of the vertical component on the response measured by the HWF as also supported by the theoretical models. The reflection response is also examined using a set of engineered SF and HWF fibres. The main seismic reflections are present in both fibres with higher amplitude in SF compared to HWF, contrary to what was expected. Also, using post-stack images we see that the SF and HWF provide reflection structural images comparable to surface-deployed geophones but with an (expected) lower signal-to-noise ratio. We show that the combined use of SF and HWF is useful, as reflections were better shown for the shallow section, unlike HWF which provided better reflections in deeper sections. Furthermore, we discuss the effect of gauge length on the retrieval of surface waves along with the use of different fibre shapes using active and passive sources.
With the active-source data, we show that the gauge length plays an essential role in the retrieval of surface waves depending on their wavelength range, as it might cause distortions in the waveform which appears as notches in the (frequency, horizontal-wavenumber)–domain, as well as complicates picking the dispersion curves of these waves. On the other hand, the helically wound fibres might require a longer gauge length to retrieve the surface wave properly. This decreased sensitivity of the helically wound fibres is also shown from virtual shots obtained by passive interferometry as well as a recorded earthquake in the area.
Distributed acoustic sensing has been limited in its use for surface-seismic reflection measurements due to the fiber’s decreased broadside sensitivity when the fiber is deployed horizontally. Deploying the fiber in a helically wound fashion has the promise of being more sensitive to broadside waves (e.g., P-wave reflections) and less sensitive to surface waves than a straight fiber (SF). We examine such claims and compare the responses of SFs and helically wound fibers (HWFs) with different wrapping angles, using standard and engineered fibers. These fibers have been buried in a 2 m deep trench in a farmland in the province of Groningen in The Netherlands, where we performed an active-source survey. We observe in our field data that using HWF has a destructive effect on the surface-wave amplitudes. Our data confirms the effect of the wrapping angle on the polarity of the surface-wave arrival and the dampening effect of the helical winding, behaving in quite a predictable fashion. Apart from the effect of the wrapping angle, the different design choices, e.g., cable filling and material type, do not show a significant effect on the amplitude of the signals. As for P-wave reflections, we observe that engineered SF and HWF provide reflection images comparable with those obtained from simultaneously deployed geophones at the surface despite the SF’s decreased broadside sensitivity. A polarity reversal and an amplitude difference between the SF and HWFs are observed. Finally, we demonstrate that the combined use of SF and HWF proved to be useful because SF showed better sensitivity in the shallower part and HWF in the deeper part.
...
Distributed acoustic sensing has been limited in its use for surface-seismic reflection measurements due to the fiber’s decreased broadside sensitivity when the fiber is deployed horizontally. Deploying the fiber in a helically wound fashion has the promise of being more sensitive to broadside waves (e.g., P-wave reflections) and less sensitive to surface waves than a straight fiber (SF). We examine such claims and compare the responses of SFs and helically wound fibers (HWFs) with different wrapping angles, using standard and engineered fibers. These fibers have been buried in a 2 m deep trench in a farmland in the province of Groningen in The Netherlands, where we performed an active-source survey. We observe in our field data that using HWF has a destructive effect on the surface-wave amplitudes. Our data confirms the effect of the wrapping angle on the polarity of the surface-wave arrival and the dampening effect of the helical winding, behaving in quite a predictable fashion. Apart from the effect of the wrapping angle, the different design choices, e.g., cable filling and material type, do not show a significant effect on the amplitude of the signals. As for P-wave reflections, we observe that engineered SF and HWF provide reflection images comparable with those obtained from simultaneously deployed geophones at the surface despite the SF’s decreased broadside sensitivity. A polarity reversal and an amplitude difference between the SF and HWFs are observed. Finally, we demonstrate that the combined use of SF and HWF proved to be useful because SF showed better sensitivity in the shallower part and HWF in the deeper part.
On the Multi-component Information of DAS for Near-Surface Seismic
A Pilot Field Experiment in the Groningen Area
In a surface-seismic setting, Distributed Acoustic Sensing (DAS) is still not a widely adopted method for near-surface characterisation, especially for reflection seismic imaging, despite the dense spatial sampling it provides over long distances. This is mainly due to the decreased broadside sensitivity that DAS suffers from when buried horizontally in the ground (that is when the upgoing wavefield (e.g. reflected wavefield) is perpendicular to the optical fibre). This is unlike borehole settings (e.g. zero-offset Vertical Seismic Profiling), where DAS has been widely adopted for many monitoring applications. Advancements in the field, like shaping the fibre to a helix, commonly known as helically wound fibre, allow better sensitivity for the reflections. The promise of spatially dense seismic data over long distances is an attractive prospect for retrieving the local variations of near-surface properties. This is particularly valuable for areas impacted by induced seismicity, as is the case in the Groningen Province in the north of The Netherlands, where near-surface properties, mostly composed of clays and peats, play an essential role on the amount of damage on the very near-surface and the structures built on it. Installing fibre-optic cables for passive and active measurements is valuable in this situation. We installed multiple cables containing different fibre configurations of straight and helically wound fibres, buried in a 2-m deep trench. The combination of the different fibre configurations allows us to obtain multi-component information. We observe differences in the amplitude and phase information, suggesting that these differences can be used for separating the different components of the wave motion. We also see that using enhanced backscatter fibres, reflection images can be obtained for the helically wound fibre as well as the straight fibre, despite the decreased broadside sensitivity for the latter.
...
In a surface-seismic setting, Distributed Acoustic Sensing (DAS) is still not a widely adopted method for near-surface characterisation, especially for reflection seismic imaging, despite the dense spatial sampling it provides over long distances. This is mainly due to the decreased broadside sensitivity that DAS suffers from when buried horizontally in the ground (that is when the upgoing wavefield (e.g. reflected wavefield) is perpendicular to the optical fibre). This is unlike borehole settings (e.g. zero-offset Vertical Seismic Profiling), where DAS has been widely adopted for many monitoring applications. Advancements in the field, like shaping the fibre to a helix, commonly known as helically wound fibre, allow better sensitivity for the reflections. The promise of spatially dense seismic data over long distances is an attractive prospect for retrieving the local variations of near-surface properties. This is particularly valuable for areas impacted by induced seismicity, as is the case in the Groningen Province in the north of The Netherlands, where near-surface properties, mostly composed of clays and peats, play an essential role on the amount of damage on the very near-surface and the structures built on it. Installing fibre-optic cables for passive and active measurements is valuable in this situation. We installed multiple cables containing different fibre configurations of straight and helically wound fibres, buried in a 2-m deep trench. The combination of the different fibre configurations allows us to obtain multi-component information. We observe differences in the amplitude and phase information, suggesting that these differences can be used for separating the different components of the wave motion. We also see that using enhanced backscatter fibres, reflection images can be obtained for the helically wound fibre as well as the straight fibre, despite the decreased broadside sensitivity for the latter.
The results of an experiment aimed at identifying the nature of major noise sources within an urban area are described. We found the strongest noise source to be an irrigation pump located adjacent to the geophones. The noise from the pump had a narrow bandwidth centered at 75 Hz with a duration of 5 minutes every 17 and 34 minutes during the day and night, respectively. Traffic noise was mainly restricted to between 10 and 25 Hz, with its strength decreasing between 9 p.m. and 6 a.m. Passing aircraft resulted in noise between 30 and 200 Hz lasting about 1 minute. Electrical noise was observed at the supply frequency of 50 Hz, although additional noise at 45 Hz also was observed. Given these results we recommended that acquisition within the area should be restricted to late evening or early morning, receiver locations should be selected to avoid strong localized sources of electrical and/or mechanical noise, and any cables associated with the recording system should be as short as possible (although nodal systems are preferable). If nodal systems are deployed for logistical reasons, real-time noise monitoring should be deployed to identify and avoid bursts of high-amplitude, short-duration noise.
...
The results of an experiment aimed at identifying the nature of major noise sources within an urban area are described. We found the strongest noise source to be an irrigation pump located adjacent to the geophones. The noise from the pump had a narrow bandwidth centered at 75 Hz with a duration of 5 minutes every 17 and 34 minutes during the day and night, respectively. Traffic noise was mainly restricted to between 10 and 25 Hz, with its strength decreasing between 9 p.m. and 6 a.m. Passing aircraft resulted in noise between 30 and 200 Hz lasting about 1 minute. Electrical noise was observed at the supply frequency of 50 Hz, although additional noise at 45 Hz also was observed. Given these results we recommended that acquisition within the area should be restricted to late evening or early morning, receiver locations should be selected to avoid strong localized sources of electrical and/or mechanical noise, and any cables associated with the recording system should be as short as possible (although nodal systems are preferable). If nodal systems are deployed for logistical reasons, real-time noise monitoring should be deployed to identify and avoid bursts of high-amplitude, short-duration noise.