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Rob Long, Peter Cawley and Mike Lowe Press PGDN when arrow appears Acoustic wave propagation in buried iron water pipes WITE Programme

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Work reported in this presentation 1. Predict wave propagation characteristics in water pipes 2. Validate predictions using tests on buried water mains in streets.

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Presentation Content 1: Introduction Motivation for research 2: Predictions 2:1 Dispersion curves for guided waves in water pipes 2:2 Mode shapes of fundamental modes 2:3 Phase velocity dispersion of fundamental modes 2:4 Effect of pipe bore variation on velocity dispersion 2:5 Effect of soil properties on mode attenuation 2:6 Effect of joints and fittings on mode attenuation 3: Validations 3:1 Experimental technique 3:2 Mode phase velocity measurement 3:3 Mode attenuation measurement 3:4 Soil property measurement 3:5 Experimental results 4: Summary

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Leakage from water pipes is a major issue concerning all water companies Leaking pipes should be located And Repaired However many leaks are not so obvious from the surface Introduction Motivation for research

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One method is to locate leaks by acoustic signal analysis Acoustic noise that arises from the leak propagates through the system Accelerometers are mounted typically on valve stems to record the signals Data recorded results in two signals These two signals are cross correlated so as to obtain a time delay t t V. t d d Z 2 d = z - (V.t ) The distance to the leak d from one monitoring point is then formulated by assuming that the leak noise propagates at a non dispersive (ie does not vary with frequency) velocity V

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How reasonable is it to assume that leak noise propagates non dispersively ? If we are considering sound propagation in bulk materials that have no boundaries then it would be a reasonable assumption For sound propagation in structures such as pipes reflection and refraction of waves at the boundaries sets up a series guided waves. In the case of leak noise the vibrations recorded by the accelerometers are dominated by a guided wave that predominantly propagates in the water contained within the pipe With guided waves we need to look at the dispersive characteristics

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We use the Disperse software developed by the NDT Group Imperial College to obtain dispersion curve numerical solutions Lets solve dispersion curves for a water filled 250mm bore 10mm wall thickness cast iron pipe surrounded by a vacuum The solution shown plots the phase velocity of each mode as a function of frequency Modes in red are axially symmetric modes while those in blue are non axially symmetric modes Predictions Dispersion curves for guided waves in water pipes

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Let us now examine the mode shapes of three modes that exist at low frequencies We will first look at the characteristics of the so called L(0,1) fundamental longitudinal mode The Mode Shape window shows radial displacements and axial displacements in the water and iron layers for the given mode at the given frequency. 0 - + water iron For L(0,1) at near zero frequency the radial displacements are insignificant in both the water and iron layers. While axial displacements predominantly occur in the pipe wall. Watch the animation of the mode displacements for L(0,1) at near zero frequency. Notice the displacements are axially symmetric, predominantly occur in the pipe wall and the motion is purely extensional/longitudinal. 0 - + Next we will look at the characteristics of the so called F(1,1) fundamental Flexural mode at near zero frequency. Notice the axial displacements for F(1,1) are insignificant.While the radial displacements dominate in both the water and iron layer water iron 0 - + water iron Watch the animation of the mode displacements for F(1,1) at near zero frequency. Notice the motion of the mode behaves as if bending/flexural. Finally we will look at the 1 mode shapes The axial displacements occur predominantly in the water in the pipeThe radial displacements are insignificant in the water and iron layers Watch the animation of the mode displacements for 1 at near zero frequency. Notice the displacements are axially symmetric, predominantly occur in the water and the motion is purely extensional/longitudinal. Mode shapes of fundamental modes

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Let us now examine the dispersion characteristics of the three modes that exist at low frequencies The fastest mode shown is the so called L(0,1) mode. L for longitudinal- mode displacements at low frequencies predominantly longitudinal 0 for zero phase change over the circumference ie axially symmetric 1 for the first Longitudinal mode that appears L(0,1) Notice how the phase velocity of the L(0,1) mode varies with frequency (dispersion). For 10 inch pipe the L(0,1) mode is particularly dispersive about 4kHz to 6kHz. 0kHz Vph 4048m/s2kHz Vph 4031m/s4kHz Vph 3900m/s6kHz Vph 1950m/s8kHz Vph 1650m/s Next the so called F(1,1) mode. F for flexural- since mode displacements at low frequencies are as if the pipe is being flexed 1 for one phase change over the circumference ie non axially symmetric 1 for the first Flexural mode that appears F(1,1) 0kHz Vph 0m/s2kHz Vph 1102m/s4kHz Vph 785m/s6kHz Vph 724m/s8kHz Vph 771m/s For 10 inch pipe the phase velocity of the F(1,1) mode is dispersive particularly about 0kHz to 2kHz. 0kHz Vph 1212m/s2kHz Vph 1152m/s4kHz Vph 829m/s6kHz Vph 725m/s8kHz Vph 829m/s 11 Finally the alpha 1 mode. It is the low frequency asymptote of the 1 mode that corresponds to velocity that leak location techniques assume leak noise to propagate at. For 10inch pipe the 1 mode is particularly dispersive about 2kHz to 4kHz Phase velocity dispersion of fundamental modes

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Frequency kHz Phase Velocity m/ms 0 1 2 3 4 0246810 Let us compare dispersion curves for different bore pipes. First the dispersion curves for a 6 inch bore pipe showing the L(0,1), F(1,1) and 1 modes Followed by the curves for a 10 inch bore pipe Then those for a 24 inch bore pipeFollowed finally by those for a 36 inch bore pipe Notice that the effect of an increase in bore size shifts the dispersion curves to the left for L(0,1) 1 and F(1,1) For a given ratio of pipe-wall thickness to pipe bore size we can plot one set of curves as a function of Frequency-radius product for all pipe sizes. Effect of pipe bore variation on velocity dispersion

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Up to now we have considered the wave propagation only for a pipe surrounded by a vacuum Now we need to look at the effect of embedding the pipe in a surrounding medium Dispersion Curves shown Coloured curves for water filled pipe surrounded by water (w-p-w) Black dotted curves for water filled pipe surrounded by a vacuum (w-p-v) For w-p-w system L(0,1) Phase velocity dispersion is very similar to w-p-v at lower frequencies then follows higher order Longitudinal modes at higher frequencies For w-p-w system a phase velocity is very similar to w-p-v at lower frequencies F(1,1) phase velocity is slower than w-p-v due to the surrounding medium Now we will consider the effects of surrounding the pipe with soil. Typical soils are either saturated such as a clay slurry or unsaturated such as unconsolidated sand or clay Both types of soil will be characterised by density and the bulk longitudinal C L and shear C S velocities in the soil If the phase velocity of a mode is above C L or C S in the soil then the mode will couple to leaking longitudinal or shear waves in the soil These leaking waves carry away energy into the soil leading to mode attenuation First we will plot attenuation due to leakage for a pipe surrounded by saturated soil where =1000kg/m 3, C L =1500m/s and C S varies from Frequency-radius (MHz-mm) Attenuation (dB-mm/m) Frequency-radius (MHz-mm) Attenuation (dB-mm/m) Frequency-radius (MHz-mm) Attenuation (dB-mm/m) 25m/s25 to 50m/s25 to 75m/s25 to 100m/s mode F(1,1) modeL(0,1) mode For saturated soil All modes couple to leaking shear waves in the soil. Only L(0,1) couples to leaking longitudinal waves in the soil. Attenuation due to leakage increases for all modes with increasing bulk shear velocity in the soil Of the three modes the mode is less attenuated at low frequencies such that it would be expected to become the dominate mode in received signals for long propagation distances mode Effect of soil properties on mode attenuation

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Next we will plot attenuation due to leakage for a pipe surrounded by unsaturated soil where =1900kg/m 3, C S =100m/s and C L varies from 250m/s 250 to 500m/s250 to 750m/s250 to 1000m/s Frequency-radius (MHz-mm) Attenuation (dB-mm/m) Frequency-radius (MHz-mm) Attenuation (dB-mm/m) Frequency-radius (MHz-mm) Attenuation (dB-mm/m) mode F(1,1) modeL(0,1) mode mode Again of the three modes the mode is less attenuated at low frequencies such that it would be expected to become the dominate mode in received signals for long propagation distances

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soil pipe water In practice a water main will have fittings such as Joint r Branch a joints every few metres that connect individual lengths and tees where pipes of bore r branch off to another pipe of bore a As a mode encounters such fittings attenuation will occur due to scattering and will be a function of wavelength and hence frequency. First we look at mode propagation across a joint. We consider a solid metal to metal contact joint and a soft joint where the joint is filled with sealant or rust. The water borne mode suffers little attenuation for either joint whereas attenuation of the pipe-wall borne L(0,1) mode is significant particularly for the soft joint Next we look at mode propagation passed a branch with ratios of branch bore a over pipe bore r of 0.125 to 1. A branch acts as a high pass filter particularly when the branching is large. Effect of joints and fittings on mode attenuation

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Alnwick (Northumberland Water) Greenwich (Thames Water) Imperial College Guildford (Thames Water) Experiments were performed on buried water pipes at various sites in the UK to measure mode phase velocity and attenuation Pipes of various bore sizes buried in different soils were chosen for the measurements At a given site pits were dug to get access to the full circumference of the pipe in 3 locations At one location an automatic tapper device was mounted on the pipe surface to input low frequencies vibrations At 2 other locations 4 off accelerometers were mounted equi-spaced around the circumference to monitor propagating signals Tap on pipe to excite LF modes Monitor sound with 4 off accelerometers Monitor sound with 4 off accelerometers Joint Path length Z Measurements were conducted for a pipe buried in soil and for a pipe surrounded by aggregate for a pipe surrounded by air Excavation soil pipe water Validations Experimental technique

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Received signal at location a and b are windowedThe FFTs of each signal is computed Location a(t) Location b(t) The Phase spectrum is then computed FFT A*( ) FFT B( ) Phase spectrum The Phase spectrum is unwrapped Unwrap ( ) The Phase velocity V ph is computed from which the group velocity V gr can be obtained Mode phase velocity Measurement

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Mode attenuation Measurement

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We also need to evaluate the acoustic properties of the soil that surrounds the pipe We use the pipe material and measured pipe dimensions to produce predictions which we will compare to experimental results At each site the material of the pipe was noted Pipe wall thickness was measured by the pulse-echo technique As was the pipe circumference Soil property measurement

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We need a technique to evaluate the acoustic properties of near surface unconsolidated material Testing something like dry sand would be somewhat challenging Whereas wet sand would be a bit more manageable

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We use a technique that infers the bulk velocity in the soil from the attenuation characteristics of a mode that propagates down a bar embedded in the soil Piezo electric element Backing Axial excitement We take a steel bar about 1m long with a piezo electric element bonded at one end An electrical pulse is applied across the piezo electric element resulting in an axial excitement in the bar This mechanical pulse propagates down the bar Is reflected off the other end is received at the piezo electric element where an electrical signal is produced and saved soil Bar The bar is then embedded in the soil up to a length L L Signal for bar in air The pulse again propagates down the bar Into the embedded portion where it attenuates due to leakage Is reflected, attenuates in the embedded portion again And is received at the element Signal for embedded bar Attenuation = [20 log (R soil/Rair)]/2L The attenuation characteristics of the mode are then obtained by dividing the FFT of the signal for a bar in soil by that for a bar in air

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The measured attenuation is then plotted A series of predicted dispersion curves are solved for soils with different values of C L and C S in the soil The predicted dispersion curve that best matches the measured attenuation infers the soil properties Frequency (MHz) Attenuation (dB/m)

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Goals To verify predicted alpha mode phase velocity for a pipe surrounded by soil, air and aggregate To verify predicted alpha mode attenuation for a buried pipe Site location in Guildford UK Tests conducted over 3 days in June 2002 A number of tests have been carried out on various water mains at sites in the UK. Presented are results from Pipe details Path Length 15m Ductile Iron 6 inch bore 6.5mm wall thickness Measured soil Properties Density 1900kg/m 3 C L soil 900m/s C S soil 80m/s Frequency (MHz) Attenuation (dB/m) Experimental Result

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Verification of mode phase velocity Frequency (kHz) Phase Velocity (m/s) Predicted dispersion curves for pipe surrounded byairand clay Experimental dispersion curves for pipe surrounded byairclay and aggregate Predicted dispersion verified

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Verification of mode attenuation due to leakage Predicted dispersion curves for pipe surrounded byairand aggregate Experimental dispersion curves for pipe surrounded byairand aggregate Predicted dispersion verified Frequency (kHz) Attenuation (dB/m)

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Identified what modes propagate over short and long path lengths on different pipe diameters Introduced new technique for measuring bulk velocities in near surface soils Verified predicted dispersion curves Main project achievements covered in this presentation Summary

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