Imaging of propagating wave fronts resulting from ultrasonic pulses incident on heel bones using refracto-vibrometry Acoustical Society of America Meeting.

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Imaging of propagating wave fronts resulting from ultrasonic pulses incident on heel bones using refracto-vibrometry Acoustical Society of America Meeting Boston, MA June 29, 2017 Thomas Huber Physics Department, Gustavus Adolphus College, St. Peter, MN Matthew Huber, Brent Hoffmeister Physics Department, Rhodes College, Memphis, TN

Introduction Osteoporosis detection using ultrasound wave propagation through calcaneus heel bone Refracto-Vibrometry for optical measurement of full-field traveling ultrasonic wavefronts Visualization of ultrasonic wave interaction with heel bone Conclusions

Osteoporosis Screening using Ultrasound Propagation through Heel (Calcaneus) Speed of ultrasound wave through bone is slightly higher than speed of sound in water Wave speed depends on bone density and strength, so can be used for detection of osteoporosis Measure time-of-flight of ultrasonic pulse (launched from water) through bone; detected using 2nd transducer Commercial ultrasonic heel scanners are an inexpensive, cost-effective method for osteoporosis screening One research area: accurately characterize bone health using backscattered ultrasound. This may enable direct testing of back or hip which are difficult to measure with transmission. Goal of current project: Full-field in vitro measurements to visualize the traveling ultrasonic waves as they interact with the calcaneus (heel bone)

Conventional Ultrasonic Heel Measurements (Piezo Transducers for Transmit and Receive) Receiver Voltage: After Propagation Through Bone Ultrasound Transmitter Ultrasound Receiver Max: 100 mV Arrival: 76.5µs Receiver Voltage: Reference, Bone Removed Max: 2V Shift in arrival time and changes in amplitude/frequency can be used to estimate bone parameters Arrival: 77.8µs

Scanning Laser Doppler Vibrometry Uses Doppler shift of laser reflected off target surface to measure vibration Scanning mirrors allows measurement laser to be directed at multiple scan points Software allows surface plots for visualization of operating deflection shapes Common method utilized for modal testing However, we are not going to be talking about vibration measurement today... We are repurposing the scanning vibrometer to measure ultrasonic waves in water

Refracto-Vibrometry: Laser Measurement of Ultrasonic Waves Heel Bone Sound is a compressional wave: changing density changes the index of refraction Vibrometer beam (~200µm diameter) passes through tank off retroreflector When sound wave passes through vibrometer beam, changes the optical path length, ∅ ∅= 𝑝𝑎𝑡ℎ 𝑛 𝑠 𝑑𝑠 Although there is no mechanical vibration in the tank, the Polytec vibrometer software interprets and displays the time-varying density as a “deflection shape” Thus, the scanning vibrometer can be used to visualize traveling ultrasound pulses

Top View Vibrometer View Refracto-Vibrometry for Calcaneus Heel Bone Ultrasound emitted from 500kHZ transducer (on left) For this measurement, no Receive transducer in tank Vibrometer beam directed at one of ~15000 scan point locations Vibrometer signal sampled at 12.8MHz after pulse emission Average 100 ultrasound pulses at each scan point Repeat for all 15000 scan points: acquisition time of 2 hours! Heel Bone Vibrometer View

Top View Vibrometer View Potential Advantages of Refracto-Vibrometry Very high bandwidth (flat response to about 20 MHz) Non-invasive: no distortions due to receive transducer Each scan point (about 200µm diameter) is narrow path integral with full time-domain response Create full-field videos of traveling ultrasonic waves Top View Heel Bone Vibrometer View Heel Bone

Refracto-Vibrometry: For each scan point, full time-domain measurement Vibrometer Voltage: With Bone In Tank Max: 40 mV Scan Point Arrival: 76.5µs Vibrometer Voltage: Reference Bone Removed Max: 5V 1.3 µs shift in arrival time consistent with measurements with piezo receiver Arrival: 77.8µs

Comparison of Single Refracto-Vibrometry Scan Point and Piezo Transducer Vibrometer Voltage: With Bone In Tank Max: 40 mV Scan Point Arrival: 76.5µs Piezo Transducer Voltage: With Bone in Tank Vibrometer gives similar pulse shape with transducer. Receiver with larger bandwidth and freedom from reflection/damping artifacts

Refracto-Vibrometry Video: Empty Tank (Reference) Superimposed dataset from 15,000 scan points Scan Point Color scaling: Zero volts is black Increasing positive voltage red (Negative voltages not displayed) Time-domain measurement at indicated scan point

Refracto-Vibrometry Video: With Bone in tank Scan Point Color scaling: Zero volts is black Increasing positive voltage blue Over range goes to white (Negative voltages not displayed) Time-domain measurement at indicated scan point

Refracto-Vibrometry: Superimposed Videos Scan Point Color scaling: Zero volts is black Red coloration for reference (bone removed) Blue coloration with bone in tank Time-domain with bone in place Time-domain for reference (no bone)

Refracto-Vibrometry: Superimposed Videos “Red wave” passing through bone is artifact of video overlay Synchronization of incoming and non-interacting waves Speed of sound larger in bone than water: blue emerges before red Emitted wave is planar even though non-uniform thickness; backscatter is non-planar Time-domain with bone in place Time-domain for reference (no bone)

Refracto-Vibrometry: Superimposed Videos Time-domain with bone in place Time-domain for reference (no bone)

For more info and link to video Conclusions Refracto-vibrometry can be used for full-field videos of traveling ultrasound Non-invasive, quantitative measurements without interference from a receiver Emitted wave from bone is time-advanced relative to empty target Time offset is consistent with conventional piezoelectric receiver Could be utilized for estimates such as speed of sound in bone Emitted waves are nearly planar Acknowledgements For more info and link to video on Youtube Gustavus Physics Students: Matt Mehrkens and Ben Rorem This material is based upon work supported by the National Science Foundation under Grant Nos. 1300591 and 1635456 Any opinions, findings, and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation.