Topic 6 of 6
Using ultrasound
Ultrasound is sound above the usual upper limit of human hearing, conventionally above about 20 kHz. Its echoes can locate reflecting boundaries.
1 kHz = 1000 Hz, so 20 kHz is 20000 Hz. Ultrasound is still a mechanical sound wave and needs a material medium. The high frequency does not make it electromagnetic radiation.
Underwater echo sounding
An active echo-sounding system can emit a short ultrasound pulse into water. Its transducer converts an electrical signal into sound and converts a received echo back into an electrical signal. The time between emission and reception indicates the distance along the beam when the sound speed is known.
For a vertical beam reflected from the seabed, the pulse travels down from the transducer and back up. Using an approximately uniform water sound speed, depth below the transducer = vt/2.
Sonar calculation
A vertical return after 0.060 s
Use the supplied speed 1500 m/s. The round-trip interval is 0.060 s.
d = 1500 x 0.060 / 2 = 45 m.
This is the seabed distance below the transducer. It is not automatically the depth below the sea surface if the transducer is submerged. A sloping beam would measure distance along its path rather than the vertical depth.
This example uses an active sonar system with ultrasound. Sonar more broadly uses sound: some systems listen without emitting a ranging pulse, and not every sonar frequency is ultrasonic.
Use reflected pulses to locate a boundary
Active echo sounding with ultrasound
Supplied sound speed 1500 m/s; return delay 0.060 s. A vertical beam locates the seabed 45 m below the transducer.
A probe receives echoes from tissue boundaries
This supplied uniform-speed model uses 1540 m/s along the path. Depths are measured from the probe face; the coupling layer is included in this simplified path.
A: 3.08 cm, echo after 40 microseconds. B: 6.16 cm, echo after 80 microseconds.
Locate soft-tissue boundaries
A scanning probe sends ultrasound pulses into the body and receives returning echoes. At a boundary between tissues, some of a pulse can reflect while some continues farther. Later echoes can therefore return from deeper boundaries.
- Emit a pulse: record its emission time.
- Receive echoes: identify the delays of the returned signals.
- Estimate depth: combine each round-trip delay with an appropriate assumed sound speed.
- Build an image: combine information from many beam positions. Echo strength as well as timing contributes to the displayed image.
One echo does not give a complete photograph of an organ. The system assembles information from many reflections. In the simple model here, timing locates a boundary along the beam; a taller signal does not by itself mean a deeper boundary.
Why the probe uses coupling gel
Gel fills gaps between the probe and skin so that sound can pass into the body more effectively. An intervening air layer would cause strong reflection at the boundaries and reduce transmission. This does not mean that air cannot carry sound; the change between materials affects how much is transmitted or reflected.
Soft-tissue calculation
An echo after 80.0 microseconds
Use the supplied uniform sound speed 1540 m/s. One microsecond (µs) is 0.000001 s, so 80.0 µs = 0.0000800 s.
- Complete path: vt = 1540 x 0.0000800 = 0.1232 m.
- Boundary depth: d = 0.1232/2 = 0.0616 m = 6.16 cm.
Under the same model, a 40 µs echo comes from a nearer boundary at 3.08 cm. These depths are measured from the probe along the beam. The supplied speed is a model value, not a claim that every tissue has exactly the same sound speed.
Convert the time and retain the return path. Microseconds are millionths of a second. Multiplying speed by an echo delay gives the complete path; the boundary depth is half of it in this model.