Two opposite waves make a standing wave
Add two plane waves of equal amplitude travelling in opposite directions and the travelling parts cancel. What is left keeps a fixed shape in space and only rises and falls in time. The pressure is always zero where ; these points are pressure nodes. It swings most where , the pressure antinodes.
The velocity follows from the equation of motion. It has the shape and lags the pressure by a quarter period. So a pressure node is a velocity antinode, a quarter wavelength away from the nearest pressure antinode. In a standing wave, a “node” always needs the name of the quantity.
Source: R. Barnkob · M. Settnes and H. Bruus
Resonance between hard walls
Liquid cannot flow through a hard wall, so the normal velocity there is zero: . Both side walls, and , must satisfy this, so the channel width has to be a whole number of half wavelengths.
The silicon–glass chip of Barnkob and co-workers (2012) has a channel wide and high. With ideal hard walls the resonance would be at 1.985 MHz; they drove the chip at 1.940 MHz, about 2 % lower. A real chip is not an ideal hard-walled box, which is why experiments sweep the frequency to find the resonance.
Source: R. Barnkob · M. Settnes and H. Bruus
Drum, plate and liquid: three standing waves, three kinds of node
Two other experiments on this site show standing waves, but something different vibrates in each. A drum skin is a stretched membrane: what moves is its sideways displacement, and tension pulls it back. The natural frequencies of a round drum come from zeros of Bessel functions, so the overtones are not whole multiples of the fundamental; the first overtone is about 1.59 times the fundamental.
A Chladni plate is a metal plate with bending stiffness, and bending pulls it back. For a square plate with simply supported edges the natural frequencies grow as , faster with mode number than a membrane’s. Sand is thrown off where the plate moves and settles on the lines that stay still. Those are displacement nodes.
The liquid in a channel is a pressure field. What oscillates is the scalar pressure, and the liquid moves back and forth along the direction of travel: a longitudinal wave. From the next chapter on, beads stiffer and denser than water are pushed to the pressure nodes, which is exactly where the liquid moves fastest. Both “collect at a node”, but Chladni sand stops where the displacement is zero, while beads in an acoustic trap stop where the pressure is zero and the velocity is largest.
The mechanical lattice experiment is yet another case: discrete masses and springs, where the frequency stops being proportional to the wavenumber once the wavelength approaches the spacing. The continuum acoustics in this course holds only for wavelengths much longer than any microscopic structure.
Source: R. Barnkob · M. Settnes and H. Bruus
Worked example: pressure nodes in a 377 µm channel
Take a sound speed of 1497 m/s. For , , the wavelength is and the pressure node sits at . For the frequency doubles to 3.97 MHz and the nodes are at 94.3 µm and 282.8 µm.
Take an energy density . From , . At the pressure node the liquid’s velocity amplitude is and its displacement amplitude .
That displacement is more than two hundred times smaller than a 5 µm bead. The bead is not washed to the node by the liquid: in one period it only rocks back and forth by tens of nanometres. What moves it to the node is a second-order radiation force that survives time averaging, the subject of Chapter 5.
Source: R. Barnkob · M. Settnes and H. Bruus