Weird Science

Acoustic Wave Interference

Polish ver­sion is here

Aco­u­stic Wave Inter­fe­rence

What is inter­fe­rence? Most peo­ple have heard this term and often asso­ciate it vagu­ely with waves or vibra­tions. Howe­ver, a phy­si­cist would define it pre­ci­sely as the phe­no­me­non of over­lap­ping waves, lea­ding to an incre­ase or decre­ase in the ampli­tude of the resul­tant wave. Inter­fe­rence occurs with all types of waves (elec­tro­ma­gne­tic, mecha­ni­cal, de Bro­glie, etc.) and in all media where such waves can pro­pa­gate.

This phe­no­me­non fol­lows the prin­ci­ple of super­po­si­tion, which sta­tes that the resul­tant ampli­tude A at any point where par­tial waves over­lap is given by the equ­a­tion:

Ilustracja

where: A1, A2 - ampli­tu­des of the par­tial waves, and φ - the phase dif­fe­rence between the two waves.

As shown, the resul­tant wave can have a maxi­mum ampli­tude of A = A1 + A2 when φ = 2k. In this case, the pha­ses of both waves are per­fec­tly ali­gned: cor­re­spon­ding points of the par­tial waves (cre­sts and tro­u­ghs) coin­cide in space and time. Thus, the resul­tant ampli­tude is the sum of the ampli­tu­des of both par­tial waves, resul­ting in con­struc­tive inter­fe­rence.

For oppo­site pha­ses (φ = 2k + 1), the resul­tant ampli­tude is mini­mi­zed, descri­bed by A = A1 - A2. Here, the waves are out of phase, and their oppo­site ele­ments (cre­sts and tro­u­ghs) over­lap, cau­sing destruc­tive inter­fe­rence. If both par­tial waves have the same ampli­tude, the resul­tant ampli­tude is A = 0.

Gene­ra­ting Aco­u­stic Waves Using Software

A sim­ple way to gene­rate aco­u­stic waves with pre­ci­sely con­trol­led fre­qu­ency and phase is by using a com­pu­ter and appro­priate software. While there are many software-based gene­ra­tors, we will take a sli­gh­tly unco­nven­tio­nal appro­ach and use Auda­ci­ty—a music edi­ting tool. This advan­ced, multi-track audio edi­tor is distri­bu­ted under the GNU GPL license (ava­i­la­ble for free down­load). It is ava­i­la­ble for mul­ti­ple ope­ra­ting sys­tems, inc­lu­ding Unix/Linux, Micro­soft Win­dows, and Mac OS.

After down­lo­a­ding and instal­ling Auda­city, you will need the pro­ject file I have pre­pa­red. You can down­load it here. After extrac­ting the archive, you will find a fol­der con­ta­i­ning the file "inter­fe­ren­cja.aup." Dou­ble-clic­king it sho­uld launch Auda­city with two loa­ded audio wave­forms. It sho­uld look like this:

We see two audio wave­forms: the upper one is for the left spe­a­ker, and the lower one is for the right spe­a­ker. To play the audio, press the green play but­ton on the top tool­bar. Notice that the fre­qu­en­cies of these sounds dif­fer sli­gh­tly: 440Hz for the left chan­nel and 441Hz for the right chan­nel. The dif­fe­rence between the fre­qu­en­cies is 1Hz. The signal level rema­ins con­stant thro­u­ghout the dura­tion of the sound, as seen in both chan­nels. Now, turn on your spe­a­kers and play the audio. Does the sound appear uni­form? Not at all! You can cle­arly hear alter­na­ting moments of incre­a­sed and decre­a­sed loud­ness. By liste­ning care­fully, you will notice that the time between two moments of decre­a­sed ampli­tude (or incre­a­sed ampli­tude) is one second, indi­ca­ting an ampli­tude modu­la­tion fre­qu­ency of 1Hz. Inte­re­stin­gly, this fre­qu­ency is exac­tly the dif­fe­rence between the two gene­ra­ted fre­qu­en­cies. Why?

Let’s ana­lyze why we hear these varia­tions in loud­ness. Each spe­a­ker rece­i­ves a ste­ady signal with no ampli­tude fluc­tu­a­tions. You can verify this by muting one chan­ne­l—you’ll hear a con­ti­nu­ous sound. This indi­ca­tes that the varia­tions are due to the inte­rac­tion of both fre­qu­en­cies. To inve­sti­gate this fur­ther, use the zoom tool (a small magni­fy­ing glass with a plus sign on the top tool­bar) to zoom in until the sinu­so­i­dal wave­form is cle­arly visi­ble:

We see two text­book sine waves. Their fre­qu­en­cies dif­fer sli­gh­tly, altho­ugh this dif­fe­rence is not easily noti­ce­a­ble at this scale. Ini­tially, both waves are in phase at t = 0s (as indi­ca­ted by the time scale above the wave­forms). Their cre­sts and tro­u­ghs align per­fec­tly, resul­ting in con­struc­tive inter­fe­rence that incre­a­ses the resul­tant ampli­tude. Note that the lower wave­form has a sli­gh­tly higher fre­qu­ency, cau­sing its cre­sts to gra­du­ally shift ahead of the upper wave­form's cre­sts. Altho­ugh this shift is minor at this point, let's scroll to t = 0.5s (half the period at 1Hz):

The situ­a­tion chan­ges signi­fi­can­tly. Now, the wave­forms are in oppo­site pha­ses (cre­sts align with tro­u­ghs and vice versa). Their ampli­tu­des can­cel out, cau­sing destruc­tive inter­fe­rence and a signi­fi­cant drop in loud­ness.

These effects repeat alter­na­tely every second (check it!). This results in an ampli­tude modu­la­tion fre­qu­ency of 1Hz. As we obse­rved, this fre­qu­ency is always the dif­fe­rence between the fre­qu­en­cies of the two wave­forms. The two inter­fe­ring fre­qu­en­cies pro­duce a resul­tant wave whose oscil­la­tion fre­qu­ency is 1Hz. Let's prove this by sum­ming the displa­ce­ments of both sine waves from their equ­i­li­brium posi­tions. To do this, open the track menu (on the left side of the upper wave­form; click the black trian­gle next to the track name) and select "Make Ste­reo Track." Then, from the top menu, cho­ose Tracks - Mix - Mix Ste­reo Down to Mono. This sums the ampli­tu­des, as we discus­sed ear­lier. The result sho­uld look like this:

This result con­firms our obse­rva­tions. The ampli­tude chan­ges with a fre­qu­ency of 1Hz, with maxi­mum rein­for­ce­ment at full seconds and can­cel­la­tion in between. The prin­ci­ple of super­po­si­tion holds true. The ani­ma­tion below illu­stra­tes this pro­cess in detail: the red and blue wave­forms repre­sent the par­tial waves (left and right chan­nels), while the black wave­form repre­sents the resul­tant wave.

Ilustracja

The phe­no­mena we obse­rved here also occur with all other types of waves.

Enjoy expe­ri­men­ting! :)

Fur­ther rea­dings:

Marek Ples

Aa