Name ……………………………………………………… Advancing Physics AS Chapter 3.2a Signalling Student Notes August 2008 John Mascall The King’s School, Ely Section 3.2 Signalling with electromagnetic waves: radio spectrum; polarisation; spectrum of a signal; bandwidth Learning outcomes ● Communication with electromagnetic waves uses frequencies from a few thousand hertz to infrared frequencies and above, divided into bands used for different purposes. ● Electromagnetic waves can be polarised; the orientation of a detector has to take this into account. ● A signal can be analysed into the frequencies it consists of – its spectrum. ● A signal channel has a capacity, the rate at which it can transmit information, measured in bits per second. ● The bandwidth of a signal is the range of frequencies in its spectrum. The larger the bandwidth the greater the rate of transmission of information. ● Noise limits the rate at which information can be transmitted. The radio spectrum It is worth recalling details of the electromagnetic spectrum (page 6 of the student text) with particular reference to communication wave bands such as radio. Display Material 80O OHT 'Signal bands for communication' Communication wavebands frequency wavelength 10 km 30 kHz LF low frequency navigation, radio beacons, long-distance broadcasting MF medium frequency national broadcasting, aeronautical nav igation HF high frequency long-distance broadcasting, amateur radio, maritime radio VHF very high frequency FM radio, mobile radio communications UHF ultra high frequency telev ision, mobile telephone networks SHF super high frequency satellite links, ground microwave links, radar 1 km 300 kHz 3 MHz 30 MHz 100 m 10 m 300 MHz 3 GHz 30 GHz 300 GHz 1m 100 mm 10 mm EHF extremely high radar, radio astr onomy far infrared infrared astronomy 1 mm 100 m 3 THz mid infrared infrared astronomy near infrared optical fibre, remote controls, bar codes, CD player 10 m 30 THz 300 THz 1 m Communications use wave lengths of between 1m and 10km Page | 2 The following paragraph taken from Activity 110H Home Experiment ‘Home experiments with radio and television signals’ illustrates the meaning of bandwidth: Do you have a portable FM radio with dial rather than push-button tuning? If so, spin the dial and notice the frequencies at which stations come up. Typical frequencies are in the range 90–100 MHz or so. The strong signals will not be closer than 0.2 MHz (200 kHz) apart. Notice the range of frequencies over which you can still hear a strong signal as you tune the radio 'through' its frequency. It may be about 0.1 MHz either side of the correct frequency. That 'bandwidth' allows for the variations in frequency produced by the radio waves carrying the audible signal. Polarisation It is convenient to start with portable television aerials, noting their polarisation (and directionality). We revisit Activity 110H Home Experiments 'Home experiments with radio and television signals'. You may wish to carry out further work on this at home. Polarisation with waves on a rope, light, 3 cm microwaves, and 1 GHz UHF radio waves should all be demonstrated using Activity 120P Presentation 'Polarisation of waves'. Display Material 90O OHT 'Polarisation' Polarisation by scattering should be demonstrated. When the permitted direction of vibration or polarisation of the filter is parallel to the direction of the polarisation of the wave, it is transmitted by the filter. When the permitted direction of vibration or polarisation of the filter is perpendicular to the direction of the polarisation of the wave, it is absorbed or reflected but not transmitted. Page | 3 The following activities are optional: Activity 130E Experiment 'Polarisation by scattering' Activity 140D Demonstration 'Polarisation of reflected light' Spectra of signals It is useful to start with the spectra of sounds. Sounds can be synthesised and the sound spectra analysed. In this part it is important to keep going backwards and forwards between waveform and spectrum, and considering the relation between them. You can try Activity 150H Home Experiment ‘Telling frequencies apart’ which shows that the ear can sort out a sound into the different frequencies that sound is made up of. Your eyes are unable to do this. If you shine two differently coloured lights onto a screen you will see one new colour and not two mixed colours. Activity 170E Experiment ‘Spectrum analysis: simple signals’ starts with simple waveforms from a signal generator. Different signals are then added to look at the effect of having more than one frequency. A spectrum analyser can be used to identify which frequencies are present in the waveform. In Activity 160S Software Based 'Filtering sounds' you can make a sound with two frequencies, hear them both, and then get rid of one of them. This exercise uses the Audacity software. In Activity 180S Software Based 'Spectrum analysis: Going further' we use Multimedia Sound to carry out spectral analysis on more complex waveforms. The bandwidth of a signal’s spectrum is the range of frequencies it covers. This idea can be reinforced by using an exercise on listening to sounds with reduced bandwidth to simulate the problems experienced by the deaf. Try Activity 190S Software Based 'Hearing impairment: Using a digital filter'. The healthy human ear is able to hear sounds with frequencies from a few tens of hertz to between 15 and 20 kHz. This range is greatly reduced for people who have hearing difficulties and this demonstration will give you some idea of what such a partially deaf person might hear. Try Activity 210S Software Based 'Cleaning up a sound' Being able to see a recorded sound as a complex of frequencies helps to suggest strategies for identifying and highlighting the sound you intended to record. In this activity you manipulate a sound file that contains wanted and unwanted signals. Activity 220S Software Based 'Building up a sound' involves synthesising a complex waveform from pure tones. Fourier showed that a waveform of any complexity can be broken down into a mixture of waveforms which are pure tones – that is, waves which can be described by simple sines and cosines. In this activity you build up a complex waveform from a series of simple tones. Tone telephones use such mixtures of tones to signal the different dialling numbers. Page | 4 The following sound files from the Advancing Physics CD-ROM may useful. File 10L Launchable File 'Samples of music' File 20L Launchable File 'Samples of everyday sounds' File 30L Launchable File 'Samples of speech' File 40L Launchable File 'Whistle over radio' Much of the work on sounds can be summarised using Display Material 100S Computer Screen 'Atlas of sound spectra' Here you can see the waveforms and spectra of a variety of sounds, some natural and some electronically generated. The oboe The oboe produces a complex sound, with a considerable number of different frequencies in its spectrum. The musical character of the sound is indicated by the discretely spaced frequencies, having simple numerical relationships to one another. The clarinet The clarinet here, like the oboe, produces a range of discrete frequencies simply related to one another. The lower frequencies are rather dominant, but the spectrum extends over a wide range. The xylophone The sound of the xylophone has been caught just as a note is struck. Initially the sound contains a highfrequency 'ringing', but this dies away and the sound becomes the pure tone being struck. Page | 5 The snare drum A drum does not produce a simple musical tone consisting of one or more discrete related frequencies, but instead produces a spectrum covering a wide range of frequencies. The sound has a pitch, decided by the range of frequencies over which the spectrum is centred. A single pure tone An electronically generated 1000 Hz pure sinusoidal oscillation has a simple spectrum: just a single peak at 1000 Hz. Two tones sounding together Tones of 1000 Hz and 3000 Hz were here electronically combined. The spectrum shows two peaks. Page | 6 'White' noise This noise was electronically generated. It makes a 'rushing' sound something like wind in trees or a mountain stream or waterfall. It is called 'white' noise because its spectrum is uniformly spread over the whole audible frequency range. ('Pink' noise has larger low-frequency components.) Single short pulse This single short pulse of 1000 Hz tone, lasting only 5 ms (five cycles) was generated electronically. It is difficult to obtain the 'spectrum' of such a sound, but the spectrum shown does have the important correct feature of spreading over a wider range of frequencies than a continuous pure tone. Page | 7