1 John McCloskey NASA/GSFC Chief EMC Engineer Code 565 Building 23, room E203 301-286-5498 Fundamentals of EMC Time Domain vs.

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Presentation transcript:

1 John McCloskey NASA/GSFC Chief EMC Engineer Code 565 Building 23, room E Fundamentals of EMC Time Domain vs. Frequency Domain

2 Full Demo/Tutorial Video Video of full demonstration/tutorial on NESC Academy website “Effects of Rise/Fall Times on Signal Spectra” Link on GSFC EMC Working Group XSPACES SITE:

3 Purpose of Demo/Tutorial Demonstrate the relationship between time domain and frequency domain representations of signals In particular, demonstrate the relationship between rise/fall times of digital clock-type signals and their associated spectra Fast rise/fall times can produce significant high frequency content out to 1000 th harmonic and beyond Common cause of radiated emissions that can interfere with on-board receivers Can be reduced by limiting rise/fall times

4 Topics Sinusoid: Time Domain vs. Frequency Domain Fourier series expansions of: Square wave Rectangular pulse train Trapezoidal waveform Comparison to measured results for these waveforms Observations

5 Demo 4: Time Domain vs. Frequency Domain

6 Demo 4: Time Domain vs. Frequency Domain (cont.) Equipment Tektronix MDO3104 oscilloscope (built-in signal generator) 2 RG-58 coax cables T connector BNC-N adaptor Setup AFG: 1 MHz sine, square, pulse with 300 ns width (30% duty cycle)

7 Demo 4: Time Domain vs. Frequency Domain (cont.)

8

9

10 Sinusoid: Time Domain vs. Frequency Domain TIME DOMAIN FREQUENCY DOMAIN Frequency Amplitude A f

11 Fourier Series Expansion of Signal Waveforms Recommended reading for an in-depth look at Fourier series expansions of signal waveforms: Clayton Paul, “Introduction to Electromagnetic Compatibility,” sections 3.1 and 3.2

12 Fourier Series Expansion of Square Wave Odd harmonics only

13 Fourier Series Expansion of Rectangular Pulse Train sin(x)/x (next slide) Even harmonics included NOTE: For 50% duty cycle (τ/T = 0.5), this equation reduces to that for the square wave on the previous slide.

14 Response and Envelope of sin(x)/x Envelope of |sin(x)/x|: 1 for x < 1 1/x for x > 1 Response of |sin(x)/x|: 0 for x = nπ 1/x for x = (n+1)π/2 Lines meet at x = 1

15 Envelope of Rectangular Pulse Train Spectrum f 0 dB/decade -20 dB/decade PULSE WIDTH f1f1 f2f2 f3f3 f4f4 f5f5 etc… DC offset Low frequency “plateau” Harmonic response

16 Fourier Series Expansion of Trapezoidal Waveform Additional sin(x)/x term due to rise/fall time τ τrτr τfτf T A Assume τ r = τ f : NOTE: τ r and τ f are generally measured between 10% and 90% of the minimum and maximum values of the waveform.

17 Envelope of Trapezoidal Waveform Spectrum f 0 dB/decade -20 dB/decade -40 dB/decade PULSE WIDTH RISE/FALL TIME DC offset Low frequency “plateau” Harmonic response (pulse width) Harmonic response (rise/fall time) f1f1 f2f2 f3f3 f4f4 f5f5 etc…

18 Envelope of Trapezoidal Waveform Spectrum f 0 dB/decade -20 dB/decade -40 dB/decade PULSE WIDTH RISE/FALL TIME Slower rise/fall times provide additional roll-off of higher order harmonics

19 Time Domain vs. Frequency Domain Test Setup WAVETEK 801 pulse generator TEKTRONIX DPO7054 oscilloscope (1 MΩ input) TEKTRONIX RSA5103A spectrum analyzer (50 Ω input)

20 Applied Waveform A = 1 V T = 200 µs(f 0 = 5 kHz) τ, τ r, & τ f varied as indicated on following slides τ τrτr τfτf T A

21 τ = 100 µs ( τ /T = 50%); τ r = τ f = 40 ns 2A(τ/T) = 1 V = 120 dBµV

22 τ = 100 µs ( τ /T = 50%); τ r = τ f = 360 ns 2A(τ/T) = 1 V = 120 dBµV

23 τ = 100 µs ( τ /T = 50%); τ r = τ f = 3.6 µs 2A(τ/T) = 1 V = 120 dBµV

24 τ = 100 µs ( τ /T = 50%); τ r = τ f = 10 µs 2A(τ/T) = 1 V = 120 dBµV

25 τ = 80 µs ( τ /T = 40%); τ r = τ f = 40 ns 2A(τ/T) = 0.8 V = 118 dBµV

26 τ = 80 µs ( τ /T = 40%); τ r = τ f = 360 ns 2A(τ/T) = 0.8 V = 118 dBµV

27 τ = 80 µs ( τ /T = 40%); τ r = τ f = 3.3 µs 2A(τ/T) = 0.8 V = 118 dBµV

28 τ = 80 µs ( τ /T = 40%); τ r = τ f = 10 µs 2A(τ/T) = 0.8 V = 118 dBµV

29 τ = 10 µs ( τ /T = 5%); τ r = τ f = 40 ns 2A(τ/T) = 0.1 V = 100 dBµV

30 τ = 10 µs ( τ /T = 5%); τ r = τ f = 350 ns 2A(τ/T) = 0.1 V = 100 dBµV

31 τ = 10 µs ( τ /T = 5%); τ r = τ f = 2 µs 2A(τ/T) = 0.1 V = 100 dBµV

32 τ = 2 µs ( τ /T = 1%); τ r = τ f = 20 ns 2A(τ/T) = 0.02 V = 86 dBµV

33 τ = 2 µs ( τ /T = 1%); τ r = τ f = 160 ns 2A(τ/T) = 0.02 V = 86 dBµV

34 τ = 2 µs ( τ /T = 1%); τ r = τ f = 400 ns 2A(τ/T) = 0.02 V = 86 dBµV

35 τ = 100 ns ( τ /T = 0.05%); τ r = τ f = 8 ns 2A(τ/T) = V = 60 dBµV

36 Observations (1 of 2) Measured spectra show good agreement with expected values “3-line” envelope provides simple, accurate, and powerful analytical tool for correlating signal spectra to trapezoidal waveforms Even harmonics Reduced, but not zero, amplitude for 50% duty cycle Varying amplitude for other than 50% duty cycle Must be considered as potentially significant contributors to spectrum Low frequency plateau scales with duty cycle Spectrum for low duty cycle waveforms gives artificial indication of low amplitude First “knee” frequency may be quite high, producing relatively flat spectrum for many harmonics (100s or 1000s in these examples) Low duty cycle waveforms should be observed in time domain (oscilloscope) as well as frequency domain (spectrum analyzer)

37 Observations (2 of 2) Signal spectra significantly more determined by rise/fall times than by fundamental frequency of waveform Uncontrolled rise/fall times can produce significant frequency content out to 1000 th harmonic and beyond Common cause of radiated emissions 5 MHz clock can easily produce harmonics out to 5 GHz and beyond Potential interference to S-band receiver (~2 GHz), GPS (~1.5 GHz), etc. Controlling rise/fall times can significantly limit high frequency content at source LIMIT THOSE RISE/FALL TIMES!!!