Sinusoidal Waveforms, RMS Values & Phase

A sinusoid is determined by amplitude, angular frequency, and phase. RMS converts its heating effect to an equivalent DC value, while phase differences determine timing and power exchange.

Sinusoidal steady state is the regime reached by a stable linear circuit after transients have decayed while the excitation remains sinusoidal. Every voltage and current then shares the source angular frequency; only magnitude and phase differ. That closure is why differential equations become complex algebra.

Parameterizing the waveform #

Write

x(t)=Xmcos⁡(ωt+ϕ),x(t)=X_m\cos(\omega t+\phi),

where XmX_m is peak amplitude, ω=2πf\omega=2\pi f is angular frequency, and ϕ\phi is phase relative to a declared reference. The period is T=1/fT=1/f.

Phase has meaning only as a difference. If

v(t)=Vmcos⁡(ωt+ϕv),i(t)=Imcos⁡(ωt+ϕi),v(t)=V_m\cos(\omega t+\phi_v),\qquad i(t)=I_m\cos(\omega t+\phi_i),

then the physically relevant angle is ϕ=ϕv−ϕi\phi=\phi_v-\phi_i. Changing the time origin shifts both phases equally and leaves ϕ\phi unchanged.

RMS is a power-equivalent value #

For any periodic waveform,

Xrms=1T∫0Tx2(t) dt.X_{rms}=\sqrt{\frac{1}{T}\int_0^T x^2(t)\,dt}.

For a sinusoid, Xrms=Xm/2X_{rms}=X_m/\sqrt2. A resistor driven by a sinusoidal voltage dissipates the same average power as it would under DC voltage VrmsV_{rms}:

P=Vrms2R.P=\frac{V_{rms}^2}{R}.

Peak, peak-to-peak, average, and RMS are different quantities. A zero-mean sinusoid has average value zero but nonzero RMS.

Phase as time displacement #

A phase difference corresponds to time shift

Δt=Δϕω.\Delta t=\frac{\Delta\phi}{\omega}.

The same time shift produces a different phase angle at a different frequency. This is why a constant propagation delay is not a constant phase shift over bandwidth.

The phasor method applies one frequency at a time. A nonsinusoidal periodic waveform must be decomposed into harmonics, analyzed frequency by frequency in a linear circuit, and recombined.

Two sinusoids with a phase difference Voltage leads current by forty-five degrees; dashed lines mark peak and RMS levels. ωtv(t)i(t)peakRMS = peak/√2phase is horizontal displacement at a fixed frequency
RMS is an energy-equivalent magnitude; phase records relative position within a cycle

RMS must be computed over a stated interval. For a periodic waveform, use an integer number of periods; otherwise the value can depend on the window position even when the underlying signal is unchanged.

Sources

  1. articleADSP-CM403 HAE—Harmonic Analysis in Solar Applications

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