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tdehaeze committed 2026-10-14 16:07:55 +02:00
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@@ -345,21 +345,21 @@ If we left multiply the equation by \\(\Phi^T\\) and we use the orthogonalily re
\\[ diag(\mu\_i) \ddot{z} + \Phi^T C \Phi + diag(\mu\_i \omega\_i^2) z = \Phi^T f \\]
If \\(\Phi^T C \Phi\\) is diagonal, the **damping is said classical or normal**. In this case:
\\[ \Phi^T C \Phi = diag(2 \xi\_i \mu\_i \omega\_i) \\]
\\[ \Phi^T C \Phi = diag(2 \zeta\_i \mu\_i \omega\_i) \\]
One can verify that the Rayleigh damping \eqref{eq:rayleigh\_damping} complies with this condition with modal damping ratios \\(\xi\_i = \frac{1}{2} ( \frac{\alpha}{\omega\_i} + \beta\omega\_i )\\).
One can verify that the Rayleigh damping \eqref{eq:rayleigh\_damping} complies with this condition with modal damping ratios \\(\zeta\_i = \frac{1}{2} ( \frac{\alpha}{\omega\_i} + \beta\omega\_i )\\).
And we obtain decoupled modal equations \eqref{eq:modal\_eom}.
<div class="cbox">
\begin{equation}\label{eq:modal\_eom}
\ddot{z} + 2 \xi \Omega \dot{z} + \Omega^2 z = z^{-1} \Phi^T f
\ddot{z} + 2 \zeta \Omega \dot{z} + \Omega^2 z = z^{-1} \Phi^T f
\end{equation}
with:
- \\(\xi = diag(\xi\_i)\\)
- \\(\zeta = diag(\zeta\_i)\\)
- \\(\Omega = diag(\omega\_i)\\)
- \\(\mu = diag(\mu\_i)\\)
@@ -373,12 +373,12 @@ Typical values of the modal damping ratio are summarized on [Table 2](#table--ta
Typical Damping ratio
</div>
| **Damping Ratio** | **Application** |
|--------------------------------|-------------------------|
| \\(\xi \simeq 0.001 - 0.005\\) | Space structures |
| \\(\xi \simeq 0.01 - 0.02\\) | Mechanical engineering |
| \\(\xi \simeq 0.05\\) | Civil engineering |
| \\(\xi \simeq 0.2\\) | When ground is involved |
| **Damping Ratio** | **Application** |
|----------------------------------|-------------------------|
| \\(\zeta \simeq 0.001 - 0.005\\) | Space structures |
| \\(\zeta \simeq 0.01 - 0.02\\) | Mechanical engineering |
| \\(\zeta \simeq 0.05\\) | Civil engineering |
| \\(\zeta \simeq 0.2\\) | When ground is involved |
The assumption of classical damping is often justified for light damping, but it is questionable when the damping is large.
@@ -407,7 +407,7 @@ With:
- \\(D\_i(\omega)\\) is the dynamic amplification factor of mode \\(i\\) given by
\begin{equation}\label{eq:dynamic\_amplification}
D\_i(\omega) = \frac{1}{1 - \omega^2/\omega\_i^2 + 2 j \xi\_i \omega/\omega\_i}
D\_i(\omega) = \frac{1}{1 - \omega^2/\omega\_i^2 + 2 j \zeta\_i \omega/\omega\_i}
\end{equation}
<a id="figure--fig:neglected-modes"></a>
@@ -489,7 +489,7 @@ By looking at [Figure 7](#figure--fig:collocated-control-frf), we see that negle
The open-loop transfer function of a lighly damped structure with a collocated actuator/sensor pair can be written:
\begin{equation}\label{eq:frf\_lighly\_damped\_collocated}
G(s) = G\_0 \frac{\Pi\_i(s^2/z\_i^2 + 2 \xi\_i s/z\_i + 1)}{\Pi\_j(s^2/\omega\_j^2 + 2 \xi\_j s /\omega\_j + 1)}
G(s) = G\_0 \frac{\Pi\_i(s^2/z\_i^2 + 2 \zeta\_i s/z\_i + 1)}{\Pi\_j(s^2/\omega\_j^2 + 2 \zeta\_j s /\omega\_j + 1)}
\end{equation}
The corresponding Bode plot is represented in [Figure 9](#figure--fig:alternating-p-z). Every imaginary pole at \\(\pm j\omega\_i\\) introduces a \\(\SI{180}{\degree}\\) phase lag and every imaginary zero at \\(\pm jz\_i\\) introduces a phase lead of \\(\SI{180}{\degree}\\).
@@ -576,14 +576,14 @@ The transfer function between the total force and the current \\(i\\) applied to
<div class="cbox">
\begin{equation}\label{eq:proof\_mass\_eq}
\frac{F}{i} = \frac{-s^2 T}{s^2 + 2\xi\_p \omega\_p s + \omega\_p^2}
\frac{F}{i} = \frac{-s^2 T}{s^2 + 2\zeta\_p \omega\_p s + \omega\_p^2}
\end{equation}
with:
- \\(T\\) is the transducer constant
- \\(\omega\_p = \frac{k}{m}\\) is the natural frequency of the spring-mass system
- \\(\xi\_p\\) is the damping ratio
- \\(\zeta\_p\\) is the damping ratio
</div>
@@ -609,7 +609,7 @@ If \\(x\_0\\) is the displacement of the support and if the voice coil is open (
By using the two equations, we obtain:
\begin{equation}\label{eq:geophone}
\frac{e}{\dot{x\_0}} = \frac{-s^2 T}{s^2 + 2\xi\_p\omega\_p s + \omega\_p^2}
\frac{e}{\dot{x\_0}} = \frac{-s^2 T}{s^2 + 2\zeta\_p\omega\_p s + \omega\_p^2}
\end{equation}
Above the corner frequency, the gain of the geophone is equal to the transducer constant \\(T\\).