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Figure
2 shows an idealized, one degree-of-freedom isolator based
on a simple harmonic oscillator. It consists of three components:
The isolated mass (M) represents the payload being isolated and
is shown here as a single block mass with no internal resonances.
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A spring (k) supports
the payload and produces a force on the payload given by: |
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where Xe and
Xp represent the (dynamic) position of the earth and
payload, respectively. The third component is the damper (b), which
is represented schematically as a dashpot. It absorbs any kinetic
energy the payload (M) may have by turning it into heat, eventually
bringing the system to rest. It does this by producing a force on
the payload proportional and opposite to its velocity relative to
the earth: |
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The presence
of Xe in both of these equations shows that vibration
of the earth is transmitted as a force to the payload by both the
spring (k) and the damper (b). Rather than use the parameters
(M), (k), and (b) to describe a system, it is common to define a
new set of parameters which relate more easily to the observables
of the mass-spring system. The first is the natural
resonant frequency 0: |
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It describes the frequency
of free oscillation for the system in the absence of any damping
(b = 0) in radians/second. The frequency in cycles per second, or
Hertz (Hz), is this angular frequency divided by 2 .
One of two common parameters are used to describe the damping in
a system: The Quality factor Q
or the damping ratio : |
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It can be shown that
the transmissibility for this idealized system is: |
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Figure
3 plots the transmissibility of the system versus the frequency
ratio / 0 for
several values of the quality factor Q. The values of Q plotted
range from 0.5 to 100. Q = 0.5 is a special case called critical
damping and is the level of damping at which the system will
not overshoot the equilibrium position when displaced and released.
The damping ratio is
just the fraction of the system’s damping to critical damping.
We use Q rather than because
T Q
at = 0,
for Qs above about 2. There are several features which characterize
the transmissibility shown in Figure
3: |
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In the region  << 0,
the transmissibility for the system is  1.
This simply means that the payload tracks the motion of the earth
and no isolation is provided.
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In the region where 0,
the transmissibility is greater than one, and the spring/damper
isolator amplify the ground motion by a factor roughly equal to Q.
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As  becomes
greater than 0,
the transmissibility becomes proportional to
( 0 /  ) 2.
This is the region where the isolator is providing a benefit.
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In the region  >> 0,
the best isolation is provided by the system with the smallest
level of damping. Conversely, the level of isolation is compromised
as the damping increases. Thus, there is always a tradeoff between
providing isolation in the region  >> 0 versus 0.
The amplitude of motion transmitted
to the payload by forces directly applied to it has a slightly
different form than that expressed in Equation
7. This transfer function has units of displacement per unit
force, so it should not be confused with a transmissibility: |
 [8] |
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Figure
4a plots this function versus frequency. Unlike Figure
3, decreasing the Q reduces the response of the payload
at all frequencies, including the region >> 0. |
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TMC’s MaxDamp® isolators
take advantage of this for applications where the main disturbances
are generated on the isolated payload. Figure
4b shows the time-domain response of the payload corresponding
to the curves shown in Figure
4a. This figure also illustrates the decay of the system once
it is disturbed. The envelope for the decay is exp (- 0t /
2Q). |
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There are some significant
differences between real systems and the simple model shown in Figure
2, the most significant being that real systems have six degrees-of-freedom
(DOF) of motion. These DOF are not independent but strongly couple
in most systems. For example, “horizontal transfer functions” usually
show two resonant peaks because horizontal motions of a payload
drive tilt motions and vice-versa. A detailed description of this
type of coupling is beyond the scope of this catalog.
Back to Technical
Background Index |
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Figure
5 shows a simplified pneumatic isolator. The isolator works
by the pressure in the volume (V) acting on the area of
a piston (A) to support the load against the force of gravity. |

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A reinforced rolling
rubber diaphragm forms a seal between the air tank and the piston.
The pressure in the isolator is controlled by a height control valve
which senses the height of the payload and inflates the isolator
until the payload is “floating.” There are many advantages
to pneumatic isolators. It can be shown that the resonant frequency
of the payload on such a mount is approximately: |
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where g is acceleration
of gravity (386 in/s2 or 9.8 m/s2)
and n is the gas constant for air and equal to 1.4. Unlike steel
coil springs, this resonant frequency is nearly independent of the
mass of the payload, and the height control valve always brings the
payload back to the same operating height.* Gas
springs are also extremely lightweight, eliminating any internal
spring resonances which can degrade the isolator’s performance. |
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The load capacity of
an isolator is set by the area of the piston and the maximum pressure
the diaphragm can tolerate and is simply the product of these two
numbers. It is common to rate the capacity at 80 psi of pressure.
This allows a 4 in. piston to support a 1,000-lb load (for example).
Though the simple isolator in Figure
5 will work, it has very little horizontal isolation and has
very little damping.
Back
to The Technical Background Index |
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*Equation 9 assumes
the isolator’s pressure is high compared with atmospheric
pressure. Lightly loaded isolators will exhibit a slightly higher
resonant frequency.
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