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Introduction
to the
Microsurf, Photomap and Zoomsurf Profilers
PhotoMap
is
based on the Peak Fringe Scanning Microscopy principle. It measures,
without contact and with high accuracy, the micro-relief of a
surface and quantifies its roughness-undulation by means of a
statistical analysis.
The
vertical nanometric displacement is controlled by computer and
the interferometric data is automatically computed to render 3D
imaging of the topography. With this technique a complete 3x2.5
mm can be taken in less than 30seconde with very high resolution.
The instrument can also be used to measure the thickness of translucent
layers or films.
Detailed
principle of operation :
A
Michelson interferometer splits the beam emitted by the source
(So) into two " half-beams ". One half-beam is reflected on the
reference mirror (M), the other on the sample. The beam splitter
(Sp) transmits both reflected beams to the camera target (C) through
the lens (L). The intensity I(d) measured on the camera target,
varies as a function of the path difference (d) between 1 and
2. The I(d) signal (fringes pattern (F)) is maximum for d = 0.
Non-contact
Accuracy
The
method could be summarized by considering that the interferences
generates a horizontal light plane (P). This light plane (P) is
used as a probe. A vertical displacement (Z) of the measured surface
makes the latter cross up the probe plane. The successive intersections
between the probe plane and the sample are the relief level curves
(isophots). The acquisition system keeps the coordinates (x,y,z)
of all the points making the isophots and interpolates from one
level curve to another so as to get a better measurement resolution.
The displacement of the measured surface along (Z) is servo-controlled
by capacitive sensors. The principle of the capacitance-based
technology, well known for its high accuracies, is the following
: the measured capacity is conversely proportional to the desired
distance. The positioning is better than 1 nm.
The CCD target (782 x 582 pixels) carries out simultaneously the
measurement of all the points on the measured surface. There is
no need to mechanical scanning along the x and y axes. This
allows for small areas to be scanned with very high resolutions
very quickly.

Michelson
interferometer
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No
lateral scanning in x and y
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Probe
plane
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Isophote
(n)
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Isophote
(n+ 1)
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Isophote
(n + 2)
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Carte
des
Isophotes
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Relief
measurement by means of isophots (level curves)
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Laboratory
Services Available
Microsurf
3D
Zoomsurf
3D
Photomap
3D
Other
complementary profilometry system
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