International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B7, 2012
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia
4.2 Calibrated amplitude reading
Beside geometrical information, the VZ-line additionally
delivers a calibrated amplitude information for each target
echo, which can be used to improve the object classification.
The amplitude reading is defined as the ratio of the actual
detected optical amplitude of the echo pulse versus detection
threshold (eq. 1). The ratio is stated in decibels (dB).
D ( 1 )
thr
A, =10-log
where
Agp = calibrated amplitude [dB]
Pecho 7 echo signal power [W]
Pa, — power detection limit [W]
4.3 Calibrated reflectance reading
With the VZ-series of laser scanners, Riegl has introduced
some measure of the laser radar cross-section by providing a
reflectivity value for each target echo. The reflectivity value
gives the ratio of the actual optical amplitude versus the
optical amplitude of a diffuse white target located at the same
range (it is furtherly assumed that the white target is larger
than the laser footprint, 100% reflecting, flat, and its surface
is orthogonal to the laser beam). The value is again given in
dB (eq. 2).
Pre (R7) = Ay (R, Y Ag white (R,) Q)
where
Ry = target Trange [m]
Pra (Rz) = calibrated reflectance of target T at range Ry
Agp 1 = calibrated amplitude of T at range Ry [dB]
Agp white - amplitude of white target T at range Rr [dB]
White diffuse targets would have assigned about 0 dB, while
black paper with a reflectance of 10% would give about -10
dB. Reflectivity values above 0 dB indicate that the target
returns an optical echo amplitude larger than those of a
diffuse white target, ie, the target is (partially) retro-
reflecting. By assigning a brightness value to each point of a
point cloud according to the reflectivity, objects with the
same reflectivity will have the same brightness regardless of
the distance to the scanner. Note that this applies only to
single and first targets, not for the succeedings ones located
along the laser beam axis. Indeed, except for single and first
targets, the response of each subsequent target hit by the laser
beam is a combination of the respective laser radar cross
section and of the attenuation of the laser pulse due to the
preceding targets. Since this target-induced attenuation
cannot be retrieved from the amplitude of the backscattered
pulse, actually the calibrated reflectance readings are
representative of the backscattering properties of just the
single or first targets acquired by a multi-echo digitizing
system. An example of calibrated amplitude and calibrated
reflectance is shown in figures 3(a) and 3(b), while a small
portion of a VZ-400 scan coloured according to the recorded
multiple echoes is displayed in figure 4.
514
(b)
Figure 3: Front view of the test area rendered according to the
calibrated amplitude (a) and the calibrated reflectance (b).
Figure 4: Side view of a small portion of the landslide
surveyed with the Riegl VZ-400 laser scanner. Green color
denotes single targets, yellow first targets, light blue
intermediate targets and blue last targets.
5. VEGETATION FILTERING
The data collected in the same subarea of the Brustolé
landslide with the Riegl LMS-Z620 and the VZ-400 laser
scanners were properly filtered in order to remove as much as
possible the dense vegetation. The resulting DTMs were then
compared to assess the potential of a multi-target TLS system
with online waveform processing capability, such as the
Riegl VZ-400, for better discriminate between vegetation and
terrain. A slight different processing workflow was applied to
the collected datasets. Firstly, the VZ-400 scan, covering the
area of interest, was pre-filtered by exploiting the multi-target
capability and the "calibrated relative reflectance" readings
provided by this TLS. Out of the four types of echoes
recorded by the instrument, only single, first and last targets
were extracted from the original point cloud. Intermediate
("others") targets were discarded as they were most likely
originated by non-ground points. Then a subsequent filtering