mean velocity. We considered that the highest
contribution to the velocity signal of the radar comes
from the pelvis since it has the largest surface area
(Yardibi et al. 2011). The mean velocity calculated
using the Doppler radar signals is then compared to
the mean velocity of the center of mass of the pelvis
obtained using Vicon. The main challenge in this
study was the irregularity of the signals obtained from
the Doppler device, which was resolved using the
Lomb-Scargle Periodogram (LS) (Scargle et al.
1982). A proper algorithm was proposed to extract
features from the radar signals that would help in
calculating the gait velocity.
2 EXPERIMENTAL SETUP
2.1 Doppler
The radar used in our study is a commercially
available Doppler sensor (X-Band Doppler Motion
Detector MDU 1130, Microwave Solutions LTD.,
Marlow United Kingdom) with a carrier frequency of
9.9 GHz. The device was placed on a 1m high table
and was put in a friendly, decorative box in order to
be more acceptable for future experiments in an
elderly environment. The radar was connected to an
application installed on a Tablet via Bluetooth, in
such a way that the recorded values of the velocity are
stored in a file and sent directly to the Tablet once
acquisition is over.
2.2 Vicon
The commercial 3-D motion analysis system, Vicon
system, used in this study consists of eight infrared
cameras and motion capture software installed in a
computer. During the acquisition, the cameras emit
infrared light that is reflected by the retro reflective
markers put on the moving subject. The reflected light
is then picked up by the cameras and eventually the
spatial position of each marker in an x, y, and z
coordinate system is obtained. In our study, we used
16 reflective markers that were put on the toes, heels,
wrists, fingers, shoulders and pelvis. Out of these
markers, we were able to extract the exact
instantaneous location of the center of mass of the
feet, hands, pelvis and shoulders. We considered that
the mean velocity of the center of mass of the pelvis
yields approximately the mean gait velocity. This
velocity was calculated simply by dividing the
distance travelled by the center of mass of the pelvis
by the time (over 10 ms intervals).
A synchronization system was built in order to
make sure that the radar and Vicon are acquiring the
same data for the exact walking sequence of each
subject. The system consisted of two infrared sensors
barriers that detect the start and the end of the walking
sequence. These two sensors are connected
simultaneously to the Tablet and the Vicon system.
2.3 Protocol and Data Processing
The aim of this study was to compare the velocities
obtained by the Doppler device to those obtained by
Vicon. Four persons, all of whom were members of
the laboratory, had given their informed consent to
participate in the experiments. Each subject
conducted five 5m walks towards the device,
resulting in 20 walking sequences. The signals
obtained from the radar contain the instantaneous
velocity of each movement detected in an irregular
time sampling. To filter the signals and remove high
and low frequencies, we used a Butterworth bandpass
filter between 5 and 100 Hz, applied to the signal in
the time domain. The frequencies contained in the
filtered signal were then obtained using the LS
periodogram (Eq. 2) which is known for detecting and
characterizing periodic signals in an unevenly
sampled data (
VanderPlas et al. 2018). A time delay
(Eq. 3) was added in order to overcome the problem
of the irregularity of the signals.
(
)
=
∑
∑
+
∑
∑
(2)
tan(2)=
∑
(
)
∑
(
)
(3)
The frequency with the highest peak corresponds to
the frequency of the steps made during the walk (Fig.
3), i.e. the number of steps performed in one second.
By inversing this frequency, we obtained the time
taken to complete each step for each of the subjects
who participated in the experiments. Furthermore, an
FFT was also conducted on the radar signals, with a
sampling frequency equal to the length of the signal.
The frequency peaks obtained from the FFT
corresponded to the number of steps performed by the
subject during the whole walking sequence. The
velocity was then calculated using this equation:
=
()
×
(4)
As for Vicon, an FFT was also conducted to obtain
the frequency of the velocity signals of each center of
gravity and then it was compared to the frequency
obtained from the LS periodogram applied to the
corresponding radar signals. We considered that the