Xivanki Share !!: Movement patterns

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This blog entry does not have associated example program, the samples of this post were taken using the sensor monitoring application presented here. This time I will give a taste what can be achieved by using the acceleration sensor for identifying movement patterns. Previously we have seen that the acceleration sensor is pretty handy at measuring the orientation of the device relative to the Earth's gravity. At that discussion we were faced with the problem what if the device is subject to acceleration other than the Earth's gravity. In that measurement, it caused noise. For example if you move the device swiftly, you can force change between landscape and portrait mode even if the device's relative position to the Earth's surface is constant. That's because the acceleration of the device's movement is added to the Earth's gravity acceleration, distorting the acceleration vector.

In this post, we will be less concerned about the device's orientation. We will focus on these added accelerations. Everyday movements have characteristic patterns and by analysing the samples produced by the acceleration sensor, cool context information can be extracted from the acceleration data.

The acceleration sensor measures the acceleration along three axes. This 3D vector is handy when one wants to measure orientation of e.g. the gravity acceleration vector. When identifying movements, it is more useful to work with the absolute value of the acceleration because the device may change its orientation during the movement. Therefore we calculate

ampl=sqrt( x^2 + y^2 + z^2 )

where x,y,z are elements of the measured acceleration vector along the three axes. Our diagrams will show this ampl value.

Let's start with something simple.



This is actually me walking at Waterloo station. The diagram shows the beginning of the walking. It starts with stationary position then I start to walk. In order to understand the pattern, we must remember that acceleration is change of the velocity vector. This means that if we move quickly but our velocity does not change, we have 0 acceleration. On the other hand, if we move with constant speed but our direction changes, that's quite a significant change in the velocity vector. That is the source of the gravity acceleration, the Earth's surface (and we along with it) rotates with constant speed but as the speed is tangent to the Earth's surface, its direction constantly changes as the Earth rotates.

The same goes for walking. Whenever the foot hits the ground, its velocity vector changes (moved down, starts to move up). Similarly, when the foot reaches the highest point, it moved up and then it starts to move down. The maximums and the minimums of the acceleration amplitude are at these points. As these accelerations are added to the Earth's acceleration (9.81 m/s^2), you will see an offset of about 10. The sine wave-like oscillation of the acceleration vector's absolute value is unmistakable. The signal is not exactly sine wave but the upper harmonics attenuate quickly. You can see that my walking caused about 1.2g fluctuation (-0.6 g to 0.6 g).

Running is very similar except that the maximum acceleration is much higher - about 2 g peak-to peak.



And now, everybody's favourite, the shaking. Shaking is very easy to identify. First, the peak acceleration is very high (about 3 g in our case). Also, the peaks are spike-like (very high upper harmonic content).



In the following, I will present some algorithms that produce handy values when identifying these movements.