Define a function with a field output: the viscous free fall example¶
In this example, we define a function which has a vector input and a field output. This is why we use the PythonPointToFieldFunction
class to create the associated function and propagate the uncertainties through it.
Introduction¶
We consider an object inside a vertical cylinder which contains a viscous fluid. The fluid generates a drag force which limits the speed of the solid and we assume that the force depends linearily on the object speed:
for any where:
is the speed ,
is the time ,
is the maximum time ,
is the gravitational acceleration ,
is the mass ,
is the linear drag coefficient .
The previous differential equation has the exact solution:
for any
where:
is the altitude above the surface ,
is the initial altitude ,
is the initial speed (upward) ,
is the limit speed :
is time caracteristic :
The stationnary speed limit at infinite time is equal to :
When there is no drag, i.e. when , the trajectory depends quadratically on :
for any .
Furthermore when the solid touches the ground, we ensure that the altitude remains nonnegative i.e. the final altitude is:
for any .
References¶
Steven C. Chapra. Applied numerical methods with Matlab for engineers and scientists, Third edition. 2012. Chapter 7, “Optimization”, p.182.
Define the model¶
[1]:
from __future__ import print_function
import openturns as ot
import numpy as np
We first define the time grid associated with the model.
[2]:
tmin=0.0 # Minimum time
tmax=12. # Maximum time
gridsize=100 # Number of time steps
mesh = ot.IntervalMesher([gridsize-1]).build(ot.Interval(tmin, tmax))
The getVertices
method returns the time values in this mesh.
[3]:
vertices = mesh.getVertices()
vertices[0:5]
[3]:
v0 | |
---|---|
0 | 0.0 |
1 | 0.12121212121212122 |
2 | 0.24242424242424243 |
3 | 0.36363636363636365 |
4 | 0.48484848484848486 |
Creation of the input distribution.
[4]:
distZ0 = ot.Uniform(100.0, 150.0)
distV0 = ot.Normal(55.0, 10.0)
distM = ot.Normal(80.0, 8.0)
distC = ot.Uniform(0.0, 30.0)
distribution = ot.ComposedDistribution([distZ0, distV0, distM, distC])
[5]:
dimension = distribution.getDimension()
dimension
[5]:
4
Then we define the Python function which computes the altitude at each time value. In order to compute all altitudes with a vectorized evaluation, we first convert the vertices into a numpy
array
and use the numpy
function exp
and maximum
: this increases the evaluation performance of the script.
[6]:
def AltiFunc(X):
g = 9.81
z0 = X[0]
v0 = X[1]
m = X[2]
c = X[3]
tau = m / c
vinf = - m * g / c
t = np.array(vertices)
z = z0 + vinf * t + tau * (v0 - vinf) * (1 - np.exp( - t / tau))
z = np.maximum(z,0.)
return [[zeta[0]] for zeta in z]
In order to create a Function
from this Python function, we use the PythonPointToFieldFunction
class. Since the altitude is the only output field, the third argument outputDimension
is equal to 1
. If we had computed the speed as an extra output field, we would have set 2
instead.
[7]:
outputDimension = 1
alti = ot.PythonPointToFieldFunction(dimension, mesh, outputDimension, AltiFunc)
Sample trajectories¶
In order to sample trajectories, we use the getSample
method of the input distribution and apply the field function.
[8]:
size = 10
inputSample = distribution.getSample(size)
outputSample = alti(inputSample)
[9]:
ot.ResourceMap.SetAsUnsignedInteger('Drawable-DefaultPalettePhase', size)
Draw some curves.
[10]:
graph = outputSample.drawMarginal(0)
graph.setTitle('Viscous free fall: %d trajectories' % (size))
graph.setXTitle(r'$t$')
graph.setYTitle(r'$z$')
graph
[10]:
We see that the object first moves up and then falls down. Not all objects, however, achieve the same maximum altitude. We see that some trajectories reach a higher maximum altitude than others. Moreover, at the final time , one trajectory hits the ground: for this trajectory.