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3

Time Shifting and Scaling of Functions

We’ll begin with a square function, f(t), that has a an amplitude of 1, a start time of 2 seconds and an end time of 4 seconds.

square-wave

Next, a time shift is demonstrated. Here our function is changed from f(t) to f(t-2). Notice that subtracting 2 from t in the function results in a positive shift of the graph.

positive-shifted-square-wave

In the next two graphs t will be scaled. Scaling t is not quite as intuitive as we may have expected. When we multiply t by 2, corresponding points of the function now occur at 1/2 the time they previously had. When we divide t by 2, each corresponding time on the graph occurs at a t that is now multiplied by 2. Notice that each of these factors directly affects the duration of the signal.

time-shifted-square-wave
time-shifted-square-wave2

Scaling the amplitude has more intuitive results. If we multiply f(t) by 2, the amplitude of 1 is changed to 2. Multiplying f(t) by 1/2 results in an amplitude of 1/2.

taller-square-wave
truncated-square-wave

Finally, multiplying t by -1 mirrors our function over the y-axis. Each time now occurs at its negative.

mirrored-square-wave


Example:

Here we will attempt to convert f(t) into 2*f(.5t+3). The graph of f(t) is shown below.

triangle-wave

The easiest way to handle this type of problem without error is to manipulate the function one step at a time. First, I have converted f(t) into 2*f(t). Only the peaks are changed here (by a factor of 2).

triangle-wave2

Next, I convert 2*f(t) into 2*f( \frac{1}{2} t). Notice how the \frac{1}{2} actually expands our graph duration by a factor of 2 (from a 6 sec duration to a 12 sec duration).

shifted-triangle-wave

Finally, we move from 2*f( \frac{1}{2} t) to 2*f( \frac{1}{2} t + 3). As shown in the discussion above, this is a time shift. Time shifts can be a little confusing because adding results in a negative shift of our graph. Try to think of it as our signal occurring 3 seconds earlier than before, reading from left to right on the graph. The easiest way to do this part is shift each x-intercept by 3 seconds (to the left, of course).

shifted-triangle-wave2

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0

Calculating Electron and Hole Concentrations in a p-n Junction

TweetCalculating hole and electron concentrations Sometimes it can be complicated understanding and calculating hole and electron concentrations. My intent in this article is to briefly, but thoroughly describe what the variables used in these calculations mean and how to use them. To begin I will introduce our variables concentration of free electrons (donors) concentration of [...]

 
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Conversions Between Cartesian, Cylindrical and Spherical Coordinates

TweetThe 3 common methods of describing a point in a three dimensional coordinate system are Cartesian, Cylindrical and Spherical. The most simple is Cartesian but certain teachers find it necessary to use the others. There are a few simple conversions between them but first it is necessary to know their notation. Cartesian: Cylindrical: Spherical: In [...]

 
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Unit Vector Between Two Points

TweetSuppose you are interested in finding the unit vector between two points, and , which are described in cartesian coordinates as and , respectively. You would begin by finding the vector between these two points. The direction of this vector may be important so look for key words such as . Once we have established [...]

 
3

Laplace Transforms

TweetWhat is the Laplace Transform method? The Laplace Transform is a method that simplifies integral and differential equations into algebraic equations. This practice is commonly used to solve for a function out of a differential equation, which otherwise may have been unsolvable or very difficult. The following integrals can be used to transform between where [...]

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