Now that we are right in the heart of quantum mechanics, it is time we reviewed all that has happened so far. The start of the 20th century saw a surge in the number of experiments conducted by physicists, all in the same field of trying to figure out a way to model the seemingly unpredictable behaviour of electrons and similar particles.
In the double-slit experiment, thought experiments were performed about directing a single electron at the set up. By physical measurement, it is a simple task (atleast in theory) to ascertain which slit the electron went through. But that gives us no real information, if you think of it. Well we know for sure where the electron is, now, but that tells us nothing about where it tends to go, in general. This was quite a revelation at that time, considering the fact that a large number of scientists were breaking their heads over the particle (or wave-like) nature of the electron.
One thing was clear: the electron was and is a particle. There are no two ways about it.
But this particle behaves as if its properties (speed, energy, momentum and the like) were determined by a wave-like probability distribution.

Wait, what?
A wave-like probability? Does that mean that interference can take place? - Yes! Why not?
We must note that although these properties seem very counter-intuitive, they are the results of experimental study and we need to craft a model to fit the experiments best.
Since interference can take place, it is no surprise that the likelihood of finding an electron at one place is influenced by the probability distribution of another electron in the same system. So we need a parameter that can depict the probability distribution of a particle, and also give us information about its energy.
Welcome the wavefunction - ψ.
Αs of now, it will suffice to say that psi is such that the square of its modulus gives us the probability of finding the electron somewhere. A wavefunction needs to obey a few properties for it to be of use to us. We will be looking at these properties later.
In the double-slit experiment, thought experiments were performed about directing a single electron at the set up. By physical measurement, it is a simple task (atleast in theory) to ascertain which slit the electron went through. But that gives us no real information, if you think of it. Well we know for sure where the electron is, now, but that tells us nothing about where it tends to go, in general. This was quite a revelation at that time, considering the fact that a large number of scientists were breaking their heads over the particle (or wave-like) nature of the electron.
One thing was clear: the electron was and is a particle. There are no two ways about it.
But this particle behaves as if its properties (speed, energy, momentum and the like) were determined by a wave-like probability distribution.
Wait, what?
A wave-like probability? Does that mean that interference can take place? - Yes! Why not?
We must note that although these properties seem very counter-intuitive, they are the results of experimental study and we need to craft a model to fit the experiments best.
Since interference can take place, it is no surprise that the likelihood of finding an electron at one place is influenced by the probability distribution of another electron in the same system. So we need a parameter that can depict the probability distribution of a particle, and also give us information about its energy.
Welcome the wavefunction - ψ.
Αs of now, it will suffice to say that psi is such that the square of its modulus gives us the probability of finding the electron somewhere. A wavefunction needs to obey a few properties for it to be of use to us. We will be looking at these properties later.




