Slide 38
In 3D: If the amplitude of the wavefunction of a particle at some point (x,y,z) is Y(x,y,z) then the probability of finding the particle between x and x+dx, y+dy and z+dz, ie, in a volume dV = dx dy dz is given by
Y(x,y,z) dV
dx
dy
dz
x
z
y
It follows therefore that
2
2
Y(x,y,z)
is a probability density.
In spherical coordinates
2
Y(r,q,f)
Slide 39
More important to know probability of finding electron at a given distance from nucleus!
dx
dy
dz
x
z
y
dV=dxdydz
Cartesian coordinates
not very useful to describe orbitals!
… in a shell of
dA = r2sinqdfdq
dA=dxdy
dV = r2sinqdfdqdr
Surface element
Volume element
Slide 40
Slide 41
For spherically symmetric orbitals:
the radial distribution function is defined as
2
P(r)= 4pr2 Y(r)
and P(r)dr is the probability of finding the electron in a shell of radius r and thickness dr
Slide 42
For spherically symmetrical orbitals
P(r)
Slide 43
Important
Born
interpretation
prob = Y2dt
Hence plot
P(r) = r2R(r)2
P(r)=4pr2Y2
(for spherical symmetry)
Pn(r) has
nodes
Slide 44
So what do we learn?
R(r)
R(r)2
P(r)
r
r
r
The 2p orbital is on average closer to the nucleus, but note the 2s orbital’s high probability of being
Slide 45
3d vs 4s
P(r)
Slide 46
The Ylm(,) angular part
of the solution form a set
of functions called the
n.b. These are generally
imaginary functions -we use
real linear combinations to
picture them.
Slide 47
Shapes arise from combination of radial R(r) and angular parts Ylm(,) of the wavefunction.
Usually represented as boundary surfaces which include of the probability density. The electron does not undergo planetary style circular orbits.