the one-dimensional infinite square w ell defined over from x = 0 to x = a, so ‘width’ of well...
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The One-Dimensional Infinite Square Well• defined over from x = 0 to x = a, so ‘width’ of well is a• potential V(x) is even about center of well x = a/2• evenness/oddness of wavefunctions about x = a/2• theme: if potential is even, lowest energy wavefunction (ground state) will be even too.. then O, E…• this follows because the second derivative of a function has the same evenness/oddness as the function itself
• inside the well V = 0: free particle wavefunctions work• outside the well V = ∞: the wavefunction must be zero• the monstrous (INFINITE) jump in V at the well edges [x = 0, x = a] implies that the wavefunction’s slope is not continuous at those places• the wavefunction must always be continuous, no matter what V(x)!!
axx
axxVd
or 0
00)( is potentialSW 1
Wavefunction inside the 1d ∞ Square Well
• rightward-moving and leftward-moving free wavicles have the same energy E, so a linear combination of them also solves the TISE with that same E• choose a linear combination that satisfies the boundary conditions (0) = (a) = 0
mE
kikxAikxAx2
: expexp)( RL
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expexp 00)(
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n
Even or Odd about a/2?
• these are even solutions about well middle (includes ground state)• they are labeled, however, by odd integers n = 1,3,5…
• These are odd solutions about well middle (first excited state…) • (labeled by even integers)
• lower sign (–)• let AL = A/2i
• upper sign (+)• Let AL = A/2
• Both:28
22
22
22
2
22
2
so ma
nh
ma
n
mnk
na
nn Ek
6,4,21)cos(
)cos( expexp2
)(
nnakka
kxAikxikxA
x
n
5,3,11)sin(
)sin( expexp2
)(
nnakka
kxAikxikxi
Ax
n
Probability densities for 1d∞SW
E3 = 9 E1
E2 = 4 E1
• the wavefunctions are standing waves, so regardable as the sum of two oppositely-traveling wavicles with equal amplitudes• wavefunctions are sinusoidal, so probability densities are sine-squared functions with integral number of cycles: area underneath is half the maximum times the width. NORMALIZE:
• typical value for a = 1 nm: E1 ≈ (50 x 10-68)/(10)(10-30)(10-18) ≈ 5 x 10-20 J ≈ 1/3 eV [since 1 eV = 1.602 x 10-19 J]
Hydrogen atom is about 20 times smaller (.53 Å) E = – 13.6 eV
a
aAa
AdxAdxxxa
a
xn 22
||)(sin||)()(1 2
0
22*
E1 = h2/8ma2
Things to note regarding this example• walls are ‘infinitely high’ and correspond to impenetrable• infinite jump in V causes a ‘kink’ in – unusual!• energy spectrum climbing like n2 is the MOST rapid climb it can possibly be for ANY well since well ‘sides’ are ∞-ly steep!• crucial helpful fact: eigenfunctions are ‘orthonormal’:
a
xn
a
xm
a
xn
a
xm
a
xnm sinsincoscos
)(cos since
mn
a
a
a
a
a
nm
nma
adx
a
xm
a
nma
xnm
nma
xnm
nm
dxa
xnm
a
xnm
a
dxa
xn
a
xm
adxxx
for 12
2sin
2
for 0)(
sin)(
1)(sin
)(
1
)(cos
)(cos
1
sinsin2
)()(
0
2
0
0
*
Expectation values and uncertainties I• Expectation value for position should be middle of the well
• this tells us very little about ‘where’ the particle is• <x2> requires two integrations by parts; result is
• this is evidently a measure of the typical ‘distance’from the center, and grows for larger n; in the limit, <x2> a2/3
well theof middle 28
1
8
2cos
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2
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2cos
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2sin
22
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2cos1sinuse
so let ;sin
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0
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2
nadx
a
xnx
ax
a
Expectation values and uncertainties II• uncertainty in position is x = (<x2> – <x>2)1/2
• turning to the momentum expectations and uncertainty
• ground state has lowest product, which still exceeds minimum uncertainty, and the product grows with n• begs the question of how to achieve minimum uncertainty
22
2
222 2
3
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242
1
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n
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idea trigaverage'' theused we where2
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a
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a
n
dxa
xn
a
n
ap
xp
dxa
xn
a
xn
a
n
a
ip
xip
a
a
Using these orthonormal wavefunctions as building blocks: Fourier Series
• wavefunctions {n}, are orthonormal, as we have seen• they are complete: any odd [f(–x) = – f(x); f(0) = 0] periodic [f(x + 2a) = f(x), so period is 2a] (this is not the most general situation – stay tuned) function can be expressed as a linear combination
11
sin2
)()(n
nn
nn a
xnc
axcxf
• Fourier’s Trick: to get the {cm}, multiply expansion of f(x) by m*(x) and integrate term by term from 0 to a:
)()(2
2
sinsin2
sin2
sin2
0
*
11
1 010
a
mmmn
nmnn
nmn
nn
a
nn
a
dxxfxcccca
a
dxa
xnc
a
xm
adx
a
xnc
aa
xm
a
More general remarks about the Fourier series
• for any [odd or even or neither] periodic [f(x + 2a) = f(x), so period is 2a] function can be expressed as a linear combination• conventionally, the limits are now taken to be from –a to a so the new normalization is 1/√a• both cosines and sines must be included
• Fourier’s Trick is now very similar—the cosines and the constant are both even contributions, so
a
d
a
xnd
a
xnc
a
dxdxcxf
nnn
nnnnn
2cossin
1
2)()()( 0
11
0
0,1,2,3... for )(cos1
1,2,3... for )(sin1
mdxxfa
xm
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xm
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a
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