Fourier transforms
We will use the following convention for the Fourier transforms:ρ(q)=F[ρ(r)](q)≜∫Vρ(r)exp(−iqr)drρ(r)=F−1[˜ρ(q)](r)≜1(2π)3∫R3˜ρ(q)exp(iqr)dq where we integrate in real space over the (as yet unspecified) volume of interest V and in reciprocal space over the entire R3.
Wiener-Khinchine theorem
The autocorrelation of the real-space density function is Γρρ=∫Vρ(r′)ρ(r′+r)dr′, which can be developed (using the second line of (1)) into:Γρρ(r)=1(2π)6∫Vdr′ρ(r′)∫R3dq˜ρ(q)exp(iqr′)∫R3dq′˜ρ(q′)exp[iq′(r′+r)]=1(2π)6∫R3dq∫R3dq′˜ρ(q)˜ρ(q′)exp(iq′r)∫Vdr′exp[i(q+q′)r]⏟(2π)3δ(q+q′)=1(2π)3∫R3dq′exp(iq′r)˜ρ(q′)∫R3dq˜ρ(q)δ(q+q′)⏟˜ρ(−q′) where we assumed that everything converges, and thus we can interchange the integration order at will. Dropping the prime and noting that ˜ρ(−q)=¯˜ρ(q) (Friedel's law) we finally prove the Wiener-Khinchine theorem: the autocorrelation function of the scattering length density is the inverse Fourier transform of its spectral density: Γρρ(r)=1(2π)3∫R3dqexp(iqr)|˜ρ(q)|2=F−1[|˜ρ(q)|2]
The Patterson function
As discussed during the lecture, the scattered intensity is precisely the spectral density of ρ(r): I(q)=|˜ρ(q)|2. Unlike ρ(r) itself, its autocorrelation Γρρ(r) is directly accessible via Fourier transform from the experimental data, provided their quality and q-range are sufficient. Since it is frequently used in crystallography, it has a specific name: the Patterson function, denoted by P(r).
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