where is defined as . can be obtained from by inverse FT:
and are inverse variables, e.g. frequency and time.
Obtaining directly requires that is well known from to , vice versa. In real experimental data this is rarely the case due to noise and limited measured range, say is known from to . Performing a FT on in the limited range may lead to systematic errors and overfitting.
An indirect Fourier transform (IFT) is a solution to this problem.
Indirect Fourier transformation in small-angle scattering
In small-angle scattering on single molecules, an intensity is measured and is a function of the magnitude of the scattering vector , where is the scattered angle, and is the wavelength of the incoming and scattered beam (elastic scattering). has units 1/length. is related to the so-called pair distance distribution via Fourier Transformation. is a (scattering weighted) histogram of distances between pairs of atoms in the molecule. In one dimensions ( and are scalars), and are related by:
where is the angle between and , and is the number density of molecules in the measured sample. The sample is orientational averaged (denoted by ), and the Debye equation [1] can thus be exploited to simplify the relations by
In 1977 Glatter proposed an IFT method to obtain form ,[2] and three years later, Moore introduced an alternative method.[3] Others have later introduced alternative methods for IFT,[4] and automatised the process [5][6]
The Glatter method of IFT
This is an brief outline of the method introduced by Otto Glatter.[2] For simplicity, we use in the following.
In indirect Fourier transformation, a guess on the largest distance in the particle is given, and an initial distance distribution function is expressed as a sum of cubic spline functions evenly distributed on the interval (0,):
1
where are scalar coefficients. The relation between the scattering intensity and the is:
2
Inserting the expression for pi(r) (1) into (2) and using that the transformation from to is linear gives:
where is given as:
The 's are unchanged under the linear Fourier transformation and can be fitted to data, thereby obtaining the coefficients . Inserting these new coefficients into the expression for gives a final . The coefficients are chosen to minimise the of the fit, given by:
where is the number of datapoints and is the standard deviations on data point . The fitting problem is ill posed and a very oscillating function would give the lowest despite being physically unrealistic. Therefore, a smoothness function is introduced:
.
The larger the oscillations, the higher . Instead of minimizing , the Lagrangian is minimized, where the Lagrange multiplier is denoted the smoothness parameter.
The method is indirect in the sense that the FT is done in several steps: .
^ abO. Glatter (1977). "A new method for the evaluation of small-angle scattering data". Journal of Applied Crystallography. 10 (5): 415–421. doi:10.1107/s0021889877013879.
^P.B. Moore (1980). "Small-angle scattering. Information content and error analysis". Journal of Applied Crystallography. 13 (2): 168–175. doi:10.1107/s002188988001179x.
^B. Vestergaard and S. Hansen (2006). "Application of Bayesian analysis to indirect Fourier transformation in small-angle scattering". Journal of Applied Crystallography. 39 (6): 797–804. doi:10.1107/S0021889806035291.