Fcc Paracrystal

#fcc paracrystal model #note model title and parameter table are automatically inserted #note - calculation requires double precision .. warning:: This model and this model description are under review following concerns raised by SasView users. If you need to use this model, please email help@sasview.org for the latest situation. *The SasView Developers. September 2018.*

Definition

Calculates the scattering from a **face-centered cubic lattice** with paracrystalline distortion. Thermal vibrations are considered to be negligible, and the size of the paracrystal is infinitely large. Paracrystalline distortion is assumed to be isotropic and characterized by a Gaussian distribution.

The scattering intensity $I(q)$ is calculated as

$$ I(q) = \frac{\text{scale}}{V_p} V_\text{lattice} P(q) Z(q)
$$
where *scale* is the volume fraction of spheres, $V_p$ is the volume of the primary particle, $V_\text{lattice}$ is a volume correction for the crystal structure, $P(q)$ is the form factor of the sphere (normalized), and $Z(q)$ is the paracrystalline structure factor for a face-centered cubic structure.

Equation (1) of the 1990 reference[#CIT1990]_ is used to calculate $Z(q)$, using equations (23)-(25) from the 1987 paper[#CIT1987]_ for $Z1$, $Z2$, and $Z3$.

The lattice correction (the occupied volume of the lattice) for a face-centered cubic structure of particles of radius $R$ and nearest neighbor separation $D$ is

$$ V_\text{lattice} = \frac{16\pi}{3}\frac{R^3}{\left(D\sqrt{2}\right)^3}
$$
The distortion factor (one standard deviation) of the paracrystal is included in the calculation of $Z(q)$

$$ \Delta a = gD
$$
where $g$ is a fractional distortion based on the nearest neighbor distance.

Face-centered cubic lattice.

For a crystal, diffraction peaks appear at reduced q-values given by

$$ \frac{qD}{2\pi} = \sqrt{h^2 + k^2 + l^2}
$$
where for a face-centered cubic lattice $h, k , l$ all odd or all even are allowed and reflections where $h, k, l$ are mixed odd/even are forbidden. Thus the peak positions correspond to (just the first 5)

$$ \begin{array}{cccccc} q/q_0 & 1 & \sqrt{4/3} & \sqrt{8/3} & \sqrt{11/3} & \sqrt{4} \\ \text{Indices} & (111) & (200) & (220) & (311) & (222) \end{array}
$$
.. note::

The calculation of $Z(q)$ is a double numerical integral that must be carried out with a high density of points to properly capture the sharp peaks of the paracrystalline scattering. So be warned that the calculation is slow. Fitting of any experimental data must be resolution smeared for any meaningful fit. This makes a triple integral which may be very slow.

The 2D (Anisotropic model) is based on the reference below where $I(q)$ is approximated for 1d scattering. Thus the scattering pattern for 2D may not be accurate particularly at low $q$. For general details of the calculation and angular dispersions for oriented particles see `orientation` . Note that we are not responsible for any incorrectness of the 2D model computation.

Orientation of the crystal with respect to the scattering plane, when $\theta = \phi = 0$ the $c$ axis is along the beam direction (the $z$ axis).

References

.. [#CIT1987] Hideki Matsuoka et. al. *Physical Review B*, 36 (1987) 1754-1765 (Original Paper) .. [#CIT1990] Hideki Matsuoka et. al. *Physical Review B*, 41 (1990) 3854 -3856 (Corrections to FCC and BCC lattice structure calculation)

Authorship and Verification

**Author:** NIST IGOR/DANSE **Date:** pre 2010
**Last Modified by:** Paul Butler **Date:** September 29, 2016
**Last Reviewed by:** Richard Heenan **Date:** March 21, 2016