# parallelepiped model # Note: model title and parameter table are inserted automatically r""" Definition ---------- This model calculates the scattering from a rectangular parallelepiped (:numref:`parallelepiped-image`). If you need to apply polydispersity, see also :ref:`rectangular-prism`. For information about polarised and magnetic scattering, see the :ref:`magnetism` documentation. .. _parallelepiped-image: .. figure:: img/parallelepiped_geometry.jpg Parallelepiped with the corresponding definition of sides. The three dimensions of the parallelepiped (strictly here a cuboid) may be given in *any* size order. To avoid multiple fit solutions, especially with Monte-Carlo fit methods, it may be advisable to restrict their ranges. There may be a number of closely similar "best fits", so some trial and error, or fixing of some dimensions at expected values, may help. The form factor is normalized by the particle volume and the 1D scattering intensity $I(q)$ is then calculated as: .. Comment by Miguel Gonzalez: I am modifying the original text because I find the notation a little bit confusing. I think that in most textbooks/papers, the notation P(Q) is used for the form factor (adim, P(Q=0)=1), although F(q) seems also to be used. But here (as for many other models), P(q) is used to represent the scattering intensity (in cm-1 normally). It would be good to agree on a common notation. .. math:: I(q) = \frac{\text{scale}}{V} (\Delta\rho \cdot V)^2 \left< P(q, \alpha, \beta) \right> + \text{background} where the volume $V = A B C$, the contrast is defined as $\Delta\rho = \rho_\text{p} - \rho_\text{solvent}$, $P(q, \alpha, \beta)$ is the form factor corresponding to a parallelepiped oriented at an angle $\alpha$ (angle between the long axis C and $\vec q$), and $\beta$ ( the angle between the projection of the particle in the $xy$ detector plane and the $y$ axis) and the averaging $\left<\ldots\right>$ is applied over all orientations. Assuming $a = A/B < 1$, $b = B /B = 1$, and $c = C/B > 1$, the form factor is given by (Mittelbach and Porod, 1961 [#Mittelbach]_) .. math:: P(q, \alpha) = \int_0^1 \phi_Q\left(\mu \sqrt{1-\sigma^2},a\right) \left[S(\mu c \sigma/2)\right]^2 d\sigma with .. math:: \phi_Q(\mu,a) &= \int_0^1 \left\{S\left[\frac{\mu}{2}\cos\left(\frac{\pi}{2}u\right)\right] S\left[\frac{\mu a}{2}\sin\left(\frac{\pi}{2}u\right)\right] \right\}^2 du \\ S(x) &= \frac{\sin x}{x} \\ \mu &= qB where substitution of $\sigma = cos\alpha$ and $\beta = \pi/2 \ u$ have been applied. NB: The 2nd virial coefficient of the parallelepiped is calculated based on the averaged effective radius, after appropriately sorting the three dimensions, to give an oblate or prolate particle, $(=\sqrt{AB/\pi})$ and length $(= C)$ values, and used as the effective radius for $S(q)$ when $P(q) \cdot S(q)$ is applied. For 2d data the orientation of the particle is required, described using angles $\theta$, $\phi$ and $\Psi$ as in the diagrams below, for further details of the calculation and angular dispersions see :ref:`orientation` . .. Comment by Miguel Gonzalez: The following text has been commented because I think there are two mistakes. Psi is the rotational angle around C (but I cannot understand what it means against the q plane) and psi=0 corresponds to a||x and b||y. The angle $\Psi$ is the rotational angle around the $C$ axis against the $q$ plane. For example, $\Psi = 0$ when the $B$ axis is parallel to the $x$-axis of the detector. The angle $\Psi$ is the rotational angle around the $C$ axis. For $\theta = 0$ and $\phi = 0$, $\Psi = 0$ corresponds to the $B$ axis oriented parallel to the y-axis of the detector with $A$ along the x-axis. For other $\theta$, $\phi$ values, the parallelepiped has to be first rotated $\theta$ degrees in the $z-x$ plane and then $\phi$ degrees around the $z$ axis, before doing a final rotation of $\Psi$ degrees around the resulting $C$ axis of the particle to obtain the final orientation of the parallelepiped. .. _parallelepiped-orientation: .. figure:: img/parallelepiped_angle_definition.png Definition of the angles for oriented parallelepiped, shown with $A (abc[2] - abc[1]) length = np.where(selector, abc[0], abc[2]) # surface average radius (rough approximation) radius = sqrt(np.where(~selector, abc[0]*abc[1], abc[1]*abc[2]) / pi) ddd = 0.75 * radius * (2*radius*length + (length + radius)*(length + pi*radius)) return 0.5 * (ddd) ** (1. / 3.) # VR defaults to 1.0 def random(): length = 10**np.random.uniform(1, 4.7, size=3) pars = dict( length_a=length[0], length_b=length[1], length_c=length[2], ) return pars # parameters for demo demo = dict(scale=1, background=0, sld=6.3, sld_solvent=1.0, length_a=35, length_b=75, length_c=400, theta=45, phi=30, psi=15, length_a_pd=0.1, length_a_pd_n=10, length_b_pd=0.1, length_b_pd_n=1, length_c_pd=0.1, length_c_pd_n=1, theta_pd=10, theta_pd_n=1, phi_pd=10, phi_pd_n=1, psi_pd=10, psi_pd_n=10) # rkh 7/4/17 add random unit test for 2d, note make all params different, # 2d values not tested against other codes or models qx, qy = 0.2 * cos(pi/6.), 0.2 * sin(pi/6.) tests = [[{}, 0.2, 0.17758004974], [{}, [0.2], [0.17758004974]], [{'theta':10.0, 'phi':20.0}, (qx, qy), 0.0089517140475], [{'theta':10.0, 'phi':20.0}, [(qx, qy)], [0.0089517140475]], ] del qx, qy # not necessary to delete, but cleaner