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	<entry>
		<id>http://gisaxs.com/index.php?title=Form_Factor:Cube&amp;diff=600&amp;oldid=prev</id>
		<title>KevinYager at 21:07, 13 June 2014</title>
		<link rel="alternate" type="text/html" href="http://gisaxs.com/index.php?title=Form_Factor:Cube&amp;diff=600&amp;oldid=prev"/>
		<updated>2014-06-13T21:07:49Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 21:07, 13 June 2014&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class=&#039;diff-marker&#039;&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[Image:Cube.png|200px|right]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&#039;diff-marker&#039;&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Equations==&lt;/div&gt;&lt;/td&gt;&lt;td class=&#039;diff-marker&#039;&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Equations==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&#039;diff-marker&#039;&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;For cubes of edge-length 2&amp;#039;&amp;#039;R&amp;#039;&amp;#039; (volume &amp;lt;math&amp;gt;V_{cube}=(2R)^3&amp;lt;/math&amp;gt;):&lt;/div&gt;&lt;/td&gt;&lt;td class=&#039;diff-marker&#039;&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;For cubes of edge-length 2&amp;#039;&amp;#039;R&amp;#039;&amp;#039; (volume &amp;lt;math&amp;gt;V_{cube}=(2R)^3&amp;lt;/math&amp;gt;):&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>KevinYager</name></author>
		
	</entry>
	<entry>
		<id>http://gisaxs.com/index.php?title=Form_Factor:Cube&amp;diff=327&amp;oldid=prev</id>
		<title>68.194.136.6: Created page with &quot;==Equations== For cubes of edge-length 2&#039;&#039;R&#039;&#039; (volume &lt;math&gt;V_{cube}=(2R)^3&lt;/math&gt;): ===Form Factor Amplitude=== ::&lt;math&gt; F_{cube}(\mathbf{q})  = \left\{          \begin{array...&quot;</title>
		<link rel="alternate" type="text/html" href="http://gisaxs.com/index.php?title=Form_Factor:Cube&amp;diff=327&amp;oldid=prev"/>
		<updated>2014-06-05T02:00:11Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;==Equations== For cubes of edge-length 2&amp;#039;&amp;#039;R&amp;#039;&amp;#039; (volume &amp;lt;math&amp;gt;V_{cube}=(2R)^3&amp;lt;/math&amp;gt;): ===Form Factor Amplitude=== ::&amp;lt;math&amp;gt; F_{cube}(\mathbf{q})  = \left\{          \begin{array...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;==Equations==&lt;br /&gt;
For cubes of edge-length 2&amp;#039;&amp;#039;R&amp;#039;&amp;#039; (volume &amp;lt;math&amp;gt;V_{cube}=(2R)^3&amp;lt;/math&amp;gt;):&lt;br /&gt;
===Form Factor Amplitude===&lt;br /&gt;
::&amp;lt;math&amp;gt;&lt;br /&gt;
F_{cube}(\mathbf{q})  = \left\{&lt;br /&gt;
    &lt;br /&gt;
    \begin{array}{c l}&lt;br /&gt;
&lt;br /&gt;
        \Delta\rho V_{cube} \mathrm{sinc}(q_x R) \mathrm{sinc}(q_y R) \mathrm{sinc}(q_z R)&lt;br /&gt;
        &amp;amp; \mathrm{when} \,\, \mathbf{q}\neq(0,0,0)\\&lt;br /&gt;
        \Delta\rho V_{cube}&lt;br /&gt;
        &amp;amp; \mathrm{when} \,\, \mathbf{q}=(0,0,0) \\&lt;br /&gt;
    \end{array}&lt;br /&gt;
    &lt;br /&gt;
\right.&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
===Isotropic Form Factor Intensity===&lt;br /&gt;
&lt;br /&gt;
::&amp;lt;math&amp;gt;&lt;br /&gt;
P_{cube}(q)  = \left\{&lt;br /&gt;
    &lt;br /&gt;
    \begin{array}{c l}&lt;br /&gt;
&lt;br /&gt;
        \frac{16 \Delta\rho^2 V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi}&lt;br /&gt;
        \frac{1}{\sin\theta}\left( \frac{ \sin(q_zR) }{ \sin(2\theta) } \right)^2&lt;br /&gt;
         \int_{0}^{2\pi} &lt;br /&gt;
             \left(&lt;br /&gt;
             \frac{\sin(q_xR)\sin(q_yR)}&lt;br /&gt;
                  { \sin(2\phi) }&lt;br /&gt;
             \right)^2&lt;br /&gt;
         \mathrm{d}\phi \mathrm{d}\theta&lt;br /&gt;
&lt;br /&gt;
        &amp;amp; \mathrm{when} \,\, q\neq0\\&lt;br /&gt;
        4\pi \Delta\rho^2 V_{cube}^2&lt;br /&gt;
        &amp;amp; \mathrm{when} \,\, q=0 \\&lt;br /&gt;
    \end{array}&lt;br /&gt;
    &lt;br /&gt;
\right.&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==Sources==&lt;br /&gt;
====Byeongdu Lee (APS)====&lt;br /&gt;
From [http://www.nature.com/nmat/journal/v9/n11/extref/nmat2870-s1.pdf Supplementary Information] of: Matthew R. Jones, Robert J. Macfarlane, Byeongdu Lee, Jian Zhang, Kaylie L. Young, Andrew J. Senesi, and Chad A. Mirkin &amp;quot;[http://www.nature.com/nmat/journal/v9/n11/full/nmat2870.html DNA-nanoparticle superlattices formed from anisotropic building blocks]&amp;quot; Nature Materials &amp;#039;&amp;#039;&amp;#039;9&amp;#039;&amp;#039;&amp;#039;, 913-917, &amp;#039;&amp;#039;&amp;#039;2010&amp;#039;&amp;#039;&amp;#039;. [http://dx.doi.org/10.1038/nmat2870 doi: 10.1038/nmat2870]&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
F_{cube}(\mathbf{q}) = V_{cube} \mathrm{sinc}(q_xR) \mathrm{sinc}(q_yR) \mathrm{sinc}(q_zR)&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
Where &amp;#039;&amp;#039;2R&amp;#039;&amp;#039; is the edge length of the cube, such that the volume is:&lt;br /&gt;
::&amp;lt;math&amp;gt; V_{cube} = \left(2R \right)^3 &amp;lt;/math&amp;gt;&lt;br /&gt;
and sinc is the [http://en.wikipedia.org/wiki/Sinc_function unnormalized sinc function]:&lt;br /&gt;
::&amp;lt;math&amp;gt;&lt;br /&gt;
\mathrm{sinc}(x) = \left\{&lt;br /&gt;
\begin{array}{c l}&lt;br /&gt;
  1 &amp;amp; \mathrm{when} \,\, x=0 \\&lt;br /&gt;
  \frac{\sin x}{x} &amp;amp; \mathrm{when} \,\, x\neq0&lt;br /&gt;
\end{array}&lt;br /&gt;
\right.&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
====Pedersen====&lt;br /&gt;
From Pedersen review, [http://linkinghub.elsevier.com/retrieve/pii/S0001868697003126 Analysis of small-angle scattering data from colloids and polymer solutions: modeling and least-squares fitting] Jan Skov Pedersen, Advances in Colloid and Interface Science 1997, 70, 171. [http://dx.doi.org/10.1016/S0001-8686(97)00312-6 doi: 10.1016/S0001-8686(97)00312-6]&lt;br /&gt;
For a rectangular [http://en.wikipedia.org/wiki/Parallelepiped parallelepipedon] with edges &amp;#039;&amp;#039;a&amp;#039;&amp;#039;, &amp;#039;&amp;#039;b&amp;#039;&amp;#039;, and &amp;#039;&amp;#039;c&amp;#039;&amp;#039;:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
P(q, a,b,c) = \frac{2}{\pi}\int_{0}^{\pi/2}\int_{0}^{\pi/2} &lt;br /&gt;
    \frac { \sin(q a \sin\alpha\cos\beta) }{ q a \sin\alpha\cos\beta }&lt;br /&gt;
    \frac { \sin(q b \sin\alpha\cos\beta) }{ q b \sin\alpha\sin\beta }&lt;br /&gt;
    \frac { \sin(q c \cos\alpha) }{ q c \cos\alpha }&lt;br /&gt;
    \sin\alpha \mathrm{d}\alpha \mathrm{d}\beta&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
For a cube of edge length &amp;#039;&amp;#039;a&amp;#039;&amp;#039; this would be:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
P_{cube}(q,a) = \frac{2}{\pi q^3 a^3}\int_{0}^{\pi/2}\int_{0}^{\pi/2} &lt;br /&gt;
    \frac { \sin(q a \sin\alpha\cos\beta) }{ \sin\alpha\cos\beta }&lt;br /&gt;
    \frac { \sin(q a \sin\alpha\cos\beta) }{ \sin\alpha\sin\beta }&lt;br /&gt;
    \frac { \sin(q a \cos\alpha) }{ \cos\alpha }&lt;br /&gt;
    \sin\alpha \mathrm{d}\alpha \mathrm{d}\beta&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==Derivations==&lt;br /&gt;
===Form Factor===&lt;br /&gt;
For a cube of edge-length 2&amp;#039;&amp;#039;R&amp;#039;&amp;#039;, the volume is:&lt;br /&gt;
::&amp;lt;math&amp;gt; V_{cube} = \left(2R \right)^3 &amp;lt;/math&amp;gt;&lt;br /&gt;
We integrate over the interior of the cube, using [http://en.wikipedia.org/wiki/Cartesian_coordinate_system Cartesian coordinates]:&lt;br /&gt;
::&amp;lt;math&amp;gt;\mathbf{q} = (q_x, q_y, q_z)&amp;lt;/math&amp;gt;&lt;br /&gt;
::&amp;lt;math&amp;gt;\mathbf{r} = (x, y, z)&amp;lt;/math&amp;gt;&lt;br /&gt;
::&amp;lt;math&amp;gt;\mathbf{q}\cdot\mathbf{r} = q_x x + q_y y + q_z z&amp;lt;/math&amp;gt;&lt;br /&gt;
Such that:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
F_{cube}(\mathbf{q}) &amp;amp; = \int\limits_V e^{i \mathbf{q} \cdot \mathbf{r} } \mathrm{d}\mathbf{r} \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = \int_{z=-R}^{R}\int_{y=-R}^{R}\int_{x=-R}^{R} e^{i (q_x x + q_y y + q_z z) } \mathrm{d}x \mathrm{d}y \mathrm{d}z \\&lt;br /&gt;
 &amp;amp; = \int_{-R}^{R} e^{i q_x x} \mathrm{d}x \int_{-R}^{R} e^{i q_y y} \mathrm{d}y  \int_{-R}^{R} e^{i q_z z} \mathrm{d}z &lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
Each integral is of the same form:&lt;br /&gt;
::&amp;lt;math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
f_{cube,x}(q_x) &amp;amp; = \int_{-R}^{R} e^{i q_x x} \mathrm{d}x \\&lt;br /&gt;
 &amp;amp; = \int_{-R}^{R} \left[\cos(q_x x) + i \sin(q_x x)\right] \mathrm{d}x \\&lt;br /&gt;
 &amp;amp; = \left[\frac{-1}{q_x}\sin(q_x x) + \frac{i}{q_x} \cos(q_x x)\right]_{x=-R}^{R} \\&lt;br /&gt;
 &amp;amp; = \left[ \frac{-1}{q_x}\sin(q_x R) + \frac{i}{q_x} \cos(q_x R) - \frac{-1}{q_x}\sin(-q_x R) - \frac{i}{q_x} \cos(-q_x R)  \right] \\&lt;br /&gt;
 &amp;amp; = \left[ -\frac{1}{q_x}\sin(q_x R) - \frac{1}{q_x}\sin(q_x R)   \right] \\&lt;br /&gt;
 &amp;amp; = -\frac{2}{q_x}\sin(q_x R) \\&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
Which gives:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
F_{cube}(\mathbf{q}) &amp;amp; = \frac{2}{q_x}\sin(q_x R) \frac{2}{q_y}\sin(q_y R) \frac{2}{q_z}\sin(q_z R) \\&lt;br /&gt;
 &amp;amp; = 2^3R^3 \frac{\sin(q_x R)}{q_x R} \frac{\sin(q_y R)}{q_y R} \frac{\sin(q_z R)}{q_z R} \\&lt;br /&gt;
 &amp;amp; = V_{cube} \mathrm{sinc}(q_x R) \mathrm{sinc}(q_y R) \mathrm{sinc}(q_z R)&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
===Form Factor at &amp;#039;&amp;#039;q&amp;#039;&amp;#039;=0===&lt;br /&gt;
At small &amp;#039;&amp;#039;q&amp;#039;&amp;#039;:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
F_{cube}\left(0\right)  = V_{cube}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
===Isotropic Form Factor===&lt;br /&gt;
To average over all possible orientations, we note:&lt;br /&gt;
::&amp;lt;math&amp;gt;\mathbf{q}=(q_x,q_y,q_z)=(-q\sin\theta\cos\phi,q\sin\theta\sin\phi,q\cos\theta)&amp;lt;/math&amp;gt;&lt;br /&gt;
and use:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
\left\langle F_{cube}(\mathbf{q}) \right\rangle_{\mathrm{iso}} &amp;amp; = \int\limits_{S} F_{cube}(\mathbf{q}) \mathrm{d}\mathbf{s} \\&lt;br /&gt;
 &amp;amp; = \int_{\phi=0}^{2\pi}\int_{\theta=0}^{\pi} F_{cube}(-q\sin\theta\cos\phi,q\sin\theta\sin\phi,q\cos\theta) \sin\theta\mathrm{d}\theta\mathrm{d}\phi \\&lt;br /&gt;
 &amp;amp; = V_{cube} \int_{0}^{2\pi}\int_{0}^{\pi} \mathrm{sinc}(q_x R) \mathrm{sinc}(q_y R) \mathrm{sinc}(q_z R) \sin\theta\mathrm{d}\theta\mathrm{d}\phi \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = V_{cube} \int_{0}^{\pi} \sin\theta \left( \frac{\sin(q_z R)}{q_z R} \right) &lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \left( \frac{\sin(q_x R)}{q_x R} \right)&lt;br /&gt;
           \left( \frac{\sin(q_y R)}{q_y R} \right)&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = \frac{V_{cube}}{ (qR)^3 } \int_{0}^{\pi} \frac{\sin\theta \sin(q_z R)}{\cos \theta} &lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin(q_x R) \sin(q_y R) }{- \sin \theta \cos \phi \sin \theta \sin \phi}&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = - \frac{V_{cube}}{ (qR)^3 } \int_{0}^{\pi} \frac{\sin(q_z R)}{\sin\theta \cos\theta} &lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin(q_x R) \sin(q_y R) }{\sin\phi \cos\phi }&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = - \frac{4 V_{cube}}{ (qR)^3 } \int_{0}^{\pi} \frac{\sin(q_z R)}{\sin(2\theta)} &lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin(q_x R) \sin(q_y R) }{\sin(2\phi)}&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
From symmetry, it is sufficient to integrate over only one of the eight octants: &lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
\left\langle F_{cube}(\mathbf{q}) \right\rangle_{\mathrm{iso}}&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = - \frac{32 V_{cube}}{ (qR)^3 } \int_{0}^{\pi/2} \frac{\sin(q_z R)}{\sin(2\theta)} &lt;br /&gt;
       \int_{0}^{\pi/2} &lt;br /&gt;
           \frac{\sin(q_x R) \sin(q_y R) }{\sin(2\phi)}&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
===Isotropic Form Factor Intensity===&lt;br /&gt;
To average over all possible orientations, we note:&lt;br /&gt;
::&amp;lt;math&amp;gt;\mathbf{q}=(q_x,q_y,q_z)=(-q\sin\theta\cos\phi,q\sin\theta\sin\phi,q\cos\theta)&amp;lt;/math&amp;gt;&lt;br /&gt;
and use:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
P_{cube}(q) &amp;amp; = \int\limits_{S} | F_{cube}(\mathbf{q}) |^2 \mathrm{d}\mathbf{s} \\&lt;br /&gt;
 &amp;amp; = \int_{\phi=0}^{2\pi}\int_{\theta=0}^{\pi} | F_{cube}(-q\sin\theta\cos\phi,q\sin\theta\sin\phi,q\cos\theta)|^2 \sin\theta\mathrm{d}\theta\mathrm{d}\phi \\&lt;br /&gt;
 &amp;amp; = V_{cube}^2 \int_{0}^{2\pi}\int_{0}^{\pi} | \mathrm{sinc}(q_x R) \mathrm{sinc}(q_y R) \mathrm{sinc}(q_z R) |^2 \sin\theta\mathrm{d}\theta\mathrm{d}\phi \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = V_{cube}^2 \int_{0}^{\pi} \sin\theta \left( \frac{\sin(q\cos(\theta)R)}{q \cos(\theta)R} \right)^2 &lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \left( \frac{\sin(-q\sin(\theta)\cos(\phi)R)}{-q \sin(\theta)\cos(\phi)R} \right)^2&lt;br /&gt;
           \left( \frac{\sin(q\sin(\theta)\sin(\phi)R)}{q \sin(\theta)\sin(\phi)R} \right)^2&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = \frac{V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi}&lt;br /&gt;
      \frac{\sin\theta \sin^2(q\cos(\theta)R)}{\cos^2(\theta)\sin^2(\theta)\sin^2(\theta)}&lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin^2(-q\sin(\theta)\cos(\phi)R)\sin^2(q\sin(\theta)\sin(\phi)R)}&lt;br /&gt;
                {\cos^2(\phi)\sin^2(\phi)}&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = \frac{V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi}&lt;br /&gt;
      \frac{ \sin^2(q\cos(\theta)R) }{ \sin^3(\theta)\cos^2(\theta) }&lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin^2(-q\sin(\theta)\cos(\phi)R)\sin^2(q\sin(\theta)\sin(\phi)R)}&lt;br /&gt;
                { ( \frac{1}{2} \sin(2\phi) )^2 }&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
Solving integrals that involve nested trigonometric functions is not generally possible. However we can simplify in preparation for performing the integrals numerically:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
P_{cube}(q)&lt;br /&gt;
 &amp;amp; = \frac{V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi}&lt;br /&gt;
      \frac{ \sin^2(q_zR) }{ \sin^3(\theta)\cos^2(\theta) }&lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin^2(q_xR)\sin^2(q_yR)}&lt;br /&gt;
                { ( \frac{1}{2} \sin(2\phi) )^2 }&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = \frac{2^2 V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi}&lt;br /&gt;
      \frac{ \sin^2(q_zR) }{ \sin(\theta)(\frac{1}{2}\sin(2\theta) )^2 }&lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \frac{\sin^2(q_xR)\sin^2(q_yR)}&lt;br /&gt;
                { ( \sin(2\phi) )^2 }&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
 &amp;amp; = \frac{16 V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi}&lt;br /&gt;
      \frac{1}{\sin\theta}\left( \frac{ \sin(q_zR) }{ \sin(2\theta) } \right)^2&lt;br /&gt;
       \int_{0}^{2\pi} &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(q_xR)\sin(q_yR)}&lt;br /&gt;
                { \sin(2\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
From symmetry, it is sufficient to integrate over only one of the eight octants:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
P_{cube}(q)&lt;br /&gt;
 &amp;amp; = \frac{128 V_{cube}^2}{ (qR)^6 } \int_{0}^{\pi/2}&lt;br /&gt;
      \frac{1}{\sin\theta}\left( \frac{ \sin(q_zR) }{ \sin(2\theta) } \right)^2&lt;br /&gt;
       \int_{0}^{\pi/2} &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(q_xR)\sin(q_yR)}&lt;br /&gt;
                { \sin(2\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
       \mathrm{d}\phi \mathrm{d}\theta \\&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
===Isotropic Form Factor Intensity contribution when &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt;=0===&lt;br /&gt;
The integrand of the &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt;-integral becomes:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(q_xR)\sin(q_yR)}&lt;br /&gt;
                { \sin(2\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
 &amp;amp; = &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)\cos(\phi)R)\sin(q \sin(\theta) \sin(\phi) R)}&lt;br /&gt;
                { \sin(2\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
        \\&lt;br /&gt;
 &amp;amp; = &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)\cos(\phi)R)\sin(q \sin(\theta) \sin(\phi) R)}&lt;br /&gt;
                { 2 \sin(\phi) \cos(\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
        \\&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
For small &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt;, the various &amp;lt;math&amp;gt;\sin(\phi)&amp;lt;/math&amp;gt; can be replaced by &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt;, and the various &amp;lt;math&amp;gt;\cos(\phi)&amp;lt;/math&amp;gt; can be replaced by &amp;lt;math&amp;gt;1&amp;lt;/math&amp;gt;:&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
\lim_{\phi\to0}&lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(q_xR)\sin(q_yR)}&lt;br /&gt;
                { \sin(2\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
 &amp;amp; = &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)R)\sin(q \sin(\theta) \phi R)}&lt;br /&gt;
                { 2 \phi  }&lt;br /&gt;
           \right)^2&lt;br /&gt;
        \\&lt;br /&gt;
 &amp;amp; = &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)R) q \sin(\theta) \phi R}&lt;br /&gt;
                { 2 \phi  }&lt;br /&gt;
           \right)^2&lt;br /&gt;
        \\&lt;br /&gt;
 &amp;amp; = &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)R) q \sin(\theta) R}&lt;br /&gt;
                { 2 }&lt;br /&gt;
           \right)^2&lt;br /&gt;
        \\&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
Which is a constant (with respect to &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt;). The part of the &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt;-integral near &amp;lt;math&amp;gt;\phi=0&amp;lt;/math&amp;gt; has the contribution:&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
       \int_{\phi=0}^{\phi=0+\delta} &lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(q_xR)\sin(q_yR)}&lt;br /&gt;
                { \sin(2\phi) }&lt;br /&gt;
           \right)^2&lt;br /&gt;
       \mathrm{d}\phi&lt;br /&gt;
  &amp;amp; =&lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)R) q \sin(\theta) R}&lt;br /&gt;
                { 2 }&lt;br /&gt;
           \right)^2&lt;br /&gt;
       \int_{\phi=0}^{\phi=0+\delta} &lt;br /&gt;
       \mathrm{d}\phi \\&lt;br /&gt;
  &amp;amp; =&lt;br /&gt;
           \left(&lt;br /&gt;
           \frac{\sin(-q \sin(\theta)R) q \sin(\theta) R}&lt;br /&gt;
                { 2 }&lt;br /&gt;
           \right)^2&lt;br /&gt;
       \delta \\&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
===Isotropic Form Factor Intensity at &amp;#039;&amp;#039;q&amp;#039;&amp;#039;=0===&lt;br /&gt;
At very small &amp;#039;&amp;#039;q&amp;#039;&amp;#039;:&lt;br /&gt;
:&amp;lt;math&amp;gt;&lt;br /&gt;
\begin{alignat}{2}&lt;br /&gt;
&lt;br /&gt;
P_{cube}(0) &amp;amp; = V_{cube}^2 \int_{\phi=0}^{2\pi}\int_{\theta=0}^{\pi}\sin\theta\mathrm{d}\theta\mathrm{d}\phi \\&lt;br /&gt;
 &amp;amp; = 4\pi V_{cube}^2 \\&lt;br /&gt;
&lt;br /&gt;
\end{alignat}&lt;br /&gt;
&amp;lt;/math&amp;gt;&lt;/div&gt;</summary>
		<author><name>68.194.136.6</name></author>
		
	</entry>
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