Difference between revisions of "Ewald sphere"

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(Created page with "The '''Ewald sphere''' is the surface, in reciprocal-space, that all experimentally-observed scattering arises from. (Strictly, only the ''elastic'' scattering comes from ...")
 
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Consider reciprocal-space in the incident beam coordinate system: <math>(q_x,q_y,q_z)</math>. The incident beam is the vector <math>\mathbf{k_i} = \langle 0,-k,0 \rangle</math>, where:
 
Consider reciprocal-space in the incident beam coordinate system: <math>(q_x,q_y,q_z)</math>. The incident beam is the vector <math>\mathbf{k_i} = \langle 0,-k,0 \rangle</math>, where:
 
: <math>k = \frac{2 \pi}{\lambda}</math>
 
: <math>k = \frac{2 \pi}{\lambda}</math>
where <math>\lambda</math> is, of course, the wavelength of the incident beam. An inelastic scattering event has momentum vector, and resultant momentum transfer, <math>\mathbf{q}</math>, of:
+
where <math>\lambda</math> is, of course, the wavelength of the incident beam. An elastic scattering event has momentum vector, and resultant [[momentum transfer]], <math>\mathbf{q}</math>, of:
 
: <math>
 
: <math>
 
\begin{alignat}{2}
 
\begin{alignat}{2}
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===[[TSAXS]]===
 
===[[TSAXS]]===
In conventional [[SAXS]], the signal of interest is isotropic: i.e. we only care about <math>|\mathbf{q}| = q</math>, and not the individual (directional) components <math>(q_x,q_y,q_z)</math>. In such a case:
+
In conventional [[SAXS]], the signal of interest is isotropic: i.e. we only care about <math>|\mathbf{q}| = q</math>, and not the individual (directional) components <math>(q_x,q_y,q_z)</math>. In such a case we use the form of ''q'' derived above:
 +
:<math>
 +
q  = \frac{4 \pi}{\lambda} \sin(\theta_s)
 +
</math>
 +
In the more general case of probing an anisotropic material (e.g. [[CD-SAXS]]), one must take into account the full ''q''-vector, and in particular the relative orientation of the incident beam and the sample: i.e. the relative orientation of the Ewald sphere and the reciprocal-space.
  
 
===[[GISAXS]]===
 
===[[GISAXS]]===

Revision as of 09:28, 24 June 2014

The Ewald sphere is the surface, in reciprocal-space, that all experimentally-observed scattering arises from. (Strictly, only the elastic scattering comes from the Ewald sphere; inelastic scattering is so-called 'off-shell'.) A peak observed on the detector indicates that a reciprocal-space peak is intersecting with the Ewald sphere.

Geometry

Definitions

Consider reciprocal-space in the incident beam coordinate system: . The incident beam is the vector , where:

where is, of course, the wavelength of the incident beam. An elastic scattering event has momentum vector, and resultant momentum transfer, , of:

where is the full scattering angle. The Ewald sphere is centered about the point and thus has the equation:

TSAXS

In conventional SAXS, the signal of interest is isotropic: i.e. we only care about , and not the individual (directional) components . In such a case we use the form of q derived above:

In the more general case of probing an anisotropic material (e.g. CD-SAXS), one must take into account the full q-vector, and in particular the relative orientation of the incident beam and the sample: i.e. the relative orientation of the Ewald sphere and the reciprocal-space.

GISAXS

Now let us assume that the incident beam strikes a thin film mounted to a substrate. The incident beam is in the grazing-incidence geometry (e.g. GISAXS, and we denote the angle between the incident beam and the film surface as . The reciprocal-space of the sample is thus rotated by with respect to the beam reciprocal-space coordinates. We denote the sample's reciprocal coordinate system by uppercase, , and note that the equation of the Ewald sphere becomes (the center of the sphere is at ):