Difference between revisions of "Grating alignment"

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In order to align a lithographic (nanoscale) grating with the incident x-ray beam, one must rotate it carefully about the <math>\phi</math> axis (i.e. the film normal direction) until the grating lines are exactly parallel to the incident beam. If the grating is not aligned, the scattering spots seen in [[GISAXS]] will not be symmetric.
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In order to align a lithographic (nanoscale) grating with the incident [[x-ray]] beam, one must rotate it carefully about the <math>\phi</math> axis (i.e. the film normal direction) until the grating lines are exactly parallel to the incident beam. If the grating is not aligned, the [[scattering]] spots seen in [[GISAXS]] will not be symmetric.
  
 
==Aligning==
 
==Aligning==

Revision as of 10:04, 14 June 2014

In order to align a lithographic (nanoscale) grating with the incident x-ray beam, one must rotate it carefully about the axis (i.e. the film normal direction) until the grating lines are exactly parallel to the incident beam. If the grating is not aligned, the scattering spots seen in GISAXS will not be symmetric.

Aligning

If the grating is not aligned with the incident beam, the scattering will be asymmetric, with a ring of peaks appearing on one side or the other.

  • If "ring of spots" is on right you must rotate stage counterclockwise (as viewed from above)
  • If "ring of spots" is on left you must rotate stage clockwise (as viewed from above)
phi = −0.39°
phi = −0.09°
phi = 0.00° (aligned)
phi = 0.01°
phi = 0.11°
phi = 0.61°

Origin of Ring

The "ring" of bright scattering spots that one observes arises from the intersection of the Ewald sphere with the reciprocal lattice. Because lithographic gratings are so well-ordered, the reciprocal-space peaks are extremely sharp. Thus, the scattering intensity is strongly concentrated into the plane. The curved Ewald sphere intersects this plane to give rise to a circle of intense scattering.

One can perform a 'phi rock': where one integrates the detector signal as the sample is rotated about the axis. This sweeps the Ewald sphere through reciprocal-space, effectively accumulating all the intensity that is along the plane in reciprocal-space. The end result is that the detector image includes the full array of diffraction peaks.


Grating with material

Lithographic gratings are often used to align other materials (small molecules, block-copolymers, semiconducting polymers, etc.). When assessing scattering data arising from such systems, one must be careful to correctly interpret the 'aligned' direction.

Grating align02.png

Let's say you align the grating at phi=0, and that there is a peak in reciprocal space at fairly large |q| due to some other material (let's say the P3HT 100). Normally we would say that if you see this peak on the detector when phi=0, then we can say the material (P3HT) is aligned with phi=0. However, this isn't quite right because of the curvature of the Ewald sphere. If the peak is truly aligned with the grating, then the peak on the detector will be maximized when we slightly offset phi, by just enough to counter-act the size of the Bragg angle.

Another way to think about it is to say that if you rotate your grating, and some peak is maximized at phi=gamma degrees, then you shouldn't really say "sample has maximum alignment at gamma", but actually "sample has maximum alignment at (gamma-correction)", where you calculation the correction based on the geometry, Bragg angle, etc.

Literature Examples

GISAXS from Gratings

GISAXS/GIWAXS of materials aligned using gratings

See Also

  • CD-SAXS is frequently used to study gratings in transmission mode.
  • GTSAXS can be used to study gratings in grazing-incidence mode without refraction distortions.