Anisotropic Slope Distribution and Bidirectional Reflectance of a Rough Silicon Surface

2004 ◽  
Vol 126 (6) ◽  
pp. 985-993 ◽  
Author(s):  
Q. Z. Zhu ◽  
Z. M. Zhang

Both one-dimensional (1D) and two-dimensional (2D) slope distributions were obtained from the surface topographic data, measured using an atomic force microscope for a rough silicon surface. The resulted slope distributions deviate significantly from the Gaussian distribution, with noticeable side peaks. The bidirectional reflectance distribution function (BRDF) of the same surface, measured with a laser scatterometer at 635 nm and 785 nm, exhibits subsidiary peaks. The measured slope distributions are implanted into a geometric optics model to predict the in-plane BRDF for different azimuthal angles. The 1D slope distribution has some success in predicting the BRDF at limited azimuthal angles, but is not applicable to other cases. On the other hand, the BRDF predicted using the 2D slope distribution matches well with the experimental results for any azimuthal angles. The method developed here may also help predict the BRDF for other rough surfaces with microstructures.

Author(s):  
Q. Z. Zhu ◽  
Z. M. Zhang

Surface topography of the rough side of a silicon wafer is characterized using an atomic force microscope (AFM). The slope distribution calculated from the measured surface profiles deviates significantly from the Gaussian distribution. The experimentally obtained slope distribution is incorporated into a geometric-optics model to predict the bidirectional reflectance distribution function (BRDF) of the rough surface. Comparison has been made between the predicted BRDF and that measured with a recently built bidirectional scatterometer, at 635 nm and 785 nm for different incoming angles. The trends agree well between the predicted and measured BRDFs, especially for the parallel-polarized incidence (p-polarization), although relatively large discrepancies exist near the specular peak and at large reflection angles. This work offers a plausible explanation of the second non-specular peak in the observed BRDF as associated with the subsidiary maximum in the slope distribution. Anisotropic features have been found both in the calculated slope distributions and the measured BRDFs.


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