Infrared analyses of clay minerals samples are usually performed by transmission techniques. While transmission measurements are easy and inexpensive, the sample preparation plays a primordial role in the quality of the data. Alternatively, attenuated total reflection (ATR) provides a powerful and often simpler analysis method. However, the ATR spectra reveal strong differences when compared to transmission spectra leading sometimes to confusion in the interpretations. Indeed, optical effects play a prominent role in the ATR spectral profile and their identification is mandatory for obtaining quantitative information regarding molecular/particle orientation or film thickness. Here, exact spectral simulations of montmorillonite films are performed by making use of the optical theory, following the determination of the anisotropic optical constants from the experimental reflectance spectra by Kramers-Kronig transformation. This methodology can advantageously be used (i) to choose the appropriate optical conditions for advanced and reliable characterization of clay minerals, (ii) to extract quantitative information such as the estimation of the film thickness, and (iii) to discriminate optical phenomena (optical interferences) from chemical/structural features of the sample.