How can the curvature observed at the beginning of an XRD pattern, typically in the low-angle region, be corrected without affecting the actual peak positions or intensities? Can baseline correction tools be effectively used to flatten this drift and improve the clarity of the pattern while preserving the scientific accuracy of the data?
After applying baseline correction to the XRD pattern, some negative intensity values appeared, particularly in regions close to the background or where no clear peaks were present. Although the visual appearance of the plot improved, these negative values do not reflect physical reality