“…On the contrary, J. Ohgami et al"'] determined by electrostatic force microscope combined with the voltage modulation technique that the region of the TGS surface with many small round holes and islands has a negative surface charge, and the region without holes and islands has a positive one. The investigation of TGS domain structure by lateral force microscopy, including its temperature and temporal evolution, has led A. Correia et al [14] to the deduction that the similar formations can have another nature, namely to be nuclei of opposite polarity inside large domains. There is the possibility that small round formations with various shapes are ferroelectric surface domains [23,251. It is obvious from these discrepancies, that more study of islandes and holes at the polar surface characteristic for TGS crystals is required.…”