“…The surfaces that have been investigated regarding the orientational organization comprise intercalation compounds (e.g., interlamellar regions of clay minerals, [3][4][5][6][7][8][9] K 4 Nb 6 O 17, 10 aluminium oxide 11 ) and flat substrates (e.g., external surfaces of clay minerals, 12,13 gold, 14 water, 15,16 glass/quartz [17][18][19][20] ). The orientation of dye molecules adsorbed on surfaces has been determined using one or a combination of the following techniques: X-ray diffraction, [5][6][7]9,10 polarized ultraviolet-visible (UV-Vis) spectroscopy, 6,10,12,17,19,20 fluorescence spectroscopy, 16 molecular modeling, 9 scanning tunneling microscopy, 14 second harmonic generation, 13,[15][16][17][18] near edge X-ray absorption fine structure spectroscopy 21 and polarized transmission infrared spectroscopy. [6][7][8] Smectite clay minerals are silicate materials that consist of ca.…”