“…According to the JCPDS (N o 01-086-2344), these results indicate the presence of calcite mineral (CaCO3) with a trigonal crystalline structure and belonging to the space group R-3c (167) (Oglesbee et al, 2020). Moreover, diffraction peaks (crystalline planes) at 11.65°(020), 20.87°(−121), 36.56°(-222), 39.46° (-161), and 43.19°(240) are induced by gypsum (CaSO4.2H2O) with a monoclinic crystal system and the space group I2/c, according to the JCPDS (No 01-074-1905) (Hadjadj et al, 2020). However, the XRD patterns of the Zegoum dune sand show peaks at 2θ°: 20.88°, 26.64°, 36.55°, 39.46°, 42.47°, 50.16°, 54.87°, 59.97°, 64.1°, 67.75°, 68.16°, 68.34°, 73.32°, 75.72°, and 81.49°, according to the JCPDS (N o 00-046-1045) corresponding to the (hkl) crystalline planes (100), ( 101), ( 210), ( 102), ( 111), ( 201), ( 112), ( 003), ( 211), ( 113), ( 212), ( 203), ( 301), ( 104), (302), and (310), respectively.…”