AlPO4-5 is a zeolite (structure type: AFI) with 6-and 12-membered rings, and 12-membered ring channels have a relatively large pore size of 7.3 and can take in a variety of molecules (Fig. 1).Although there have been many studies on the adsorption properties of AlPO4-5 as a molecular sieve, surprisingly, its crystal structure remains unclear.For example, the most accepted space group of AlPO4-5 is P6cc with unit cell parameters of a ~ 13.7 and c ~ 8.5 (e.g., [1]), but several space groups with lower symmetry have also been proposed (e.g., [2,3]).Furthermore, although the existence of satellite reflections suggesting the existence of modulated structures has recently been reported under high pressure [4], a detailed analysis of these satellite reflections has not been performed due to the weakness of the observed satellite reflections.Here we revisit to perform x-ray diffraction using a relatively large single crystal of AlPO4-5.Single crystal x-ray diffraction experiments for calcined AlPO4-5 single crystals were conducted using a laboratory-based x-ray diffractometer (Rigaku/Synergy custom) with a Mo rotating anode (Rigaku/MicroMax-007), a confocal x-ray mirror (Rigaku/VariMax-MoHF), and a hybrid pixel semiconductor detector (Rigaku/Hypix-6000HE).The diffraction images were obtained for single crystals of about 100 m in diameter, and we first found the satellite peaks of q = 0.3725(3) c* up to 2 nd order even at ambient conditions.The observed q value is similar to the previously reported value under high pressure [4], and its noninteger value indicates that the AlPO4-5 has an incommensurate structure.We also tested the thermal stability of the incommensurate structure by single crystal x-ray diffraction and Raman spectroscopy using a purpose-built high-temperature chamber under vacuum.The detailed analysis of the incommensurate structure and its thermal stability is going to be discussed.Figure 1.Crystal structure of AlPO4-5 along c-axis (left) and a 12-membered channel (right).