“…At 1,000 • C, Ti 3 C 2 T X was no longer present, leaving only a high temperature stable phase of rutile. Furthermore, with the protection of inert atmospheres, such as Ar, N 2 , or He, MXenes were able to retain their original layered structure over a range of temperatures, but still produced a small amount of oxide (Li et al, 2015;Rakhi et al, 2015;Han et al, 2016;Seredych et al, 2019;Xu et al, 2019). At the same time, the inert carbon layers were kept.…”