“…The ingress of seawater into cement leads to the conversion or replacement of monocarbonate with Friedel's salt, along with the removal of typical solid hydrate phases, such as C-S-H, portlandite, ettringite, etc., with a corresponding decrease in solid volume [15][16][17][18][19]. These phases are replaced with Friedel salt, Magnesium Silicate Hydrate (M-S-H), and the re-precipitation of brucite.…”