The internal structural arrangement of water is further explored by computing the orientational order parameter (𝑞 𝑡𝑒𝑡 ), the value of which varies between 0 and 1. The value 0 signifies complete random orientation, while the value 1 confirms the ice-like tetrahedral structure. In our work, we witness a gradual deviation from tetrahedrality as we introduce reline in water and increases reline concentration (Fig ).