The liquid limit (LL) of soil is a key Atterberg limit that defines the moisture content at which soil transitions from a plastic to a liquid state. Two primary methods are used for its determination: the Casagrande method (percussion cup method) and the Cone Penetrometer method (also known as the Fall Cone test). In the Casagrande method, a soil pat in a cup is grooved, and the number of blows (typically 25) required for the groove to close over 12 mm is measured to plot against moisture content. In contrast, the Cone Penetrometer method involves dropping a standardized cone (e.g., 80 g mass, 30° angle) onto a soil sample for 5 seconds and measuring the penetration depth (typically 20 mm for LL).