A two-dimensional experiments were carried out to assess the capillary depression in the soil and the migration radius of the contaminant plume prior to lateral migration caused by a diesel spill, while considering various hydraulic gradients ranging from 0.714 to 3.571. A Simplified Image Analysis Method (SIAM) was utilised due to the dynamic nature of the experiment. Based on the study, deeper diesel migration occurs in larger spilled volumes because the pressure is high enough to overcome capillary forces, and it eventually depresses the capillary fringe layer. When comparing hydraulic gradients with high and low values, it can be observed that the low hydraulic gradient results in more capillary depression. As a result, pollutants would be significantly closer to the groundwater layer. The radius of the vertical contamination plume prior to the lateral migration reveals that even with a high hydraulic gradient, the maximum contamination plume size prior to the lateral migration is the same as any other hydraulic gradient. However, in the high hydraulic gradient, LNAPL migration accelerates with increasing hydraulic gradient, leading to soil and groundwater contamination at discharge points and throughout the entire groundwater pathway.