T The jakarta region is composed of quaternary rocks that have undergone weathering, resulting in varying physical soil properties. these variations in physical properties influence the soil\\\'s capacity for water absorption. this research was conducted in the grogol petamburan area, a densely populated district, with a study area covering 4 x 4,5 km. the objective of this study is to determine the infiltration rate and its relationship with the physical characteristics of the soil in the research area. this study utilizes primary data, including infiltration rate measurements using a double ring infiltrometer, groundwater levels, soil sampling, and admt (acoustic doppler magnetic tool) data acquisition. subsequently, laboratory testing was performed to identify physical soil properties, specifically grain size, water content, porosity, and soil permeability. the results of the study indicate that the area consists of three infiltration rate zones: moderate (52 mm/hour), moderately fast (80 – 120 mm/hour), and fast (132 – 240 mm/hour). the water content and porosity values in the study area are relatively uniform, ranging from 14,03 – 65,8% and 33,98 – 52,05% respectively, classified as moderate to high. the permeability of the research area is divided into three zones: moderately fast (6,7 – 10,24 cm/hour), fast (19,63 – 22,45 cm/hour), and very fast (26,68 – 40,95 cm/hour). furthermore, from the admt data, the resistivity values were identified, revealing that the study area consists of sandstone with grain sizes ranging from coarse to fine. the depths of the unconfined and shallow aquifers in the research area were also determined. through data integration, the relationship between the infiltration rate, groundwater level, and physical soil properties in the study area was established.