The present research concentrates on the cumulative use of GPS and GIS technologies, which are excellent resources for analyzing and monitoring divergent physico-chemical parameters in groundwater, including pH, TDS, E.C., ORP, Ca +2 , Mg +2 , NO 3 -, F-, SO 4 -2 , Cl -, and PO 4 -3 with explicit regard to Uranium. Garmin GPS is used to record the locations of the sampling points in the Godda study area. The research aims to offer a thorough understanding of the relationship between soil and water, its impact on public health and the extent to which water can be used in various ways based on its quality. Utilizing the Inverse Distance Weighted (IDW) technique, it is examined how these groundwater parameters and the Water Quality Index can be estimated spatially. Additionally, a correlation analysis of the water quality parameters is computed to estimate the local population's cancer risk living in the study area. Except for calcium and magnesium, which are present in excess concentrations throughout the study area with the highest values of 325 and 406 mg/l, respectively, at Amediha, Meherma, the results showed that the maximum concentration parameters are within limits with the standard. The main reason might be the area's predominance of al sols soil type. The radioactive element uranium is found to be in a limited number. Chemo-toxicity and radiological risk assessment of the whole area lie far below the restricted cancer risk limit, i.e. 30 ppb with the highest concentration of 14 ppb in the "Sunderpahari" region, following the results obtained. The water quality index for the area ranges from "Good" to "Very Poor." The results were favorable, but a few sites, such as 'Boarijor' and its surroundings, require additional attention to enhance groundwater quality. Given Uranium's low availability in groundwater, the region's cancer risk assessment is below average.rainfall in summer and little rainfall in winter). It has a sinuous topography with solitary peaks, valleys, and rolling uplands. Godda is situated in the Rajmahal Hills' western region (Somani A., 2009). In 2022, there will be 1,466,303 people living in the district as a whole (Government of India census).
Geology and Soil typeThe geological formation of the district is very diverse, and has a convoluted tectonic systems. Three major categories have been used to group the geological formations a) the southern and central parts comprising the gneiss, b) the eastern and south-eastern parts with the Rajmahal traps and c) northern and alluvial cover with the Gondwana. The area is home to a wide range of mineral deposits. The southern portion of Poreyahat has deposits of dolerite, and the central region has deposits of quartzite and quartz schist. Basaltic traps and sedimentary beds can be found in the area geologically. The district's southern region appears to contain granite-gneisses of the Archean age, while the northern and central regions are covered in Barakar rocks made up of sandstones, shales, coal, and feldspathic rocks. These are intrusive basic...