The twelve wells were selected to carry out the various test, duration of pumping (min), maximum draw drown (m), duration of recovery (min), residual drawdown, and aquifer type in the basaltic rock aquifer parameters of Buchakewadi watershed. The source and flow of groundwater are essential concerns in hydrological systems that concern both spatially and temporally components of groundwater discharge and water supply problems. The content and temperature of groundwater flowing through an aquifer might change depending on the aquifer environment. As a result, hydrodynamic analyses can provide valuable information about a region's subsurface geology. The present research attempts of aquifer variables such as transmissivity (T) and storativity (S) estimation are significant for groundwater resource development and evaluation. There are numerous approaches for calculating precise aquifer characteristics (i.e., hydrograph analysis, pumping test, etc.). A most frequent in situ analysis is a well-pumping test, which accurately measures the decline and rise of groundwater levels. During an aquifer pumping test, to characterize aquifer properties in an undiscovered location to forecast the rate of depletion of the groundwater table/potentiometric surface. The shallow, weathering subsurface water accessible above the Deccan traps in an unconfined state is insufficient to satisfy the ever-increasing pressure on water supplies. Maharashtra is similarly dominated by hard rocks, whose rainfall susceptibility is limited by weathering and primary porosity, as is their volume to store and convey water. Based on the hydraulic parameters and Theis method, results are optimized. Aquifer mapping and pumping test results can be more important for solving problems such as water scarcity, nonpolluting water, health issues, and source of fresh water on the earth surface. However, the characterization of aquifer parameters should be significant role in the scientific planning and engineering practices.

选择 12 口井对 Buchakewadi 流域玄武岩含水层参数中的抽水持续时间 (min)、最大抽取淹没 (m)、恢复持续时间 (min)、剩余下降和含水层类型进行了各种测试。地下水的来源和流动是水文系统的基本问题，涉及地下水排放和供水问题的空间和时间组成部分。流经含水层的地下水的含量和温度可能会因含水层环境而异。因此，水动力分析可以提供有关地区地下地质的宝贵信息。目前对透水率（ T）和蓄水率（S ）等含水层变量的研究尝试) 估算对于地下水资源开发和评价具有重要意义。计算精确含水层特征的方法有很多（即水位线分析、抽水试验等）。最常见的现场分析是井抽测试，它可以准确测量地下水位的下降和上升。在含水层抽水测试期间，表征未发现位置的含水层特性，以预测地下水位/电位表面的消耗率。德干圈闭上方的浅层风化地下水在无限制状态下无法满足不断增加的供水压力。马哈拉施特拉邦同样以坚硬的岩石为主，其降雨敏感性受到风化和原生孔隙度的限制，它们储存和输送水的体积也是如此。基于水力参数和Theis方法，对结果进行了优化。含水层测绘和抽水测试结果对于解决诸如缺水、无污染水、健康问题和地球表面淡水来源等问题可能更为重要。然而，含水层参数的表征应该在科学规划和工程实践中发挥重要作用。