It enables us to monitor streams and streams in tests, measure storage capacity, and plan appropriate drainage systems. This means you can get the most out of the location of the wells and assess whether your water resources are sufficient to support your plans. Pumping tests allow us to gather information about the local permeability of an aquifer.

Research tests provide information on soil porosity and soil fluid absorption. Slug tests quickly predict the characteristics of the area around a well.

The pump test is performed to determine the hydrogeological parameters such as conductivity, hydraulic conductivity, storage coefficient of the geological unit where the well is drilled. Pump test is done in 4 stages. These stages are well development, cascade pump testing, constant flow draft and back up. The duration of the constant flow draft test differs according to the response of the well, and this time varies between 24 and 196 hours as standard. Longer duration of the pump test results in a wider view of the cone of drop, which means a larger radius of action. Like this; The existence of geological (broken-capped-fault etc.) structures in the vicinity of the well to be produced is determined.