The exchange of flow between a stream and an aquifer can be estimated solving the differential equation governing the flow using either an analytical or a numerical method. Solution of ...

The earlier practice of planning surface irrigation without much consideration of ground water status has been often resulted in waterlogging and salinity problems in the command areas after a time ...

In this report, flood frequency analysis has been carried out for Sub-Himalayan region using peak flood series data of ten small and medium size catchments varying in size from 6 sq. kms. ...

Regional dynamic ground water potential is evaluated from observed water table fluctuation and specific yield. There are different methods by which the specific yield in the zone of water ...