| Abstract: | A statistical technique which offers considerable promise in ground water studies is the fitting of polynomial trend-surfaces to ground water data and studying the variations in the surfaces and the residuals from these surfaces over a period of time. The application of trend-surface analysis to ground water study is based on the premise that the piezometric surface or water table can be approximated by a mathematically computed polynomial surface of the water levels of the wells in the aquifer. The evaluation of trend surface analysis application in ground water investigations was made up essentially of two considerations; a study of the relationship existing between the trend surfaces and the actual ground water surface and a study of the potential use of the residuals from the trend-surfaces to assist in the location of favorable sites for future development of ground water resources. The conclusions on aquifer behavior drawn from the trend surface analysis were compared with conclusions drawn from a concurrent survey of ground water conditions carried out independently of this investigation. This comparison provided the basis for the critical examination of the application of trend-surface analysis in ground water investigations. |
