A well in a water-table aquifer was pumped at a rate of 873 m 3 /day. Drawdown was measured in a fully penetrating observation well located 90 m away. The following data were obtained (Kruseman &...

A well in a water-table aquifer was pumped at a rate of 873 m³
/day. Drawdown was measured in a fully penetrating observation well located 90 m away. The following data were obtained (Kruseman & deRitter 1991):

Find the transmissivity, storativity, and specific yield of the aquifer.