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Watch your significant figures! Example 2. A confined aquifer 32.0 m thick has two monitoring wells spaced 420.0 m apart along the direction of groundwater flow. The difference in water level in the wells is 3.5 m (the difference in piezometric head). The hydraulic conductivity is 22.0 m/day. Estimate the rate of flow per meter of distance perpendicular to the flow (i.e., Q in m/day per meter of aquifer width). 420.0 m 3.5 m Flow 32.0 m Confined aquifer 22.0 M /d ay

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