The flowmeter method is based on the relative flow rate
entering the well from each geologic stratum. The data recorded by the flowmeter
accurately represent the flow rate entering or leaving each stratum as long as the ratio
of the flow bypassing the probe to the flow through the recording interior is constant.
Flow rates can be analyzed directly as recorded to estimate the hydraulic conductivity
distribution, or adjusted to account for the bypass flow. Adjustments are made using flows
measured at solid sections of the pipe. However, it is essential that data collected at
the solid joints be recognized as inconsistent with data collected in the screened
segments as shown below