Well or Borehole Storage Sample Clauses

Well or Borehole Storage. During a pumping test, a common assumption is that the pumping rate equals the discharge from the aquifer. This assumption is acceptable only as long as a small percentage of discharge originates from within the well or borehole. In any large diameter well, borehole storage is a potential concern. If borehole storage dominates the response of a single-well pumping test, the time/drawdown data will appear as a straight line on a log-log plot with a slope of one. During a pumping test, the effects of borehole storage diminish with time and may be ignored at late times. Until storage effects dissipate, the drawdown will be less than if storage effects were not present. Two problems exist if flowmeter measurements are made before borehole storage dissipates. One problem is that the total flow into the well from the aquifer is increasing with time. Hence, the flow distribution to the well will be changing with time. Another problem is that calculated transmissivity values will be too high unless the drawdown values are corrected for wellbore storage. When performing a flowmeter test of this design, borehole storage should be considered in the analyses, especially in low permeability aquifers or in boreholes of large diameters.
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