Abstract
Fiberglas soil moisture units, installed in three different ways, were calibrated both in the field and the laboratory. Laboratory calibration curves of units installed with a hydraulic inserter were most similar to field calibration curves, especially in the dry range. Replication of laboratory calibration of units installed in undisturbed soil resulted in a perfect fit of all data for each unit to its curve. A good fit of all points was obtained in the replication of field calibrations when protection tents were used to minimize hysteresis effects.

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