Abstract

Knowledge of soil moisture is needed to understand crop water use, hydrology, and microclimate. A reliable, rapidtechnique is needed, and recently an impedance soil moisture probe (Theta Probe) has been accepted by the scientificcommunity. The purposes of this study were to calibrate the probe for soils of Central Iowa through field sampling, todetermine the number of samples needed for calibration, and to determine the effect of temperature on calibration. Laboratorycalibration was conducted on Des Moines lobe soils across a range of water contents and temperatures. Including atemperature term increased the R2 from 0.85 to 0.87. Field calibration was based on Theta Probe measurements on similarsoils combined with gravimetric sampling and soil temperature determination. Although some scatter existed, the fieldcalibration was adequate for Iowa soils (R2 = 0.77). Inclusion of temperature did not significantly improve the calibrationfor the field data. To determine the appropriate number of samples needed for the field calibration, regression equations weredetermined from sample numbers ranging from 2 to 89, and the standard error was determined for each. Based on the standarderror analysis, 20 samples was an adequate number, with no further improvement for additional data points.

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