PRECISION OF NEUTRON-SCATTERING AND CAPACITANCE TYPE SOIL-WATER CONTENT GAUGES FROM FIELD CALIBRATION

Soil water content gauges based on neutron scattering (NS) have been a valuable tool for soil water investigations for some 40 yr. However, licensing, training, and safety regulations pertaining to the radioact ive source in these gauges makes their use expensive and prevents use In some situations such as unattended monitoring. A capacitance probe (CP) gauge has characteristics that would seem to make it an ideal rep lacement for NS gauges. We determined the relative precision of two br ands of NS gauges (three gauges of each) and a brand of CP gauge (four gauges) in a field calibration exercise. Both brands of NS gauges wer e calibrated vs. volumetric soil water content with coefficients of de termination (r(2)) ranging from 0.97 to 0.99 and root mean squared err ors (RMSE) <0.012 m(3) m(-3) water content. Calibrations for the CP ga uges resulted in r(2) ranging from 0.68 to 0.71 and RMSE of 0.036 m(3) m(-3) water content. Average 95% confidence intervals on predictions were three to five times higher for the CP gauges than for the NS gaug es, ranging from 0.153 to 0.161 and 0.032 to 0.052 m(3) m(-3), respect ively. Although poorly correlated with soil water content, readings we re reproducible among the four CP gauges. The poor correlation for CP gauges may be due to small-scale soil water content variations within the measurement volume of the gauge. The NS gauges provide acceptable precision but the CP gauge has poor precision and is unacceptable for routine soil water content measurements.