Apparent electrical conductivity (EC_a) as a surrogate for neutron probe counts to measure soil moisture content in heavy clay soils (Vertosols).

摘要

Site-specific measurements of the apparent electrical conductivity (EC_a) of soil using the EM38 were correlated with near-simultaneous neutron probe readings over periods of moisture extraction by an irrigated cotton crop. Thirty sites were monitored from three EC_a zones within a 96-ha field of grey Vertosol soil 30 km west of Moree, New South Wales, Australia. This study differs from previous approaches by reporting the effect on EC_a of a wetting front (irrigation) reaching a single EC_a measurement point in a field and by using polyethylene neutron probe access tubes so that the EM38 could be operated directly over the same site measured by a neutron probe. We report strong correlations (r=0.94) between neutron probe counts (CRR) averaged to a depth of 40 or 60 cm and EC_a from an EM38 held in the vertical mode 20 cm above the soil surface. All combinations of EM sensor height (0-1.2 m) to neutron probe measurement depth (0.2-1.4 m) returned correlations >0.85. The relationship between CCR and EC_a was linear for the purposes of estimating water content over a range of background EC_a levels. More critical modelling suggested a slight curve (logarithmic model) fitted best. The range of surface-surveyed EC_a from the start of irrigation (refill point) to fully irrigated (full point) was ~27 mS m-1 for this Vertosol, where surface EC_a readings typically ranged from 50 to 200 mS m-1. We suggest that the calibration of EC_a to CRR might be effected by a two-point measurement of the soil, namely at both upper (field capacity) and lower (wilting point) EC_a values, and a site-specific calibration template generated by extending these point measures to whole-field surveys.