Abstract

Considering the increased interests in biochar (BC) as a soil amendment and a growing media substrate in agriculture, we evaluated the effect of BC incorporation on TDR (time-domain reflectometer)-based volumetric soil moisture content (VSMC) estimations in a loamy sand podzolic soil. Two commercial BC types (powdered—BCP, and granular—BCG) were mixed in different rates (w/w) with a podzolic soil. The dielectric constants measured using a TDR cable tester (MOHR CT 100) were converted to VSMC. Three commonly used models: (i) Topp’s equation, M-1; (ii) mixing model, M-2; and (iii) the forest soil model, M-3, were used. The accuracy of the estimated VSMC using these three models was statistically compared with measured VSMC. BCP at lower rates produced very similar results to the actual VSMC with M-1 and M-2 but deviated with increasing rates. The M-3 showed a non-linear relationship with measured VSMC. In BCG treatments, all models overestimated the VSMC. BCG rates higher than 15% (w/w) resulted in highly attenuated TDR waveforms and the signal was completely dissipated when rates higher than 50% (w/w) were used (typical application for field soils is less than 5% w/w). These results showed that predictions of the soil moisture content based on the soil dielectric constant might not be feasible for tested podzolic soils amended at high BC rates.

Highlights

  • Among the techniques used in measuring volumetric soil moisture content (VSMC), time domain reflectometry (TDR) is the most widely used method in agriculture, forestry, hydrology, and allied disciplines

  • For the studied BC rates, Kb varied over a range from 8 to 35 for the change in the measured VSMC from 25% to 65% for the BCp -amended soil, while it was from 10% to 80% and from 28% to 43% for BCG -amended soils

  • To 20% and BCG:soil mixtures up to 5% of the w/w incorporation rates used in this study for a sandy loam podzolic soil

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Summary

Introduction

Among the techniques used in measuring volumetric soil moisture content (VSMC), time domain reflectometry (TDR) is the most widely used method in agriculture, forestry, hydrology, and allied disciplines. The TDR technique has rapidly become a method of choice for field research as it offers accurate results (usually within 2% of the VSMC). Automating TDR measurements using multiplexers and data storage devices [2]. Allows continuous spatial and temporal monitoring of VSMC. TDR can be used to monitor water levels [5], the position of advancing frost levels in freezing soils [6], and the water table in the subsurface of contaminated lands [7]

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