Abstract
Electrical imaging studies of laboratory- and small-scale plant root zones are gaining increasing attention. However, for essential moisture–conductivity calibrations on numerous substrate columns with variability in dry density, the use of one conventional strategy is relatively laborious or complicated. Thus, in this work, a relatively convenient calibration method is presented, and the objective is to identify its feasibility and potential to assess the effects of factors (e.g., volumetric water content (VWC), and dry density) on conductivity and establish necessary moisture–conductivity curves for porous materials (e.g., soils and substrates). In the method, with a specially designed fixture, variable VWCs, dry densities and related complex conductivities of the samples can be easily acquired through static compaction. The results show that the in-phase conductivity (or magnitude of conductivity) increases with the increasing VWC or dry density, primarily owing to the increase in the dominant pore water connectivity. Moreover, the effect of dry density on conductivity is relatively smaller than that of VWC. Thus, for the substrates at dry densities with certain variability, good power law relations (R2 ≥ 0.99) between in-phase conductivity (or magnitude of conductivity) and VWC at different frequencies can be established. Overall, the proposed approach is practical, promising, and relatively time- and labor-saving.
Highlights
Soil conductivity can be used to estimate the physical, chemical and biological properties of interest, and its measurement and monitoring play a significant role for numerous application fields, for soil, water and fertilizer management in agriculture [1,2]
In a given ex situ laboratory calibration, soil samples obtained from the field are controlled to different volumetric water contents (VWCs), and they are individually repacked into a specific test box to measure their bulk conductivities [3,4,5]
The results show that the increase in VWC can increase the in-phase conductivity, primarily because of the improvement in the dominant pore water connectivity
Summary
Soil conductivity can be used to estimate the physical, chemical and biological properties of interest (e.g., moisture, texture, and salinity), and its measurement and monitoring play a significant role for numerous application fields, for soil, water and fertilizer management in agriculture [1,2]. In a given ex situ laboratory calibration, soil samples obtained from the field are controlled to different volumetric water contents (VWCs), and they are individually repacked into a specific test box to measure their bulk conductivities [3,4,5]. It is usually necessary to perform laboratory or field calibrations at different horizontal locations and depths for soils with significant heterogeneity. Factors such as changes in the pore water conductivity and the presence of roots could affect the calibration relation [1]
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