Hydraulic and thermal regimes are coupled in surface soil. Accurate measurement of soil volumetric water content (θ) and thermal properties will improve our understanding of the hydraulic and thermal regimes. A thermo‐time domain reflectometry (TDR) probe was developed to simultaneously measure θ, bulk electrical conductivity (σ), thermal conductivity (λ), heat capacity (ρ c ), and thermal diffusivity (α). Time domain reflectometry was used to measure θ and σ, and the dual‐probe heat pulse (DPHP) method was used to determine λ, ρ c , and α. Laboratory tests on two soils showed that the probe determined θ accurately and the measured σ values of saturated soil correlated well with values determined by a four‐electrode probe. Measurements in agar‐immobilized water produced values of λ and ρ c that closely corresponded with standard values of these properties for water, an indication of the sensor's functionality in other media. Soil thermal properties as a function of θ also are presented. The results of these laboratory tests suggest that the thermo‐TDR probe can be a valuable tool for simultaneously monitoring θ, σ, and soil thermal properties.
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Ren et al. (1999) studied this question.
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