A thermo-TDR probe has been developed for measuring thermal properties using a dual-probe heat-pulse technique of various textured soil (sand, loamy sand, and clay loam) at different soil moisture conditions. The thermo-TDR probe containing three parallel stainless steel rods in which every individual rod was 0.045m in length, 0.0025m in outer diameter, and 0.01m in rod-to-rod spacing. Temperature change as a function of time differed with the position difference of thermocouple located in the rod and handle part of thermo-TDR probe. It was observed that maximum temperature at a specific time was also varied according to the position of thermocouple in the rod (at the boundary between handle part and rod (z=0), at the center rod (z=
L/2), and at the head of rod (z=
L)). A weighted nonlinear regression method adopted for identifying thermal diffusivity κ and volumetric heat capacity ρ
c. Thermal conductivity λ was calculated from the relationship between κ and ρ
c data. In sand soil, maximum difference in ic at different sensor position was about 2.2×10
-7 m2· s
-1. Maximum difference in pc at different sensor position was about 0.6MJ·m
-3·K
1 at low water content (θ<0.07m
3·m
-3), and the difference tented to narrower while A>0.07m
3·m
-3. Difference in λ was about 0.9, 0.6, and 0.3W·m
-1·K
-1 for sandy, loamy sand, and clay loam soil, respectively. It has been suggested that the position of thermocouple located is important for measuring the exact thermal properties of any soil.
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