Abstract

Heat dissipation sensors operate based on the temperature dependence of the transient heat conduction within the soil, which is a function of the soil characteristics and its water content. After a heat pulse with controlled energy is applied to a heater, it is possible to show that the maximum temperature rise $\Delta T_{M}$ measured in the temperature sensing element can be related to the volumetric water content of the soil $\theta _{v}$ [m3 m−3]. The design and fabrication of a low-cost soil moisture multiprobe heat pulse sensor system using conventional printed circuit boards and surface-mount devices is presented. The proposed sensor is free of the needles’ deflection problem present in conventional multiprobe sensors and is manufactured using conventional off-the-shelf electronic components. A precision low-power electronic signal conditioning circuit, using an instrumentation switched-capacitor building block, was developed and successfully used in the prototype. Due to an energy-efficient topology for the sensor and a low-power signal conditioning circuit, the average current consumption of the system (with one measurement per day) is only 3 $\mu \text{A}$ . To demonstrate the feasibility of the concept, a prototype of the sensor was tested in soils with volumetric humidity in the range from $\theta _{v} = 0.05 \,\,\rm {m^{3} \, m^{-3}}$ to $\theta _{v} = 0.41 \,\,\rm {m^{3} \, m^{-3}}$ and, with a very low heating energy pulse (3 J), showed a sensitivity, normalized by the total energy applied, $\Gamma = 211 \times \rm {10^{-3}}\,\, {^{\circ }}\rm {C} \, \rm {m^{3} \, m^{-3} \, J^{-1}}$ . Compared with a button heat pulse probe sensor which has $\Gamma = 192 \times \rm {10^{-3}}\,\, {^{\circ }}\rm {C} \, \rm {m^{3} \, m^{-3} \, J^{-1}}$ , the developed sensor shows a higher normalized sensitivity.

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