2012
DOI: 10.3390/s120709773
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Correcting the Temperature Influence on Soil Capacitance Sensors Using Diurnal Temperature and Water Content Cycles

Abstract: The influence of temperature on the dielectric permittivity of soil is the result of counteracting effect that depends on the soil's composition and mineralogy. In this paper, laboratory experiments showed that for a given water content, the soil dielectric permittivity was linearly related to the temperature, with a slope (α) that varied between samples taken in the same soil. These variations are difficult to predict and therefore, a simple and straightforward algorithm was designed to estimate α based on th… Show more

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Cited by 37 publications
(24 citation statements)
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“…Hence, the main mechanism is not related to the polarization of water molecules (or to the thermal dilation of the volume, being negligible: 0.026% °C −1 at T0=25 °C). The phenomenon has been already observed [28,29]. One explanation attributes it to the water bound to particle surface, of which dipoles have a relaxation frequency lower than that of free water dipoles [30], even lower than f of sensors (they operate here at f=20 MHz).…”
Section: Resultsmentioning
confidence: 75%
“…Hence, the main mechanism is not related to the polarization of water molecules (or to the thermal dilation of the volume, being negligible: 0.026% °C −1 at T0=25 °C). The phenomenon has been already observed [28,29]. One explanation attributes it to the water bound to particle surface, of which dipoles have a relaxation frequency lower than that of free water dipoles [30], even lower than f of sensors (they operate here at f=20 MHz).…”
Section: Resultsmentioning
confidence: 75%
“…More than 2 years of data are shown here, from sensor installation in December 2016 (DOY 341) until DOY 365 in 2018. Because ε can be affected by temperature (Chanzy, Gaudu, & Marloie, ), two additional probes were installed in dead stems to evaluate the potential effect of the temperature sensitivity of ε ( α = Δ ε /ΔT; °C −1 ) on estimates of ΔStWC. For this, α was estimated on a daily basis as the slope between ε and dead stem temperature (T STEM ; °C) recorded by the probe, and the relationship between α and mean daily ε was evaluated across the surveyed period.…”
Section: Methodsmentioning
confidence: 99%
“…This extraction of soil water extends over the entire active rooting depth. Additionally, soil water flow occurs both at night as well as during the day (Chanzy, Gaudu, & Marloie, ; Khalil, Sakai, Mizoguchi, & Miyazaki, ; Verhoef, Fernandez‐Galvez, Diaz‐Espejo, Main, & El‐Bishti, ), following water potential gradients in the soil profile. Thus, during dry weather conditions, the time series of soil water content shows a clear day‐night signal.…”
Section: Methodsmentioning
confidence: 99%