2020
DOI: 10.1029/2019wr025204
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High‐Resolution Measurement of Soil Thermal Properties and Moisture Content Using a Novel Heated Fiber Optics Approach

Abstract: Hydrological parameters are scale dependent. Efficient monitoring techniques capable of measuring hydrological parameters, such as soil moisture content (θ), over a wide range of spatial scales are essential for understanding the complexity of water and energy movement across the landscape. Techniques to measure θ over spatial scales in the range from centimeters to thousands of meters, however, are sorely lacking. Recent improvements in the distributed temperature sensing (DTS) technology supported the develo… Show more

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Cited by 14 publications
(28 citation statements)
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“…(2014) and Shehata et al. (2020). It consisted of a 1.2 mm stainless steel tube filled with a gel that surrounds two fiber‐optics, covered by a polyvinylidene difluoride jacket (custom made‐AFL Global).…”
Section: Methodsmentioning
confidence: 96%
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“…(2014) and Shehata et al. (2020). It consisted of a 1.2 mm stainless steel tube filled with a gel that surrounds two fiber‐optics, covered by a polyvinylidene difluoride jacket (custom made‐AFL Global).…”
Section: Methodsmentioning
confidence: 96%
“…The principle of superposition (Shehata et al., 2020) was applied to account for the limited duration of the applied heat pulse: T(t)={leftTr(t)0<tt0leftTr(t)Trtt0t>t0 $T(t)=\left\{\begin{array}{lc}{T}_{r}(t)\quad \hfill & \hfill 0< t\le {t}_{0}\hfill \\ {T}_{r}(t)-{T}_{r}\left(t-{t}_{0}\right)\hfill & \hfill t > {t}_{0}\hfill \end{array}\right.$ where t is the time in seconds measured from the heat‐pulse start and t 0 is the heat pulse duration ( t 0 = 120 s). The final resulting model was fitted to the sensed temperature increase during the first 300 s from the heat pulse start.…”
Section: Methodsmentioning
confidence: 99%
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