2021
DOI: 10.1016/bs.agron.2021.02.003
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A review of time domain reflectometry (TDR) applications in porous media

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Cited by 68 publications
(34 citation statements)
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“…This translated into higher VWC and drainage for +H than for -H, particularly during the over-winter period. The difference in soil VWC between +H and -H was in part affected by differences in dieletric permittivity between liquid and solid water, which affects time domain reflectometry VWC measurements (Jones et al, 2002;He et al, 2021), and indicated higher liquid water content for +H. Contrary to our initial hypothesis, the heating regime adopted in our study did not promote colder soils during the winter, a phenomenon previously described in the literature and associated with the insulation properties of the snow pack (Brown and DeGaetano, 2011;Zhou et al, 2017;Halim and Thomas, 2018).…”
Section: Discussioncontrasting
confidence: 71%
“…This translated into higher VWC and drainage for +H than for -H, particularly during the over-winter period. The difference in soil VWC between +H and -H was in part affected by differences in dieletric permittivity between liquid and solid water, which affects time domain reflectometry VWC measurements (Jones et al, 2002;He et al, 2021), and indicated higher liquid water content for +H. Contrary to our initial hypothesis, the heating regime adopted in our study did not promote colder soils during the winter, a phenomenon previously described in the literature and associated with the insulation properties of the snow pack (Brown and DeGaetano, 2011;Zhou et al, 2017;Halim and Thomas, 2018).…”
Section: Discussioncontrasting
confidence: 71%
“…Furthermore, water retention curves can be used to translate VWC into soil matric potential for a given soil. Water retention curves are commonly referred to as the relationship between matric potential and volumetric water content for soil with given structural and hydraulic characteristics and defines a critical soil hydraulic property especially when it comes to dynamics in soil drying and rewetting (Dane & Lenhard 2005;He et al 2021). Water retention curves can be determined in the lab for a given soil following standardized procedures (e.g.…”
Section: Soil Water Availabilitymentioning
confidence: 99%
“…Using Time Domain Reflectometry (TDR) sensors is the most useful and non-destructive method used to determine the moisture content in soils and other porous means. This sensor measures the transmitted signal time from one end to the other [22,23]. However, in soils with high salt content, representativeness of the measurement can be lost, in addition to the fact that it requires a high initial investment [24].…”
Section: Introductionmentioning
confidence: 99%