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Mapping variability of soil water content and flux across 1-1000 m scales using the Actively Heated Fiber Optic method

ScholarsArchive at Oregon State University

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Title Mapping variability of soil water content and flux across 1-1000 m scales using the Actively Heated Fiber Optic method
Names Sayde, Chadi (creator)
Benitez Buelga, Javier (creator)
Rodriguez-Sinobas, Leonor (creator)
El Khoury, Laureine (creator)
English, Marshall (creator)
van de Giesen, Nick (creator)
Selker, John S. (creator)
Date Issued 2014-09 (iso8601)
Note This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical Union and can be found at: http://agupubs.onlinelibrary.wiley.com/agu/journal/10.1002/%28ISSN%291944-7973/.
Abstract The Actively Heated Fiber Optic (AHFO) method is shown to be capable of measuring soil water
content several times per hour at 0.25 m spacing along cables of multiple kilometers in length. AHFO is
based on distributed temperature sensing (DTS) observation of the heating and cooling of a buried fiber-optic
cable resulting from an electrical impulse of energy delivered from the steel cable jacket. The results
presented were collected from 750 m of cable buried in three 240 m colocated transects at 30, 60, and
90 cm depths in an agricultural field under center pivot irrigation. The calibration curve relating soil water
content to the thermal response of the soil to a heat pulse of 10 W m⁻¹ for 1 min duration was developed
in the lab. This calibration was found applicable to the 30 and 60 cm depth cables, while the 90 cm depth
cable illustrated the challenges presented by soil heterogeneity for this technique. This method was used to
map with high resolution the variability of soil water content and fluxes induced by the nonuniformity of
water application at the surface.
Genre Article
Topic Soil moisture
Identifier Sayde, C., Buelga, J. B., Rodriguez‐Sinobas, L., El Khoury, L., English, M., van de Giesen, N., & Selker, J. S. (2014). Mapping variability of soil water content and flux across 1–1000 m scales using the actively heated fiber optic method. Water Resources Research, 50(9), 7302-7317. doi:10.1002/2013WR014983

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