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Mapping variability of soil water content and flux across 1–1000 m scales using the A ctively H eated F iber O ptic method
Author(s) -
Sayde Chadi,
Buelga Javier Benitez,
RodriguezSinobas Leonor,
El Khoury Laureine,
English Marshall,
van de Giesen Nick,
Selker John S.
Publication year - 2014
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1002/2013wr014983
Subject(s) - water content , calibration , transect , environmental science , flux (metallurgy) , soil science , soil water , materials science , hydrology (agriculture) , remote sensing , geotechnical engineering , geology , physics , oceanography , quantum mechanics , metallurgy
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.