Articles | Volume 12, issue 1
https://doi.org/10.5194/gi-12-45-2023
https://doi.org/10.5194/gi-12-45-2023
Research article
 | 
30 Jan 2023
Research article |  | 30 Jan 2023

Calculation of soil water content using dielectric-permittivity-based sensors – benefits of soil-specific calibration

Bartosz M. Zawilski, Franck Granouillac, Nicole Claverie, Baptiste Lemaire, Aurore Brut, and Tiphaine Tallec

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on gi-2022-8', Anonymous Referee #1, 20 Jul 2022
  • RC2: 'Comment on gi-2022-8', Steven Evett, 05 Aug 2022
  • AC1: 'Comment on gi-2022-8', Bartosz Zawilski, 05 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Bartosz Zawilski on behalf of the Authors (05 Oct 2022)  Author's response 
ED: Referee Nomination & Report Request started (19 Oct 2022) by Ralf Srama
RR by Anonymous Reviewer #1 (29 Nov 2022)
EF by Polina Shvedko (16 Jan 2023)  Manuscript   Author's tracked changes 
ED: Publish as is (16 Jan 2023) by Ralf Srama
AR by Bartosz Zawilski on behalf of the Authors (17 Jan 2023)  Author's response   Manuscript 
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Short summary
In most cases, the soil water content (SWC) measurement is carried out using commercially available dielectric-permittivity-based probes such as time domain reflectometers or frequency domain reflectometers (FDR). However, these probes use transfer functions which may be inadequate in the soil concerned. Raw SWC measurement in clayey soil shows an important relative error. A simple protocol is presented, allowing for the recovery of an acceptable accuracy of the FDR SWC measurements.