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dc.contributor.authorVisconti, Fernando
dc.contributor.authorMartínez, Delfina
dc.contributor.authorMolina, María J.
dc.contributor.authorIngelmo, Florencio
dc.contributor.authorDe-Paz, José M.
dc.date.accessioned2017-06-01T10:10:53Z
dc.date.available2017-06-01T10:10:53Z
dc.date.issued2014
dc.identifier.citationVisconti, F., Martinez, Delfina, J. Molina, M., Ingelmo, Florencio, Paz, J. Miguel de (2014). A combined equation to estimate the soil pore-water electrical conductivity: calibration with the WET and 5TE sensors. Soil Research, 52(5), 419-430.
dc.identifier.issn1838-675X
dc.identifier.urihttp://hdl.handle.net/20.500.11939/4742
dc.description.abstractAffordable, commercial dielectric sensors of the frequency domain reflectometry (FDR) and capacitance–conductance (CC) types estimate the dielectric permittivity (εb) and electrical conductivity (σb) of bulk soil. In this work, an equation was obtained to estimate the pore-water electrical conductivity (σp), which is closely related to the soil salinity in contact with plant roots, from εb and σb data, by combining the simplified dielectric mixing (SDM) model that relates εb to the soil volumetric water content (θ), with the Rhoades equation that relates θ and σb to σp. This equation was calibrated with measurements of εb and σb obtained with the Delta-T WET (FDR) and the Decagon 5TE (CC) sensors, in 20 pots filled with a clay loam soil and arranged as combinations of four levels of soil moisture with five levels of soil salinity. The calibrations were performed against reference θ and σp values. The σp was calculated with the chemical equilibrium model SALSOLCHEMEC and used as a more reliable reference than the electrical conductivity of the soil wetting water. For both sensors, the SDM model on the one hand, and the Rhoades equation on the other, provided the most accurate estimations using the least number of parameters regarding their respective alternatives, i.e. the third-order polynomial and the Hilhorst equation. The combined equation for estimation of σp subsequently provided root mean square deviations of 3.1 (WET) and 4.1 (5TE) dS m–1, which decreased to 1.5 and 2.6 dS m–1 for θ >0.22 m3 m–3, and σb <3 (WET) and 3.7 (5TE) dS m–1. A new combined equation has been proposed for reliable estimations of σp with these sensors in clayey soils for θ >0.22 m3 m–3 and σb <3.7 dS m–1.
dc.language.isoen
dc.titleA combined equation to estimate the soil pore-water electrical conductivity: calibration with the WET and 5TE sensorsen
dc.typearticle
dc.authorAddressInstituto Valenciano de Investigaciones Agrarias (IVIA), Carretera CV-315, Km. 10’7, 46113 Moncada (Valencia), Españaes
dc.date.issuedFreeForm2014
dc.entidadIVIACentro para el Desarrollo de la Agricultura Sostenible
dc.identifier.doi10.1071/SR13331
dc.journal.issueNumber5
dc.journal.titleSoil Research
dc.journal.volumeNumber52
dc.page.final430
dc.page.initial419
dc.rights.accessRightsopenAccess
dc.source.typeImpreso


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