Rapid laboratory calibration of time domain reflectometry using upward infiltration. [Erratum: July/Aug 1998, v. 62 (4), p. 905.]

We propose an upward infiltration method to calibrate a time domain reflectometry (TDR) system. The method is rapid, allows the soil to remain unchanged during the experiment, and provides hundreds of data points. Three experiments were conducted using 18.7-cm-long probes in soils of three textures...

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Veröffentlicht in:Soil Science Society of America journal 1997-05, Vol.61 (3), p.707-712
Hauptverfasser: Young, M.H. (University of Arizona, Tucson, AZ.), Fleming, J.B, Wierenga, P.J, Warrick, A.W
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container_issue 3
container_start_page 707
container_title Soil Science Society of America journal
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creator Young, M.H. (University of Arizona, Tucson, AZ.)
Fleming, J.B
Wierenga, P.J
Warrick, A.W
description We propose an upward infiltration method to calibrate a time domain reflectometry (TDR) system. The method is rapid, allows the soil to remain unchanged during the experiment, and provides hundreds of data points. Three experiments were conducted using 18.7-cm-long probes in soils of three textures (nine experiments total). Calibrations also were performed by packing soil cores with soil at progressively higher water contents. The data from the two methods were fitted using regression techniques to two published models of the dielectric constant-water content relationship. The results show that the calibration curves of all three soils, fitted simultaneously to replicate experiments, were similar in shape and statistically the same. A single calibration curve, fitted simultaneously to the replicate experiments of the three soils, was compared with Topps equation and was statistically the same. The results support the conclusion that the upward infiltration method provides a fast and repeatable calibration method consistent with conventional calibration
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Calibrations also were performed by packing soil cores with soil at progressively higher water contents. The data from the two methods were fitted using regression techniques to two published models of the dielectric constant-water content relationship. The results show that the calibration curves of all three soils, fitted simultaneously to replicate experiments, were similar in shape and statistically the same. A single calibration curve, fitted simultaneously to the replicate experiments of the three soils, was compared with Topps equation and was statistically the same. The results support the conclusion that the upward infiltration method provides a fast and repeatable calibration method consistent with conventional calibration</abstract><cop>Madison, WI</cop><pub>Soil Science Society of America</pub><doi>10.2136/sssaj1997.03615995006100030001x</doi><tpages>6</tpages></addata></record>
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source Wiley Online Library Journals Frontfile Complete
subjects Agronomy. Soil science and plant productions
ANALYTICAL METHODS
Biological and medical sciences
Calibration
CONTENIDO DE AGUA EN EL SUELO
Earth sciences
Earth, ocean, space
Exact sciences and technology
EXPERIMENTACION EN LABORATORIO
EXPERIMENTATION EN LABORATOIRE
Fundamental and applied biological sciences. Psychology
INFILTRACION
INFILTRATION
LABORATORY EXPERIMENTATION
LOAM SOILS
MEASUREMENT
MEDICION
MESURE
METHODE
METHODS
METODOS
MOUVEMENT DE L'EAU DANS LE SOL
MOVIMIENTO DEL AGUA EN EL SUELO
NORMALISATION
NORMALIZACION
Physical properties
Physics, chemistry, biochemistry and biology of agricultural and forest soils
RAPID METHODS
SANDY SOILS
SILTY SOILS
Soil science
SOIL WATER CONTENT
SOIL WATER MOVEMENT
Soils
SOL LIMONEUX
SOL SABLEUX
SOL SABLOLIMONEUX
STANDARDIZING
SUELO ARENOSO
SUELO FRANCO
SUELO LIMOSO
Surficial geology
TECHNIQUE ANALYTIQUE
TECNICAS ANALITICAS
TENEUR EN EAU DU SOL
VERTICAL MOVEMENT
Water
Water and solute dynamics
title Rapid laboratory calibration of time domain reflectometry using upward infiltration. [Erratum: July/Aug 1998, v. 62 (4), p. 905.]
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