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This article in SSSAJ

  1. Vol. 66 No. 3, p. 735-743
     
    Received: Jan 19, 2001
    Published: May, 2002


    * Corresponding author(s): vwnad@agri.gov.il
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doi:10.2136/sssaj2002.7350

Horizontal and Vertical TDR Measurements of Soil Water Content and Electrical Conductivity

  1. Arie Nadler *a,
  2. S. R. Greenb,
  3. I. Vogelerb and
  4. B. E. Clothierb
  1. a Soil and Water Institute, Agricultural Research Organization, Ministry of Agriculture, State of Israel, POB 6 Bet Dagan, Israel, 50250
    b Environmental group, HortResearch, Private bag 11-030 Palmerston North, New Zealand

Abstract

When time domain reflectometry (TDR) is used to measure soil water content (θ) and salinity, the probes can be installed either horizontally or vertically. We tested the common convention that θ values averaged from horizontal probes will be equal to a vertical direct measurement. In a laboratory experiment, a sandy loam soil, packed uniformly (0.02-m layers to 0.18-m depth) into a box, was gradually wetted to saturation by CaCl2 solutions of 0, 0.5, 1.1, 2.1, 3.1, 4.5, 5.9, and 8.4 dS m−1 Horizontal and vertical TDR probes for measuring θ and electrical conductivity of the bulk soil (σa) were installed during soil packing. A comparison between θ values averaged from three horizontal probes and from two vertical ones showed deviations of 0.02 (L L−1). A simple water redistribution model was used to attribute this deviation to the process of averaging the horizontal results. The best practical attainable reproducibility, under our experimental conditions, were close to the theoretical limit 0.005 (L L−1) but the average experimental reproducibility of θ was 0.01 to 0.02 (L L−1). Width of the soil layer affecting the moisture measurement was reconfirmed to be close to 30 mm. The resistors-in-series model was found to be a good approximation to describe the soil profile σa from separately measured horizontal σa Final values of the electrical conductivity of the soil solution (σw) after sufficient leaching were in good agreement with σw values calculated by an empirical protocol that uses σa, θ, and a soil texture property.

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Copyright © 2002. Soil Science SocietyPublished in Soil Sci. Soc. Am. J.66:735–743.

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