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Practical Aspects of Salinity Effect on TDR-Measured Water Content

A Field Study

^a Dep of Physical Chemistry of the Soil, Soil and Water Inst., ARO, Volcani Center, Bet Dagan, 50-250, Israel
^b Lab. for Pest Management Research, Agricultural Engineering Institute, ARO, Bet Dagan, 50-250, Israel
^c Hevel Maon Enterprises, M. P. Hanegev, Israel

View larger version (25K): [in a new window]   Fig. 1 EC of soil solution from 1:1 aqueous extracts corrected for water content at time of sampling, as a function of depth, at beginning (Day 1), middle (Day 75), and end (Day 145) of growing season (Nirim site)

View larger version (53K): [in a new window]   Fig. 2 A comparison of water content (m3 m-3) measured by TDR () and a neutron probe () for two depths in six plots as a function of time, in Zeelim site. SD of error is presented by the dotted (for TDR) and dashed (for the neutron probe) lines

View larger version (48K): [in a new window]   Fig. 3 A comparison of water content (m3 m-3) measured by TDR () and a neutron probe () for two depths in six plots as a function of time, in Nirim site. SD of error is presented by the dotted (for TDR) and dashed (for the neutron probe) lines