Sustainable Management of Calcareous Saline-Sodic Soil in Arid Environments: The Leaching Process in the Jordan Valley

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/aess/volume-2017/1092838/figures/1092838.fig.003a.svgz" name="1092838.fig.003a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Gypsum experiment: leaching water versus EC</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/aess/volume-2017/1092838/figures/1092838.fig.003b.svgz" name="1092838.fig.003b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Fresh water experiment: leaching water versus EC</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/aess/volume-2017/1092838/figures/1092838.fig.003c.svgz" name="1092838.fig.003c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Saline water experiment: leaching water versus EC</td></tr></table>

<div>Electrical conductivity and quantities of drained water recorded during the experiment ((a) gypsum, (b) fresh water, and (c) saline water). The black line represents the leaching water quantity (m<sup>3</sup>), and the gray line is the EC.</div>

Applied and Environmental Soil Science

fig3

Figure 3

Figure 3: Sustainable Management of Calcareous Saline-Sodic Soil in Arid Environments: The Leaching Process in the Jordan Valley 