In-situ evaluation of internal drainage in layered soils (Tukulu - hessd
In-situ evaluation of internal drainage in layered soils (Tukulu - hessd
In-situ evaluation of internal drainage in layered soils (Tukulu - hessd
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(a)<br />
(b)<br />
(c)<br />
Figure 5 K-θ-relationship from the (a) <strong>Tukulu</strong>, (b) Sepane and (c) Swartland soil types<br />
Fig. 5. K -θ-relationship represent<strong>in</strong>g variation <strong>in</strong> permeability dur<strong>in</strong>g the 1200 h <strong><strong>in</strong>ternal</strong><br />
<strong>dra<strong>in</strong>age</strong> period from saturation for the <strong>Tukulu</strong>, (a) Sepane (b) and Swartland (c) soil types.<br />
(a)<br />
(b)<br />
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Figure 6 θ-T relationships from the (a) <strong>Tukulu</strong>, (b) Sepane and (c) Swartland soil types<br />
Fig. 6. θ-T relationships depict<strong>in</strong>g the <strong>dra<strong>in</strong>age</strong> curve dur<strong>in</strong>g the first 200 h <strong>of</strong> <strong>dra<strong>in</strong>age</strong> from<br />
saturation for the (a) <strong>Tukulu</strong>, (b) Sepane and (c) Swartland soil types<br />
9840<br />
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