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The predicted temperature increases due to global warming and the consequent change in rainfall patterns are expected to have a substantial impact on both soils and demographics.
The sand fraction prevailed in both soils.
Both soils are of andic origin.
On both soils the aggregated surface layer always remained unsaturated.
NT significantly reduced CO2 emissions from both soils and sediments.
In both soils, the addition of SS increased Al, Cu and Fe concentrations in shoots.
However, the results showed that DAP and organic inputs increased the available P in both soils.
The isotherm trends for both soils were similar, which are concave-up.
Fine and coarse root lengths followed the same pattern as total root length in both soils.
In both soils, a decrease in pH was observed, which was independent of the treatments.
These results indicated that CR affects the RWC in both soils significantly (Table 4).
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