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首页> 外文期刊>日本砂丘学会誌 >Possibility of self-mulching material of Tottori sand dune soil to reduce soil evaporation
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Possibility of self-mulching material of Tottori sand dune soil to reduce soil evaporation

机译:鸟取沙丘土壤自覆盖材料减少土壤蒸发的可能性

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In this study the possibility of the quick development of a dry layer and quick cover of the Tottori sand dune soil was evaluated to identify its suitability as a self-mulching material to reduce soil evaporation. The effect of a dry surface layer onsoil evaporation reduction was also evaluated. Water was applied to the field capacity of the sand soil and that was naturally dried. The temporal water content profile below the surface showed that the sand soil in the top layer dried in 3 to 5 days after water application and formed a dry layer near the surface that covered the lower wet layer. The thickness of the dry layer was about 4 cm in our experiment conducted in May 2008. It was clear that the sand soil had a self-mulching effect. In order toevaluate the effect of the dry layer on reducing soil evaporation, soil coluiim experiments were carried out for both controlled and uncontrolled conditions. Sand soil columns were saturated and gravitational water was drained. Then, the sand soil columns were covered with a 2 cm and 5 cm thickness of dry sand soil. Evaporation reductions were observed at both thicknesses. The 5 cm thickness was more effective (than the 2 cm), with a reduction of more than 72 % compared to no cover.
机译:在这项研究中,对鸟取沙丘土壤的干燥层和快速覆盖的快速发展的可能性进行了评估,以确定其是否适合作为自覆盖材料以减少土壤蒸发。还评估了干燥表面层对减少土壤蒸发的影响。将水施加到沙土的田间容量上,然后自然干燥。在表层以下的时间水分含量分布图表明,表层的沙土在加水后的3至5天内干燥,并在覆盖下层湿层的表层附近形成了一层干层。在我们于2008年5月进行的实验中,干燥层的厚度约为4厘米。显然,沙土具有自覆盖作用。为了评估干燥层对减少土壤蒸发的影响,针对受控和非受控条件进行了土壤对比实验。沙土柱已饱和,重力水被排干。然后,用2 cm和5 cm厚的干沙土覆盖沙土柱。在两种厚度下均观察到蒸发减少。 5厘米的厚度(比2厘米)更有效(与没有覆盖物相比,减少了72%以上)。

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