有机改进剂对土壤水力特性的影响

H. Bayabil, Fitsum T. Teshome, Niguss Solomon Hailegnaw, Jian Zhang, Yuncong C. Li
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引用次数: 0

摘要

摘要:本文研究了有机土壤改良剂百有机石对土壤养分、植物生长和产量的影响。然而,其对土壤水力特性的影响尚不清楚。因此,本研究旨在探讨钙镁土对土壤蒸发、保湿、导电性和电导率的影响。采用两种毫硅土施用量(15%和30% v/v)和不加盐的对照土进行柱状试验。结果表明,与对照相比,milorganite降低了蒸发速率和蒸发过程第一阶段的长度。此外,milorganite增加了土壤在饱和和永久萎蔫点的保水能力,同时降低了土壤的导水性。此外,米尔有机石增加了土壤的导电性。总体而言,milorganite增加了土壤保水能力;然而,由于土壤盐度的增加,土壤中的水分可能不容易为植物提供。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Changes in soil hydraulic properties due to organic amendment
Abstract The effect of milorganite, a commercially available organic soil amendment, on soil nutrients, plant growth, and yield has been investigated. However, its effect on soil hydraulic properties remains less understood. Therefore, this study aimed to investigate the effect of milorganite amendment on soil evaporation, moisture retention, hydraulic conductivity, and electrical conductivity of a Krome soil. A column experiment was conducted with two milorganite application rates (15 and 30% v/v) and a non-amended control soil. The results revealed that milorganite reduced evaporation rates and the length of Stage I of the evaporation process compared with the control. Moreover, milorganite increased moisture retention at saturation and permanent wilting point while decreasing soil hydraulic conductivity. In addition, milorganite increased soil electrical conductivity. Overall, milorganite resulted in increased soil moisture retention; however, moisture in the soil may not be readily available for plants due to increased soil salinity.
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