Investigation of different organic fertilizers application on the soil water holding capacity

Desert Pub Date : 2020-12-01 DOI:10.22059/JDESERT.2020.79254
M. Mirzabaiki, N. Ebrahimipak, E. Pazira, S. Samavat
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引用次数: 1

Abstract

This study was conducted to investigate the impacts of organic fertilizers on soil water holding capacity in four different suctions (0, 0.05, 0.33 and 15 bar) and their impacts on water retention curve in three different soil textures in five governing climates of Iran, which were cultivated under wheat and maize for two consecutive years. Furthermore, the role of organic materials in aggregation process was surveyed. The influence of organic materials on soil water holding capacity was evaluated in five treatments, including 10000, 20000 kg/ha of animal manures; 10000, 20000 kg/ha of compost, and control treatment in factorial and completely randomized statistical design. The results revealed that the addition of materials resulted into an increase in the mean weight diameter of soils aggregates with more concentration on 250-500 and 500-1000µ diameter. Additionally, the improvement of soil aggregation was more in sandy loam soil and less in clay loam soil. Interestingly, the role of organic materials in increasing soil water holding capacity in different plants and consecutive years was not significant.  By adding organic materials in field capacity and permanent wilting point, soil volumetric moisture increased far better than other studied soil moisture points. Sandy loam texture and semi-arid climates indicated the greatest variability to the additional organic materials. In conclusion, compost fertilizer in arid and semi-arid climates with sandy loam texture had the most influence on soil water holding capacity, particularly in FC and PWP moisture points
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不同有机肥施用对土壤持水能力的影响
本研究旨在研究连续两年在小麦和玉米下种植的有机肥对伊朗五种控制气候下四种不同吸力(0、0.05、0.33和15bar)土壤持水能力的影响及其对三种不同土壤质地持水曲线的影响。此外,还考察了有机材料在聚合过程中的作用。评价了有机物质对土壤持水能力的影响,包括10000、20000公斤/公顷的动物粪便;10000、20000公斤/公顷堆肥和对照处理,采用析因和完全随机统计设计。结果表明,随着250-500和500-1000µ直径的浓度增加,材料的添加导致土壤团聚体的平均重量直径增加。此外,砂壤土对土壤团聚体的改善作用较大,粘壤土对土壤团聚的改善作用较小。有趣的是,有机物质在不同植物和连续年份增加土壤持水量方面的作用并不显著。通过在田间容量和永久枯萎点添加有机材料,土壤体积水分的增加远好于其他研究的土壤水分点。沙壤土质地和半干旱气候表明附加有机物质的变异性最大。总之,在沙壤土质地的干旱和半干旱气候中,堆肥肥料对土壤持水能力的影响最大,尤其是在FC和PWP水分点
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