Analysis of Soil Texture, Furrow Geometry, and Infiltration Rate for Improving Water Application Efficiency

Q3 Social Sciences
Duba Chena Dero, K. Kolhe
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引用次数: 1

Abstract

Soil texture, furrow geometry, and infiltration rate are the main characteristics for improving water application efficiency. Substantial amounts of diverted irrigation water are often lost because of poor water control, inefficient irrigation conveyance systems, poor on-farm water management, or poor application practices. Field experiments were conducted on three farm plots within the command area for water availability and accessibility under the Melka Hida small-scale irrigation scheme in the West Guji Zone of Oromia Region, Ethiopia. The physical characteristics of soil, including depth, particle distribution, textural classification, bulk density, field capacity, and permanent wilting point, were studied and the results are presented. Furrow parameters including slope, width, length, and shape geometry were measured. The cumulative infiltration and infiltration rates were also recorded. The results show that irrigation application efficiency ranged from 57 to 64% with an average of 61%, indicating that about 40% of the applied water was not used by crops. The storage efficiency ranged from 79.6 to 81.6% with an average of 80%. Soil moisture measurements showed that crops were water stressed during the experimental period. Application efficiency decreased with increasingly steep slopes and cutoff times, greater applied depth, and high inflow rate in the study area. Unavailability of irrigation water control structure, weakness of water users’ associations, and maintenance of furrows and steep slopes were observed as the major causes of inefficient water management in the Melka Hida irrigation scheme.
提高水分利用效率的土壤质地、沟槽几何形状和入渗速率分析
土壤质地、垄沟几何形状和入渗速率是提高水分利用效率的主要特征。由于水资源控制不善、灌溉输送系统效率低下、农田用水管理不善或应用方法不当,大量改道的灌溉用水经常流失。在埃塞俄比亚奥罗米亚州西古吉地区的Melka Hida小规模灌溉计划下,在指挥区内的三个农田进行了实地试验,以了解水的可利用性和可及性。研究了土壤的物理特性,包括深度、颗粒分布、质地分类、容重、田间容量和永久萎蔫点,并给出了结果。测量犁沟参数,包括坡度、宽度、长度和形状几何。同时记录了累积入渗和入渗速率。结果表明,灌溉水利用率在57% ~ 64%之间,平均为61%,表明约40%的灌溉水未被作物利用。存储效率范围为79.6 ~ 81.6%,平均为80%。土壤水分测量结果表明,试验期间作物处于水分胁迫状态。随着研究区域坡度和截止时间的增加、应用深度的增加和流入速率的增加,应用效率下降。在Melka Hida灌溉计划中,缺乏灌溉用水控制结构、用水户协会薄弱、沟槽和陡坡的维护是水管理效率低下的主要原因。
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来源期刊
Asian Journal of Agriculture and Rural Development
Asian Journal of Agriculture and Rural Development Social Sciences-Geography, Planning and Development
CiteScore
1.30
自引率
0.00%
发文量
28
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