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首页> 外文期刊>Journal of King Saud University >Investigation of soil moisture content over a cultivated farmland in Abeokuta Nigeria using electrical resistivity methods and soil analysis
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Investigation of soil moisture content over a cultivated farmland in Abeokuta Nigeria using electrical resistivity methods and soil analysis

机译:利用电阻率法和土壤分析法调查尼日利亚阿贝库塔(Abeokuta)耕地的土壤水分

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摘要

A combined 1D and 2D electrical resistivity surveys as well as laboratory determination of soil moisture contents of topsoil in a University cultivated farmland is presented. Apparent resistivity data were measured along six traverses using Schlumberger and Wenner arrays while soil samples were collected from all traverses at depths of 0.5, 1.0, 1.5 and 2.0?m respectively. The ranges of resistivity and thickness of the topsoil, clayey sand and weathered layers are 78.0–1094.0?Ωm, 0.5–1.9?m; 110.0–275.0?Ωm, 1.1–11.9?m; and 19.0–274.0?Ωm, 1.1–14.0?m respectively. 2D resistivity inverted sections revealed three zones of resistivity anomalies: topsoil with resistivity 78.0–600.0??m for traverses within the farmland and that of two traverses along the entrances to the farm. The second resistivity zone represents a clay region of high moisture content with resistivity values less than 25.0?Ωm. The third layer represents weathered/fractured layer with relatively high resistivity values ranging from 116 to 600?Ωm. The 1D resistivity models showed effective depths of more than 30.0?cm while the 2D image lines revealed that active water uptake zone extends to about 3.0?m depth. All the collected soil samples belong to sandy loam while the soil moisture content values ranged from 45 to 74% at different soil depths of 0.5–2.0?m. The study has shown that the integrated methods provide important methods for better management of soil water reserves for improved agricultural production.
机译:结合一维和二维电阻率调查以及实验室测定的大学耕地表层土壤水分含量。使用Schlumberger和Wenner阵列沿六个导线测量视电阻率数据,同时分别从所有导线在0.5、1.0、1.5和2.0?m的深度采集土壤样品。表层土壤,黏土砂和风化层的电阻率和厚度范围为78.0-1094.0?Ωm,0.5-1.9?m。 110.0–275.0?Ωm,1.1–11.9?m;和19.0–274.0?Ωm,1.1–14.0?m。二维电阻率倒置剖面显示出电阻率异常的三个区域:农田内导线的电阻率为78.0–600.0?m的表土,以及农田入口处的两个导线的电阻率。第二电阻率区代表高水分含量的粘土区域,电阻率值小于25.0?Ωm。第三层代表风化/断裂层,其相对较高的电阻率值范围为116至600?Ωm。一维电阻率模型显示的有效深度超过30.0?cm,而二维图像线则显示出有效的水吸收区扩展到了约3.0?m的深度。所有收集的土壤样品都属于沙壤土,而在0.5-2.0?m的不同土壤深度下,土壤水分含量范围为45%至74%。研究表明,综合方法为更好地管理土壤水分储备以改善农业生产提供了重要方法。

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