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A Technical Design Approach to Soil Moisture Content Measurement

机译:一种测量土壤含水量的技术设计方法

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Soil moisture is an important type of data in many fields; ranging from agriculture toenvironmental monitoring. Three soil samples were collected at definite proportions to represent the three basic soiltypes (sandy, loamy and clay soils). The moisture contents of these soil samples were analyzed using thethermogravimetric method. This paper employed the use of PC-based soil moisture content measuring system inorder to obtain accurate results. It works with the principle that there is an increase or decrease in soil conductivity assoil moisture increases or decreases respectively. The constructed prototype was used to test the three soil samples aswell and the results were compared with that of the thermogravimetric method. The results gotten from this prototypeshows the relationship between conductivity and moisture content of the soil. The system was well calibrated in orderto get standard readings and conquer the problem of transistor amplification at the signal pick up stage. This thereforemakes it possible to get fast an accurate results without wasting much time and energy.
机译:土壤水分是许多领域的重要数据类型。从农业到环境监测。以一定比例收集了三个土壤样本,以代表三种基本土壤类型(沙质,壤土和粘土)。使用热重法分析这些土壤样品的水分含量。为了获得准确的结果,本文使用了基于PC的土壤水分含量测量系统。它的原理是土壤电导率分别随着土壤水分的增加或减少而增加或减少。所构建的原型还用于测试这三个土壤样品,并将结果与​​热重法进行了比较。从该原型获得的结果表明了土壤电导率与水分含量之间的关系。为了获得标准读数并在信号拾取阶段克服晶体管放大问题,该系统经过了良好的校准。因此,这使得可以快速获得准确的结果而不会浪费很多时间和精力。

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