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首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >Measurement of soil water and nutrients by its electrical properties
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Measurement of soil water and nutrients by its electrical properties

机译:通过电学特性测量土壤水分和养分

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An instrument for measurement of soil dielectric constant epsilon r , electrical conductivity EC a, and soil temperature was tested on soils under potato crop to investigate contents of soil volumetric water and nutrients for eventual use in a field crop model. To approximate the dependence of on epsilon r , a logarithmic equation was chosen. Satisfactory results were obtained on stone-free areas, with the mean relative variance between -values determined by dielectric constant and converted from a gravimetric method remaining within the limits of measuring error. However, variances were higher for stony soils, with epsilon r -values at the same being considerably higher. To reconcile data from stony and stone-free soils, a formula was composed. Salinity, calculated by a semi-empirical model based on Hilhorst's theory using measured values of EC a, epsilon r , and soil temperature, correlated well with contents of K and Mg in the soil. A lower correlation resulted for P, and was practically absent for Ca. Inequality of these regression equations at different measuring sites demonstrates the necessity of considering soil pH when assessing plant nutrients in the soil.
机译:在马铃薯作物下的土壤上测试了一种用于测量土壤介电常数ε,电导率EC a和土壤温度的仪器,以研究土壤体积水和养分的含量,以最终用于田间作物模型。为了近似对ε的依赖性,选择了对数方程。在无石区域获得了令人满意的结果,其中-值之间的平均相对方差由介电常数确定并由重量分析法转换而仍保持在测量误差的范围内。然而,石质土壤的方差更高,同时εr值也更高。为了协调来自石质和无石质土壤的数据,组成了一个公式。盐度是根据希尔霍斯特理论使用EC a,εε和土壤温度的测量值通过半经验模型计算得出的,与土壤中的K和Mg含量密切相关。 P的相关性较低,而Ca几乎不存在。这些回归方程在不同测量点的不等式表明,在评估土壤中的植物养分时必须考虑土壤的pH值。

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