根据土壤粒度测定对EC-5电容式土壤水分传感器进行校准

C. C. Sena, J. A. Júnior, M. H. Domingos, E. J. A. Júnior, Rafael Battisti, A. Evangelista, D. Casaroli
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引用次数: 0

摘要

用于估算土壤含水量的电容式传感器的精度取决于土壤资源,需要对其进行校正。本研究的目的是校准EC-5电容式传感器,以估计与不同塞拉多土壤粒度有关的土壤含水量。在实验室条件下,采用EC-5型传感器和体积法对砂质粘土、佛朗哥砂质粘土和粘土的水分变化进行了比较。样品采集时间为0.00 ~ 0.10;Goiás塞拉多中心支点区域0.10 ~ 0.30和0.30 ~ 0.50 m。土壤饱和后,在40℃下烘干至恒重,此过程重复三次。统计指标分析表明,EC-5传感器可用于土壤水分的测定,并需要对每种土壤类型进行校准。砂质粘土的决定系数(r2)大于0.95;Franco砂质粘土r2大于0.93,粘土质地土r2大于0.81。考虑到土壤中的粘土含量,为了校准EC-5传感器,必须使用公式:θvol=0.0758-0.0023* clay %-1.056* θEC-5。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CALIBRAÇÃO DO SENSOR CAPACITIVO DE UMIDADE DO SOLO EC-5 EM RESPOSTA A GRANULOMETRIA DO SOLO
The accuracy of the capacitive sensors used to estimate the water content in the soil depends on the soil resources, requiring calibration for its correction. The objective of this study was to calibrate the EC-5 capacitive sensor to estimate soil water content in relation to different cerrado soil granulometry. Under laboratory conditions, the moisture variation of the Sandy Clay, Franco Sandy Clay and Clay soils was compared by the EC-5 sensor and the volumetric method. Samples were collected in the layers from 0.00 to 0.10; 0.10 to 0.30 and 0.30 to 0.50 m in central pivot areas in the Cerrado of Goiás. The soil was saturated and oven dried at 40oC to constant weight, this procedure was repeated three times. The statistical indices analyzed showed that the EC-5 sensor can be used for soil moisture determination and its calibration is required for each soil type. The sandy clay soil had a coefficient of determination (r2) greater than 0.95; for Franco sandy clay soil r2 was equal to or greater than 0.93 and for clay textured soil r2 was greater than 0.81. To calibrate the EC-5 sensor considering the clay content in the soil it is necessary to use the equation: θvol=0.0758-0.0023*Clay%-1.056* θEC-5.
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