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Quantifying and correcting for clay content effects on soil water measurement by reflectometers

机译:粘土含量效应对土壤水分测量对反射计的量化和校正

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The presence of clay particles increases the specific surface area of a soil and can affect the calibration of electromagnetic soil water sensors including reflectometers. To quantify and correct for this effect in two relatively new reflectometers, three TDR315 and three CS655 sensors were installed in each of five soils with clay content ranging from 5 to 49%. As the soils were dried in a temperature controlled room, sensor reported soil volumetric water content (theta(v)) according to the factory calibration was compared against reference theta(v) determined by weighing the soils. Sensor reported theta(v) was similar to reference theta(v) in the sand soil (root mean square difference (RMSD) 0.02 m(3) m(-3)), but the discrepancy was larger for the clayey soils. An increase in clay content tended to cause TDR315 to underestimate low theta(v) and tended to cause CS655 to overestimate theta(v) in a concave down pattern. At the levels evaluated in this experiment, differences in clay content produced a larger effect than differences in temperature (24 versus 35 degrees C) and salinity (0 versus 3.09 g/L CaCl2) on factory calibration accuracy of both sensors. Soil specific empirical calibrations developed using a square root mixing model fitted the experimental data very closely (R-2 > 0.93) for both sensors. By estimating calibration coefficients based on clay content alone to recalculate sensor theta(v) from sensor reported apparent relative permittivity, RMSD from reference theta(v) was reduced by approximately 36% for both sensors as compared with using the factory calibration. Applying the same procedure to independent literature data tended to improve theta(v) accuracy of both sensors increasingly as clay content increased above 20%. The findings suggest that a simple, user-friendly correction for clay content effects may provide initial practical improvement over the factory calibration of a reflectometer in clayey soils.
机译:粘土颗粒的存在增加了土壤的比表面积,并且可以影响包括反射器的电磁土水传感器的校准。为了在两个相对较新的反射器中进行量化和校正这种效果,在五个土壤中的每一个中安装了三个TDR315和三个CS655传感器,粘土含量为5至49%。当土壤在温控室中干燥时,传感器报告了根据工厂校准的土壤体积含水量(θ(v))与通过称量土壤测定的参考Theta(v)进行比较。传感器报告θ(v)与砂土中的参考θ(v)类似(均方均差(RMSD)& 0.02米(3)m(-3)),但粘土土壤的差异较大。粘土含量的增加倾向于导致TDR315低估低θ(V)并倾向于导致CS655以凹下的下置模式高估θ(V)。在该实验中评估的水平下,粘土含量的差异产生的效果大于温度(24与35摄氏度)和盐度(0与3.09g / L CaCl2)的差异,在两种传感器的工厂校准精度上。使用平方根混合模型开发的土壤具体实证校准非常紧密地(R-2> 0.93),适用于两个传感器。通过仅估计基于粘土含量的校准系数单独重新计算传感器θ(V)从传感器报告的表观相对介电常数,与使用工厂校准相比,两个传感器的RMSD从参考值θ(v)降低约36%。将相同的程序应用于独立文献数据,往往改善两个传感器的θ(v)准确度,因为粘土含量增加到20%以上。研究结果表明,对粘土内容效应的简单,用户友好的校正可以通过粘土土壤中反射计的工厂校准来提供初步的实际改善。

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