TDR calibration of organic forest floor media

M.G. Schaap, L. de Lange, T.J. Heimovaara
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引用次数: 87

Abstract

We carried out a time domain reflectometry (TDR) calibration for 25 forest floor samples of five different forest stands. Linear regression was used to estimate the volumetric water content from the refraction index. Due to the presence of bound water, it was impossible to predict the calibration line parameters from theoretical values with a refractive mixing model. However, when the apparent dielectric constant of the water was considered, it was possible to predict the offset parameter because the low forest floor bulk density caused the calibration line slope and offset to be almost reversely proportional. Calibration parameters for different forest floor materials are presented. Allowing a somewhat higher margin of error we could also establish general calibration curves which were in close agreement with a published calibration curve (Malicki et al., 1994). An error analysis showed that decomposition of organic matter, residual water and temperature effects have negligible effects on the calibration parameters. Shrinkage of the organic material significantly influenced both the volumetric water content and the TDR reflection times. If not corrected, both effects yielded systematic errors of approximately 0.02 cm3 cm−3 for a strongly shrinking H horizon.

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有机森林地面介质的TDR校准
对5个不同林分的25个森林地表样本进行了时域反射(TDR)定标。利用折射率线性回归估计体积含水量。由于束缚水的存在,用折光混合模型从理论值预测校准线参数是不可能的。然而,当考虑水的视介电常数时,由于低森林地面容重导致校准线斜率和偏移量几乎成反比,因此可以预测偏移参数。给出了不同森林地面材料的标定参数。允许较高的误差范围,我们还可以建立与已发表的校准曲线密切一致的一般校准曲线(Malicki et al., 1994)。误差分析表明,有机物分解、残余水分和温度效应对标定参数的影响可以忽略不计。有机材料的收缩对体积含水量和TDR反射时间都有显著影响。如果不加以修正,对于强烈收缩的H视界,这两种效应产生的系统误差约为0.02 cm3 cm - 3。
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