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首页> 外文期刊>Soil Science Society of America Journal >In Situ Determination of Soil Freezing Characteristics for Estimation of Soil Moisture Characteristics using a Dielectric Tube Sensor
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In Situ Determination of Soil Freezing Characteristics for Estimation of Soil Moisture Characteristics using a Dielectric Tube Sensor

机译:用介电管传感器原位测定土壤冻结特性以估算土壤水分。

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摘要

The soil freezing characteristic (SFC) plays a critical role in modeling the transport of water, heat, and solutes in frozen soil. Especially, the SFC can be used to estimate the soil moisture characteristic (SMC) for unfrozen soil due to the known similarity between them. In this study, we tested an existing portable dielectric tube sensor in vertical access tubes together with a set of temperature sensors for the determination of the in situ SFC and SMC. The experiment was conducted at three sites with sandy, loamy, and silt loam soils. At each site, three SFC curves were obtained at depths of 15, 25, and 35 cm. The resulting SMCs estimated from the SFCs were compared with the SMCs determined using a pressure plate apparatus. The data from the proposed method and those of the pressure plate fit the Campbell model with 0.806 <= R-2 <= 0.994 and fit the van Genuchten model with 0.638 <= R-2 <= 0.994. The coefficient of determination (R-2 = 0.837) and RMSE (131 kPa) showed a good agreement between the characteristic curves from the two methods. Thus, we recommend the dielectric tube sensor for determining the SFC in situ and inferring the SMC across depths.
机译:土壤冻结特征(SFC)在模拟冻结土壤中水,热和溶质的传输过程中起着至关重要的作用。特别是,由于它们之间的已知相似性,SFC可以用于估计未冻结土壤的土壤水分特征(SMC)。在这项研究中,我们测试了垂直通道中现有的便携式介电管传感器以及一组用于确定原位SFC和SMC的温度传感器。在含沙壤土,壤质壤土和粉质壤土的三个地点进行了该实验。在每个位置,在15、25和35 cm的深度处获得了3条SFC曲线。将由SFC估算出的最终SMC与使用压板设备确定的SMC进行比较。所提出的方法和压力板的数据拟合的坎贝尔模型的拟合度为0.806 <= R-2 <= 0.994,而van Genuchten模型的拟合结果为0.638 <= R-2 <= 0.994。测定系数(R-2 = 0.837)和RMSE(131 kPa)在两种方法的特性曲线之间显示出良好的一致性。因此,我们建议使用介电管传感器来就地确定SFC并推断出各个深度的SMC。

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