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Reflection Model for Soil Moisture Measurement Using Near-infrared Reflection Sensor

机译:近红外反射传感器土壤水分测量的反射模型

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Surface soil moisture is a significant parameter in environmental systems. A new sensor capable of estimating surface soil moisture from reflection data is presented, called near-infrared reflection sensor. Relative reflectance method is used for prediction model development. The present study investigated the reflection variations in four soil samples with a wide range of soil properties. The results showed that quadratic models were constructed between relative reflectance and soil moisture with R~2 of 0.902, 0.865, 0.955, and 0.953. The R~2 of all combined soils model is 0.886. Compared with individual quadratic models for each soil sample, all combined soils quadratic model generated prediction accuracy with values of root mean square error (RMSE= 2.43%, 3.34%, 5.21% and 2.99%). Soil moisture estimation is largely improved when the quadratic model are developed individually on each soil type except for the Soil 4, compared with all combined soils model. Individual quadratic model yielded performances very similar to the individual linear relationship. Therefore, it is feasible to construct a single quadratic model to minimize that factor effecting on reflection. The most important meaning of this study is that surface soil moisture can be rapidly and accurately measured by near-infrared reflection sensor. In the future, the prediction models can therefore provide quick assessment of surface soil moisture directly in the field.
机译:表面土壤水分是环境系统中的重要参数。呈现了一种能够从反射数据估计表面土壤水分的新传感器,称为近红外反射传感器。相对反射方法用于预测模型开发。本研究研究了四种土壤样品中具有广泛土壤性质的反射变化。结果表明,在相对反射率和土壤水分之间构建了二次模型,其r〜2,0.865,0.955和0.953。所有组合土壤模型的R〜2为0.886。与每个土壤样本的单个二次模型相比,所有组合的土壤二次模型产生预测精度,具有根均方误差的值(RMSE = 2.43%,3.34%,5.21%和2.99%)。与所有组合的土壤模型相比,当在不同的土壤4上单独开发时,在每种土壤类型上单独开发时,土壤水分估计大大提高。单个二次模型产生与单个线性关系非常相似的表现。因此,构建单个二次模型是可行的,以最小化对反射的影响。本研究中最重要的意义是通过近红外反射传感器可以快速准确地测量表面土壤水分。因此,预测模型可以在现场直接提供对表面土壤水分的快速评估。

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