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A comparison of point and imaging visible-near infrared spectroscopy for determining soil organic carbon

机译:点和成像可见近红外光谱法测定土壤有机碳的比较

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This study evaluated whether the accuracy of soil organic carbon measurement by laboratory hyperspectral imaging can match that of standard point spectroscopy operating in the visible–near infrared. Hyperspectral imaging allows a greater amount of spectral information to be collected from the soil sample compared to standard spectroscopy, accounting for greater sample representation. A total of 375 representative Irish soils were scanned by two-point spectrometers (a Foss NIR Systems 6500 labelled S-1 and a Varian FT-IR 3100 labelled S-2) and two laboratory hyperspectral imaging systems (two push broom line-scanning hyperspectral imaging systems manufactured by DV optics and Spectral Imaging Ltd, respectively, labelled S-3 and S-4). The objectives were (a) to compare the predictive ability of spectral datasets for soil organic carbon prediction for each instrument evaluated and (b) to assess the impact of imposing a common wavelength range and spectral resolution on soil organic carbon model accuracy. These objectives examined the predictive ability of spectral datasets for soil organic carbon prediction based on optimal settings of each instrument in (a) and introduced a constraint in wavelength range and spectral resolution to achieve common settings for instruments in (b). Based on optimal settings for each instrument, the deviation (root-mean square error of prediction) from the best fit line between laboratory measured and predicted soil organic carbon, ranked the instruments as S-1 (26.3?g?kg~(?1))?
机译:本研究评估了实验室高光谱成像的土壤有机碳测量的准确性是否可以将标准点光谱法在可见的近红外线中匹配。与标准光谱相比,高光谱成像允许从土壤样品中收集更多的光谱信息,占更大的样品表示。两点光谱仪共扫描了375个代表性的土壤(彩色NIR系统6500标记为S-1和Varian FT-IR 3100标记为S-2)和两个实验室高光谱成像系统(两个推扫帚线扫描高光谱通过DV光学和光谱成像有限公司生产的成像系统,分别标记为S-3和S-4)。目的是(a),比较用于每种仪器的土壤有机碳预测的光谱数据集的预测能力和(b),以评估施加普通波长范围和光谱分辨率对土壤有机碳模型精度的影响。这些目的基于(a)中的每种仪器的最佳设置,检查了土壤有机碳预测的光谱数据集的预测能力,并引入了波长范围的约束和光谱分辨率,以实现(b)中的仪器的常见设置。基于每个仪器的最佳设置,从实验室测量和预测土壤有机碳之间的最佳配合线的偏差(预测的根均方误差)将仪器排名为S-1(26.3?G?kg〜(?1 ))?<?s-2(29.4?g?kg〜(α1))?<Δs-3(34.3?g≤kg〜(α1))?<Δs-4(41.1?g?kg 〜(?1))。 S-1模型在所有偏最小二乘回归性能指标中表现出,并且在所有光谱范围内,并产生了最有利的结果在于测试,方差测试和显着变量的识别。假设较大波长范围为S-1和S-2产生更准确的土壤有机碳预测。在常见的仪器设置下,几乎等于S-1的S-3预测精度。结论是,在标准操作程序下,高光谱成像捕获的更大的土壤样本表示可以等于点光谱法的光谱的质量。这一结果对于土壤图像分析的实验室高光谱成像很重要。

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