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Spectral soil analysis and inference systems: A powerful combination for solving the soil data crisis

机译:光谱土壤分析和推断系统:解决土壤数据危机的强大组合

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Diffuse reflectance spectroscopy (DRS) is attracting much interest in the soil science community because it has a number of advantages over conventional methods of soil analyses. The techniques are more rapid, timely, cheaper and hence more efficientat obtaining the data when a large number of samples and analysis are required. Moreover, a single spectrum may be used to assess various physical, chemical and biological soil properties. Until now, research in soil spectroscopy has focused on spectralcalibration and prediction of soil properties using multivariate statistics. In this paper we show how these predictions may be used in an inference system to predict other important and functional soil properties using pedotransfer functions (PTFs). Thus we propose the use of soil spectral calibration and its predictions as input and as a complement to a soil inference system (SPEC-SINFERS). We demonstrate the implementation of SPEC-SINFERS with two examples. As a first step, soil mid-infrared (MIR) spectra and partial least squares (PLS) regression are used to estimate soil pH, clay, silt, sand, organic carbon content and cation exchange capacity. A bootstrap method is used to determine the uncertainties of these predictions. These predictions and their uncertainties are then used as input into the inference system, where established PTFs are used to infer (i) soil water content and (ii) soil pH buffering capacity together with their uncertainties. An important feature of SPEC-SINFERS is the propagation of both input and model uncertainties.
机译:漫反射光谱法(DRS)在土壤科学界引起了广泛兴趣,因为它比常规的土壤分析方法具有许多优势。当需要大量样本和分析时,该技术更快速,更及时,更便宜,因此更有效地获取数据。此外,单个光谱可用于评估各种物理,化学和生物土壤特性。到目前为止,土壤光谱学的研究一直集中在使用多元统计数据进行光谱校准和预测土壤性质。在本文中,我们展示了这些预测如何在推理系统中使用pedotransfer函数(PTF)来预测其他重要的和功能性的土壤特性。因此,我们建议使用土壤光谱校准及其预测作为输入,并作为土壤推断系统(SPEC-SINFERS)的补充。我们通过两个示例演示SPEC-SINFERS的实现。第一步,使用土壤中红外(MIR)光谱和偏最小二乘(PLS)回归来估算土壤的pH值,粘土,淤泥,沙子,有机碳含量和阳离子交换能力。引导法用于确定这些预测的不确定性。然后将这些预测及其不确定性用作推论系统的输入,在推论系统中,已建立的PTF用于推导(i)土壤含水量和(ii)土壤pH缓冲能力及其不确定性。 SPEC-SINFERS的一个重要特征是输入和模型不确定性的传播。

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