基于可见-近红外和中红外光谱数据融合的不同土层关键土壤特性预测

IF 2.9 Q1 AGRICULTURE, MULTIDISCIPLINARY
Dewen Qiao, Muhammad Ali and Abdul Mounem Mouazen*, 
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引用次数: 0

摘要

作物的养分利用率并不局限于表层土壤;更深的层次也是重要的来源。快速测定不同深度的土壤性质对农业投入物的精确管理至关重要。大多数现有研究都集中在使用单个传感器的光谱数据预测表层土壤性质,而探索多传感器光谱融合在不同深度土壤分析中的潜力的研究仍然有限。本研究评估了:(1)使用可见光和近红外(vis-NIR)和中红外(MIR)分光光度计的单光谱建模;(2)两种光谱融合方法──直接连接和全光谱吸光度的外产物分析──对五个关键土壤特性的预测性能:pH、总有机碳(TOC)、有效磷(AP)、有效钾(AK)和镁(Mg),覆盖三个土壤深度。该数据集包括从五块耕地的59个地点收集的176个新鲜土壤样本。使用偏最小二乘回归(PLSR)和支持向量机(SVM)建立预测模型,并使用决定系数(R2)、均方根误差(RMSE)和性能与四分位数距离之比(RPIQ)对其性能进行评估。结果表明,可见光-近红外光谱总体优于MIR,验证R2为0.39 ~ 0.67,RPIQ为0.84 ~ 3.25 (R2 = 0.42 ~ 0.62, RPIQ = 0.97 ~ 3.08)。值得注意的是,使用OPA-SVM方法的光谱融合对TOC (R2 = 0.75, RPIQ = 3.35)和AP (R2 = 0.83, RPIQ = 4.72)的预测效果最好,而DC-PLSR模型对pH的预测效果最好(R2 = 0.65, RPIQ = 2.43)。然而,融合并不总是优于单光谱模型;例如,visi - nir - svm和MIR-SVM分别对AK (R2 = 0.53, RPIQ = 1.45)和Mg (R2 = 0.61, RPIQ = 1.30)的评价结果最好。考虑到这些不同的结果,我们建议根据预测性能和实际考虑(如成本效益和操作可行性)来选择光谱技术。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Data Fusion of Visible-Near-Infrared and Mid-Infrared Spectra for Predicting Key Soil Properties across Different Soil Layers

Data Fusion of Visible-Near-Infrared and Mid-Infrared Spectra for Predicting Key Soil Properties across Different Soil Layers

Nutrient availability for crops is not limited to the topsoil; deeper layers also serve as significant sources. Rapid determination of soil properties at different depths is essential for the precision management of farming inputs. Most existing studies focus on predicting surface soil properties using spectral data from a single sensor, while research exploring the potential of multisensor spectral fusion for soil analysis at varying depths remains limited. This study evaluated the predictive performance of: (1) single-spectrum modeling using visible and near-infrared (vis–NIR) and mid-infrared (MIR) spectrophotometers and (2) two spectral fusion methods─direct concatenation and outer product analysis of full-spectral absorbance─for five key soil properties: pH, total organic carbon (TOC), available phosphorus (AP), available potassium (AK), and magnesium (Mg), across three soil depths. The data set comprised 176 fresh soil samples collected from 59 locations across five arable cropping fields. Prediction models were developed using partial least-squares regression (PLSR) and support vector machine (SVM), whose performance was assessed using the coefficient of determination (R2), root-mean-square error (RMSE), and ratio of performance to interquartile distance (RPIQ). Results showed that vis–NIR spectra generally outperformed MIR, with validation R2 ranging from 0.39 to 0.67 and RPIQ from 0.84 to 3.25, compared to MIR (R2 = 0.42–0.62, RPIQ = 0.97–3.08). Notably, spectral fusion using the OPA–SVM method yielded the best predictions for TOC (R2 = 0.75, RPIQ = 3.35) and AP (R2 = 0.83, RPIQ = 4.72), while the DC-PLSR model achieved the highest performance for pH (R2 = 0.65, RPIQ = 2.43). However, fusion was not always superior to single-spectrum models; for example, vis–NIR-SVM and MIR-SVM gave the best results for AK (R2 = 0.53, RPIQ = 1.45) and Mg (R2 = 0.61, RPIQ = 1.30), respectively. Given these varying results, we recommend selecting spectroscopic techniques based on both predictive performance and practical considerations such as cost-effectiveness and operational feasibility.

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