Improving the Estimation Accuracy of Soil Organic Matter Content Based on the Spectral Reflectance from Soils with Different Grain Sizes

Land Pub Date : 2024-07-22 DOI:10.3390/land13071111
Xayida Subi, Mamattursun Eziz, Ning Wang
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Abstract

Accurate and rapid estimation of soil organic matter (SOM) content is of great significance for advancing precision agriculture. Compared with traditional chemical methods, the hyperspectral estimation is superior in rapidly estimating SOM content. Soil grain size affects soil spectral reflectance, thereby affecting the accuracy of hyperspectral estimation. However, the appropriate soil grain size for the hyperspectral analysis is nearly unknown. This study propose a best hyperspectral estimation method for determining SOM content of farmland soil in the Ibinur Lake Irrigation Area (ILIA) of the northwest arid zones of China. The original spectral reflectance of the 20-mesh (0.85 mm) and 60-mesh (0.25 mm) sieved soil were obtained, and the feature wavebands were selected using five types of spectral transformations. Then, hyperspectral estimation models were constructed based on the partial least squares regression (PLSR), support vector machine (SVM), random forest (RF), and extreme gradient boosting (XGBoost) models. Results show that the SOM content had relatively higher correlation coefficient with spectral reflectance of the 0.85 mm sieved soil than that of the 0.25 mm sieved soil. The transformation of original spectral reflectance of soil effectively enhanced the spectral characteristics related to SOM content. Soil grain size obviously affected spectral reflectance and the accuracy of hyperspectral estimation models. The overall stability and estimation accuracy of RF model was significantly higher compared with the PLSR, SVM, and XGBoost. Finally, the RF model combined with the root mean first-order differentiation (RMSFD) of spectral reflectance of the 0.85 mm sieved soil (R2 = 0.82, RMSE = 2.37, RPD = 2.27) was identified as the best method for estimating SOM content of farmland soil in the ILIA.
基于不同粒径土壤的光谱反射率提高土壤有机质含量的估算精度
准确、快速地估算土壤有机质(SOM)含量对推进精准农业具有重要意义。与传统的化学方法相比,高光谱估算法在快速估算土壤有机质含量方面更具优势。土壤粒度会影响土壤光谱反射率,从而影响高光谱估算的准确性。然而,用于高光谱分析的合适土壤粒度几乎是未知的。本研究提出了一种确定中国西北干旱区伊比努尔湖灌区农田土壤 SOM 含量的最佳高光谱估算方法。研究分别获得了 20 目(0.85 mm)和 60 目(0.25 mm)筛分土壤的原始光谱反射率,并通过五种光谱变换选择了特征波段。然后,基于偏最小二乘回归(PLSR)、支持向量机(SVM)、随机森林(RF)和极梯度提升(XGBoost)模型构建了高光谱估算模型。结果表明,SOM 含量与 0.85 毫米筛分土壤光谱反射率的相关系数相对高于 0.25 毫米筛分土壤。对土壤原始光谱反射率的转换有效地增强了与 SOM 含量相关的光谱特征。土壤粒度明显影响光谱反射率和高光谱估算模型的精度。与 PLSR、SVM 和 XGBoost 相比,RF 模型的整体稳定性和估计精度明显更高。最后,RF 模型与 0.85 毫米筛分土壤光谱反射率的均方根一阶差分(RMSFD)相结合(R2 = 0.82,RMSE = 2.37,RPD = 2.27)被认为是估算 ILIA 地区农田土壤 SOM 含量的最佳方法。
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