利用可见光-近红外光谱估算全剖面土壤有机碳及其组分

Mingxuan Qi , Songchao Chen , Yuchen Wei , Hangxin Zhou , Shuai Zhang , Mingming Wang , Jinyang Zheng , Raphael A. Viscarra Rossel , Jinfeng Chang , Zhou Shi , Zhongkui Luo
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引用次数: 0

摘要

土壤有机碳(SOC)对土壤健康和质量至关重要,其固存被认为是应对气候变化的一种自然解决方案。准确而经济高效地测定土壤有机碳及其功能组分对有效管理土壤有机碳至关重要。可见近红外光谱法(vis-NIR)已成为一种具有成本效益的方法。然而,它预测整个剖面 SOC 含量及其组分的能力却很少得到评估。在此,我们测量了中国西北、西南和华南 183 块旱地作物田中七个连续层的 SOC 及其两个功能组分--颗粒有机碳 (POC) 和矿物相关有机碳 (MAOC),最深达 200 厘米。然后,采集土壤样本的可见光-近红外光谱来训练机器学习模型(偏最小二乘回归),以预测 SOC、POC、MAOC 以及 MAOC 与 SOC 的比率(MAOC/SOC--碳脆弱性指数)。我们发现,对于 SOC、POC、MAOC 和 MAOC/SOC 而言,验证的决定系数(Rval2)分别为 0.39、0.30、0.49 和 0.48,表明了模型的准确性。加入年平均气温后,模型性能得到改善,四个碳变量的 Rval2 分别提高到 0.64、0.31、0.63 和 0.51。进一步将 SOC 纳入模型后,Rval2 分别增至 0.82、0.64 和 0.59。这些结果表明,将可见光-近红外光谱与现成的气候数据和总 SOC 测量结果相结合,可以快速、准确地估算不同环境条件下的全剖面 POC 和 MAOC,从而有助于可靠地预测大空间范围内的全剖面 SOC 动态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Using visible-near infrared spectroscopy to estimate whole-profile soil organic carbon and its fractions

Using visible-near infrared spectroscopy to estimate whole-profile soil organic carbon and its fractions

Soil organic carbon (SOC) is crucial for soil health and quality, and its sequestration has been suggested as a natural solution to climate change. Accurate and cost-efficient determination of SOC and its functional fractions is essential for effective SOC management. Visible near-infrared spectroscopy (vis-NIR) has emerged as a cost-efficient approach. However, its ability to predict whole-profile SOC content and its fractions has rarely been assessed. Here, we measured SOC and its two functional fractions, particulate (POC) and mineral-associated organic carbon (MAOC), down to a depth of 200 ​cm in seven sequential layers across 183 dryland cropping fields in northwest, southwest, and south China. Then, vis-NIR spectra of the soil samples were collected to train a machine learning model (partial least squares regression) to predict SOC, POC, MAOC, and the ratio of MAOC to SOC (MAOC/SOC – an index of carbon vulnerability). We found that the accuracy of the model indicated by the determination coefficient of validation (Rval2) is 0.39, 0.30, 0.49, and 0.48 for SOC, POC, MAOC, and MAOC/SOC, respectively. Incorporating mean annual temperature improved model performance, and Rval2 was increased to 0.64, 0.31, 0.63, and 0.51 for the four carbon variables, respectively. Further incorporating SOC into the model increased Rval2 to 0.82, 0.64, and 0.59, respectively. These results suggest that combining vis-NIR spectroscopy with readily-available climate data and total SOC measurements enables fast and accurate estimation of whole-profile POC and MAOC across diverse environmental conditions, facilitating reliable prediction of whole-profile SOC dynamics over large spatial extents.

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