基于遥感和机器学习的土壤有机碳时空制图

Bruno dos Anjos Bartsch, Nicolas Augusto Rosin, Jorge Tadeu Fim Rosas, Raul Roberto Poppiel, Fernando Yutaro Makino, Letícia Guadagnin Vogel, Jean Jesus Macedo Novais, Renan Falcioni, Marcelo Rodrigo Alves, José A.M. Demattê
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引用次数: 0

摘要

土壤圈是最大的陆地碳库。土壤有机碳(SOC)是土壤质量和作物生产力的关键属性,与减缓气候变化和粮食安全直接相关。巴西拥有巨大的农业生产面积和巨大的碳封存潜力。然而,目前对全国有机碳的时空分布知之甚少,阻碍了低碳农业公共政策的实施。我们的目的是绘制在0.00 ~ 0.20 cm深度两个时间段内土壤有机碳的时空分布。我们评估了7年的SOC变化,生成了5个周期的时间序列,得到了平均SOC值。利用Cubist算法分别对两种短期(2年)和长期(7年/全期)土壤有机碳空间预测模型进行了标定。采用遥感数据和土壤粒度分布图作为环境协变量。我们在验证中发现,短期模型的R2值为0.47和0.25,长期模型的R2值为0.34。根据短周期模型和长周期模型,该地区有机碳含量分别下降了54.97 %和53.72 %。在短周期模型和长周期模型的预测图中,研究区土壤有机碳的变化趋势相同。
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Space-time mapping of soil organic carbon through remote sensing and machine learning
Pedosphere is the largest terrestrial carbon reservoir. Soil organic carbon (SOC) is a critical attribute for soil quality and crop productivity, being directly linked to climate change mitigation and food security. Brazil boasts a significant agricultural production area and substantial potential for carbon sequestration. Nevertheless, the spatial-temporal distribution of SOC across the country is poorly understood, hindering the implementation of low-carbon agriculture public policies. We aimed to map the spatio-temporal distribution of SOC at from 0.00 to 0.20 cm depth over two periods. We assessed the SOC variation over seven years, generating a time series with five periods, obtaining the average SOC values. The Cubist algorithm was used to calibrate two short period (two years) and a long period (seven years/all period) models for SOC spatial prediction. Remote sensing data and soil particle size distribution maps were used as environmental covariates. We found in validation R2 values of 0.47 and 0.25 for short period models, and 0.34 for the long period model. The SOC content decreased by 54.97 % in the area according to the mapping by short period models and 53.72 % according to mapping by the long-period model. The predicted maps showed the same trend of the database (soil samples with observed SOC values) for the study areas using both short period and long period models.
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