法国土壤有机碳储量的国家尺度制图:通过直接和间接方法获得的新见解和经验教训

Zhongxing Chen , Qi Shuai , Zhou Shi , Dominique Arrouays , Anne C. Richer-de-Forges , Songchao Chen
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引用次数: 1

摘要

土壤有机碳(SOC)在土壤健康和全球碳循环中起着至关重要的作用,因此准确估算其空间分布对土壤健康管理和减缓全球气候变化具有重要意义。数字土壤制图显示了其提供准确和高分辨率的土壤有机碳跨尺度空间分布的潜力。为了将有机碳含量转化为有机碳密度(SOCD),在数字土壤制图中存在两种预测SOCD的推断轨迹:直接方法(计算-模型)和间接方法(模型-计算)。然而,缺乏对它们在SOCD估算中的表现差异的全面探索,特别是在以不同气候条件为特征的地区。为了弥补这一知识差距,我们根据法国SOCD的模型性能评估了两种方法。利用LUCAS Soil 2018的916个表层土壤(0 ~ 20 cm)和24个环境协变量,采用随机森林模型和正向递归特征选择方法,通过直接和间接方法建立了SOCD的空间预测模型。结果表明,在使用随机森林模型和全协变量时,两种方法都表现出中等的性能(R2 = 0.28 ~ 0.32)。利用前向递归特征选择模型,将预测因子数量从24个减少到9个,直接方法的模型性能得到提高(R2为0.35),间接方法的模型性能没有提高(R2为0.28)。直接法和间接法测得法国表层土壤平均SOCD分别为5.29和6.14 kg m−2,土壤有机碳储量分别为2.8和3.3 Pg。我们发现直接方法明显低估了高SOCD (>9 kg m−2),而间接方法在高SOCD方面表现得更好。研究结果可为土壤镉制图提供有价值的参考,从而为维护土壤健康提供科学依据。
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National-scale mapping of soil organic carbon stock in France: New insights and lessons learned by direct and indirect approaches

Soil organic carbon (SOC) plays a crucial role in soil health and global carbon cycling, therefore accurate estimates of its spatial distribution are important for managing soil health and mitigating global climate change. Digital soil mapping shows its potential to provide accurate and high-resolution spatial distribution of SOC across scales. To convert SOC content to SOC density (SOCD), two inference trajectories exist for predicting SOCD in digital soil mapping: the direct approach (calculate-then-model) and indirect approach (model-then-calculate). However, there is a lack of comprehensive exploration regarding the differences in their performance in SOCD estimates, particularly in regions characterized by diverse pedoclimatic conditions. To bridge this knowledge gap, we evaluated the two approaches based on model performance of SOCD in France. Using 916 topsoils (0−20 ​cm) from the LUCAS Soil 2018 and 24 environmental covariates, random forest model and forward recursive feature selection were used to build the spatial predictive models of SOCD using direct and indirect approaches. The results show that, using random forest model and full covariates, both approaches show moderate performance (R2 ​= ​0.28−0.32). By utilizing forward recursive feature selection model, the number of predictors was reduced from 24 to 9, enhancing model performance for direct approach (R2 of 0.35), with no improvement for indirect approach (R2 of 0.28). The mean SOCD of the French topsoil was 5.29 and 6.14 ​kg ​m−2 by direct and indirect approaches, resulting in SOC stock of 2.8 and 3.3 ​Pg, respectively. We found that the direct approach clearly underestimated the high SOCD (>9 ​kg ​m−2), while the indirect approach performed much better for high SOCD. Our findings serve as a valuable reference for SOCD mapping, thereby providing a scientific basis for maintaining soil health.

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