Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China.
Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China; University of Chinese Academy of Sciences, 100000, Beijing, China.
J Environ Manage. 2022 Oct 1;319:115751. doi: 10.1016/j.jenvman.2022.115751. Epub 2022 Jul 20.
Carbon (C) and nitrogen (N) cycles of terrestrial ecosystems play key roles in global climate change and ecosystem sustainability. In recent decades, climate change has threatened the nutrient balance of dryland ecosystems. However, its impact on soil organic carbon (SOC) and soil total nitrogen (STN) in drylands of China are still unclear. In this study, the structural equation model (SEM) was used to explain the relationship between environmental variables used by the best model and SOC or STN. Then Adaptive Boosting Regressor (AdaBoost), Gradient Boosting Regression (GBRT), Extreme gradient boosting Regression (XGBoost) and Random Forest Regression (RF) were used to establish the prediction model of SOC and STN based on soil samples along with environmental variables. The performance of these models was assessed based on a 10-fold cross-validation method using three statistical indicators. Finally, we predicted the SOC and STN of soil samples from 2000 to 2019 based on the best model. Overall, the RF model performed better at predicting SOC and STN in drylands than the other three prediction models (AdaBoost, GBRT, XGBoost). Climate factors were the main factors affecting SOC and STN in the study area. In the Alashan, a dryland in northern China, the precipitation in the growing season increased from 2000 to 2019, at a rate of 12.9 mm/decade. During the same period, the annual sunshine duration significantly decreased by 66 h/decade. Along with interannual hydrothermal variability, SOC showed a fluctuating upward trend at a rate of 0.04 g/kg/decade, while STN exhibited a fluctuating downward trend at 0.003 g/kg/decade from 2000 to 2019. Due to the effects of climate change, dryland were considered as potential sites for carbon sequestration. However, due to the annual hydrothermal variance causing dynamic annual changes, it was deemed unstable. Moreover, it would cause STN loss, which might reduce soil fertility. More attention should be paid to STN monitoring in dryland in the future.
陆地生态系统的碳(C)和氮(N)循环在全球气候变化和生态系统可持续性中起着关键作用。近几十年来,气候变化威胁着旱地生态系统的养分平衡。然而,其对中国旱地土壤有机碳(SOC)和土壤总氮(STN)的影响仍不清楚。本研究采用结构方程模型(SEM)来解释最佳模型中使用的环境变量与 SOC 或 STN 之间的关系。然后,采用自适应提升回归器(AdaBoost)、梯度提升回归(GBRT)、极端梯度提升回归(XGBoost)和随机森林回归(RF),基于土壤样本和环境变量建立 SOC 和 STN 的预测模型。采用 10 折交叉验证方法,利用三个统计指标评估这些模型的性能。最后,根据最佳模型预测了 2000 年至 2019 年土壤样本的 SOC 和 STN。总体而言,RF 模型在预测旱地 SOC 和 STN 方面的表现优于其他三个预测模型(AdaBoost、GBRT、XGBoost)。气候因素是研究区 SOC 和 STN 的主要影响因素。在中国北方的阿拉善干旱区,生长季的降水量从 2000 年到 2019 年以 12.9mm/decade 的速度增加。同期,年日照时数以 66h/decade 的速度显著减少。随着年际水热变化,SOC 以 0.04g/kg/decade 的速度呈波动上升趋势,而 STN 则以 0.003g/kg/decade 的速度呈波动下降趋势,从 2000 年到 2019 年。由于气候变化的影响,旱地被认为是潜在的碳封存地点。然而,由于年水热变化导致动态的年际变化,它被认为是不稳定的。此外,它会导致 STN 损失,从而可能降低土壤肥力。未来应更加关注旱地的 STN 监测。