内蒙古黑土区土壤有机质空间分布的主控因子与阈值效应研究

Dominant Factors and Threshold Effects of Soil Organic Matter Spatial Distribution in the Black Soil Region of Inner Mongolia

  • 摘要:
    目的 本文旨在揭示内蒙古黑土区土壤有机质(SOM)的空间分异规律、主控因子以及阈值效应,为黑土区土壤有机质培育和区域碳管理提供科学依据。
    方法 本研究以内蒙古东部黑土区为研究对象,采用随机森林(RF)模型与Shapley可解释性方法,对多源环境和土壤属性变量的影响进行了定量解析,并与地理加权回归(GWR)和多尺度地理加权回归(MGWR)模型进行对比。
    结果 结果表明,RF模型在预测精度(R2 = 0.747,RMSE = 1.561)和稳定性方面优于传统模型以及其他机器学习模型,能有效刻画SOM与环境因子之间的非线性关系。%IncMSE与平均绝对Shapley值(Mean |Shapley|)的双重度量结果一致识别出全氮、全磷、植被指数、年均气温、土壤湿度和年均降水为主导因子。SOM对这些因子的响应呈显著非线性和阈值效应,其中土壤湿度与年均降水表现为“倒U型”变化,适中湿润条件最有利于SOM积累。空间上,SOM整体呈“东北高-西南低”分布格局,高值区集中于通辽东部与呼伦贝尔南缘,与高植被覆盖和良好水热条件区域一致。
    结论 研究区SOM的空间格局主要受养分供给、植被覆盖与水热条件的协同驱动,不同预测变量在各自梯度上表现出非线性响应与阈值转折。

     

    Abstract:
    Objective The aims were to reveal the spatial distribution patterns, controlling factors, and threshold effects of soil organic matter (SOM) in the black soil region of Inner Mongolia, in order to provide scientific basis for the cultivation of SOM and regional carbon management in this area.
    Method The black soil area in the eastern part of Inner Mongolia was as the research object, a random forest (RF) model coupled with the Shapley additive explanation (SHAP) approach was employed to quantitatively assess the influence of multi-source environmental and soil attribute variables, with comparisons drawn against the geographically weighted regression (GWR) and multiscale geographically weighted regression (MGWR) models.
    Result The results demonstrated that the RF model outperformed traditional and other machine learning models in both predictive accuracy (R2 = 0.747, RMSE = 1.561) and stability, effectively capturing the nonlinear relationships between SOM and environmental factors. Consistent rankings from both %IncMSE and mean absolute Shapley value identified total nitrogen, total phosphorus, vegetation index, mean annual temperature, soil moisture, and mean annual precipitation as the primary determinants of SOM variation. The responses of SOM to those factors exhibited pronounced nonlinearity and threshold effects. Soil moisture and annual precipitation showed an inverted "U-shaped" relationship, indicating that moderate moisture conditions favored SOM accumulation. Spatially, SOM displayed a "high in the northeast-low in the southwest" pattern, with hotspots concentrated in eastern Tongliao and the southern margin of Hulunbuir, corresponding to areas of dense vegetation and favorable hydrothermal conditions.
    Conclusion These findings highlights that the spatial pattern of SOM in the study area is mainly driven by the synergy of nutrient supply, vegetation coverage and water and heat conditions. Different predictor variables exhibit nonlinear responses and threshold transitions at their respective gradients.

     

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