Process / pipelineQuantitative pedology and soil systems modeling
土壤成因模拟——土壤形成过程的定量模拟
土壤成因模拟是一种在农学和土壤科学中使用的定量方法,用于模拟土壤随时间形成和演化的过程。现代方法植根于汉斯·詹尼(Hans Jenny)1941年的因子框架——土壤是气候、生物、地形、母质和时间的函数——将这些概念性驱动因素转化为耦合的数值过程方程,使研究人员能够重建过去的土壤状态,并预测在不断变化的土地利用或气候情景下未来的土壤特性。
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来源
- Minasny, B., Finke, P., Stockmann, U., Vanwalleghem, T., & McBratney, A. B. (2015). Resolving the integral connection between pedogenesis and landscape evolution. Earth-Science Reviews, 150, 102–120. DOI: 10.1016/j.earscirev.2015.07.004 ↗
- Jenny, H. (1941). Factors of Soil Formation: A System of Quantitative Pedology. McGraw-Hill, New York. link ↗
如何引用本页
ScholarGate. (2026, June 3). Pedogenesis Modeling: Quantitative Simulation of Soil Formation Processes. ScholarGate. https://scholargate.app/zh/agronomy/pedogenesis-model
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