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An analytical model of soil organic carbon dynamics based on a simple'hockey stick' function

机译:基于简单“曲棍球杆”功能的土壤有机碳动力学分析模型

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摘要

We developed a simple analytical model for carbon and nitrogen dynamics in soils. Description of the soil C and N dynamics focus on the total carbon residue function, R, defined as the fraction of original plant carbon input remaining in the soil as a function of time, and nitrogen concentration function, N, defined as the N concentration of the carbon residue as a function of R. A simple two-parameter function, R = Exp(-(kt)(alpha)), was used for total carbon residue function. N concentration of carbon residue is derived to be a linear function of R. We tested our model with data reported in the literature. The model parameters (k and alpha) were calculated from independently determined gross turnover time and C-14 age of soil organic carbon. Our model accurately predicts C and N dynamics in response to fertilization and manure application for time periods ranging from a few months to more than 150 years.
机译:我们为土壤中的碳和氮动力学开发了一个简单的分析模型。土壤C和N动态的描述着重于总碳残留量函数R(定义为土壤中残留的原始植物碳输入随时间的函数)和氮浓度函数N(定义为土壤中N的浓度)。碳残基作为R的函数。简单的两参数函数R = Exp(-(kt)α)用于总碳残基函数。碳残留量的N浓度是R的线性函数。我们用文献中报道的数据测试了我们的模型。根据独立确定的总周转时间和土壤有机碳的C-14年龄计算模型参数(k和alpha)。我们的模型可以准确预测碳和氮的动态变化,其响应时间从几个月到150多年不等。

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