Theoretical Ecosystem Ecology, Department of Biogeochemical Processes, Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
Theoretical Ecosystem Ecology, Department of Biogeochemical Processes, Max Planck Institute for Biogeochemistry, 07745 Jena, Germany.
Proc Natl Acad Sci U S A. 2018 Feb 6;115(6):1150-1155. doi: 10.1073/pnas.1705296115. Epub 2018 Jan 22.
Many processes in nature are modeled using compartmental systems (reservoir/pool/box systems). Usually, they are expressed as a set of first-order differential equations describing the transfer of matter across a network of compartments. The concepts of age of matter in compartments and the time required for particles to transit the system are important diagnostics of these models with applications to a wide range of scientific questions. Until now, explicit formulas for transit-time and age distributions of nonlinear time-dependent compartmental systems were not available. We compute densities for these types of systems under the assumption of well-mixed compartments. Assuming that a solution of the nonlinear system is available at least numerically, we show how to construct a linear time-dependent system with the same solution trajectory. We demonstrate how to exploit this solution to compute transit-time and age distributions in dependence on given start values and initial age distributions. Furthermore, we derive equations for the time evolution of quantiles and moments of the age distributions. Our results generalize available density formulas for the linear time-independent case and mean-age formulas for the linear time-dependent case. As an example, we apply our formulas to a nonlinear and a linear version of a simple global carbon cycle model driven by a time-dependent input signal which represents fossil fuel additions. We derive time-dependent age distributions for all compartments and calculate the time it takes to remove fossil carbon in a business-as-usual scenario.
许多自然过程都是通过隔室系统(储库/池/箱系统)建模的。通常,它们被表示为一组一阶微分方程,描述物质在隔室网络中的传递。物质在隔室中的年龄概念和粒子穿越系统所需的时间是这些模型的重要诊断指标,适用于广泛的科学问题。到目前为止,还没有针对非线性时变隔室系统的传输时间和年龄分布的显式公式。我们在隔室充分混合的假设下计算这些类型系统的密度。假设非线性系统的解至少可以数值获得,我们展示如何构建具有相同解轨迹的线性时变系统。我们演示如何利用该解来计算给定起始值和初始年龄分布的传输时间和年龄分布。此外,我们还推导出了年龄分布的分位数和矩的时间演化方程。我们的结果推广了线性时不变情况的可用密度公式和线性时变情况的平均年龄公式。作为一个例子,我们将我们的公式应用于一个由时变输入信号驱动的简单全球碳循环模型的非线性和线性版本,该输入信号代表化石燃料的添加。我们为所有隔室推导了时变年龄分布,并计算了在常规情景下去除化石碳所需的时间。