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An analytical phytoplankton model and its application in the tidal freshwater James River

机译:一种分析浮游植物模型及其在潮汐淡水湖河河流的应用

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This study constructs an analytical model to understand the phytoplankton dynamics in a one-dimensional system by integrating physical and biological processes. We present an analytical solution of phytoplankton distribution along the longitudinal direction of a tidal river. The solution has two components: water age and accumulative growth. The water age represents the overall effect of physical transport due to advection, while the accumulative growth represents the accumulation of phytoplankton biomass due to biological processes during the transport. In addition, an alternative solution with nonlinear reaction term is given to account for the feedback mechanism of nonlinear processes that affect phytoplankton growth rate. The nonlinear reaction term can be also used to approximate the effect of physical mixing on phytoplankton distribution. The analytical solutions can be further used to predict the temporal variation and spatial distribution of phytoplankton along the tidal river. They also serve as a mathematical tool to unite different field phytoplankton observations. We applied the model in the Tidal Freshwater Region (TFR) of James River under different dynamic conditions and the model results match well with the observations, which validates the theory on different time scales. Furthermore, an analysis is conducted for the Local Chlorophyll-a Maximum (LCM) in the TFR. It shows that the condition for LCM is biologically controlled, but its location is regulated by river flow and river geomorphology.
机译:该研究通过整合物理和生物过程来构建一个分析模型,以了解一维系统中的浮游植物动态。我们展示了沿潮汐河流的纵向浮游植物分布的分析解决方案。该溶液具有两种组分:水时期和累积增长。水时期代表了由于平整导致物理运输的总体效果,而累积增长是由于在运输过程中由于生物学过程而产生的浮游植物生物量的积累。另外,给出具有非线性反应项的替代溶液,以考虑影响浮游植物生长速率的非线性过程的反馈机制。非线性反应项也可用于近似物体混合对浮游植物分布的影响。分析解决方案可以进一步用于预测沿潮汐河流的时间变化和浮游植物的空间分布。它们还作为一个统一的不同场植物观测的数学工具。在不同的动态条件下,我们在詹姆斯河的潮汐淡水区(TFR)中应用了模型,模型结果与观察结果相匹配,验证了不同时间尺度的理论。此外,在TFR中对局部叶绿素 - 最大(LCM)进行分析。它表明,LCM的条件是生物控制的,但其位置由河流和河流岩层调节。

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