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Modeling phosphorus transport in a river under unsteady flow conditions.

机译:模拟非恒定流量条件下河流中的磷迁移。

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Phosphorus is the key nutrient for phytoplankton growth in water bodies; it has been identified as a source for the hypoxia problem in the Gulf of Mexico. The in-stream dynamics of phosphorus transport is complex and has not been understood well. In this study, a new model for phosphorus transport was developed to investigate within-channel river dynamics. This convective-dispersive model is coupled with hydrodynamics and sediment transport sub-models to simulate suspended sediment, total dissolved phosphorus, total phosphorus, and particulate phosphorus concentrations with changing flow conditions. It emphasizes sediment and phosphorus dynamics in unsteady flow conditions and differs from many previous solute transport studies conducted under steady-state flow conditions. The study also attempts to connect the structure of the bed sediment sub-model to the storage zone concept from previously conducted solute transport studies.; There exist possible problems of numerical dispersion and instability in the solutions, which may occur due to varying velocity under unsteady flow condition. To solve this problem, various numerical methods were tested and the implicit Lagrangian method was selected, which showed least numerical dispersion, given a computational grid size. The model is applied to a 55-km stretch of the River Swale in Yorkshire, UK, within the framework of the Generalized Likelihood Uncertainty Estimation (GLUE) methodology. The GLUE methodology is a Bayesian Monte Carlo simulation-based technique, in which multivariate information on the model system can be easily integrated. Utilizing this property, sequential conditioning corresponding to simulation dependency was carried out. In-stream dynamics was identified by comparing the model predicted results with the observed variables. Various forms of phosphorus flux between the flow and sediment were also simulated, showing the effect of sediment particle size on phosphorus transport. Finally, model parameter sensitivity analysis was carried out within the GLUE framework. Results indicate that the in-stream dynamics of phosphorus can be successfully investigated by the modeling approach.
机译:磷是水体浮游植物生长的关键营养素。它被认为是墨西哥湾缺氧问题的根源。磷运输的流动力学是复杂的,尚未被很好地理解。在这项研究中,开发了磷运输的新模型,以研究河道内河道动力学。该对流扩散模型与流体力学和泥沙输送子模型结合使用,可模拟随流动条件变化而产生的悬浮泥沙,总溶解磷,总磷和颗粒磷浓度。它强调了非稳态流动条件下的沉积物和磷动力学,并且不同于先前在稳态流动条件下进行的许多溶质运移研究。该研究还试图通过先前进行的溶质运移研究将床沉积物子模型的结构与存储区概念联系起来。解决方案中可能存在数值离散和不稳定性的问题,这些问题可能是由于在非恒定流动条件下速度变化而引起的。为了解决这个问题,测试了各种数值方法,并选择了隐式拉格朗日方法,该方法在给定计算网格大小的情况下,数值离散最小。该模型在广义似然不确定性估计(GLUE)方法的框架内,应用于英国约克郡55英里的瑞尔沃斯河(River Swale)。 GLUE方法是一种基于贝叶斯蒙特卡洛模拟的技术,可以轻松地集成模型系统上的多变量信息。利用该特性,进行了与仿真依赖性相对应的顺序条件。通过将模型的预测结果与观察到的变量进行比较来识别流内动态。还模拟了流与沉积物之间各种形式的磷通量,显示了沉积物粒径对磷迁移的影响。最后,在GLUE框架内进行了模型参数敏感性分析。结果表明,通过建模方法可以成功地研究磷的流内动力学。

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