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A numerical tool to integrate biophysical diversity of a large regulated river: hydrobiogeochemical bases. The case of the Garonne River (France)

机译:整合一条大型调节河生物物理多样性的数值工具:水生地球化学基地。加龙河(法国)

摘要

This article presents the bases of a hydrobiogeochemical model of the Garonne River (southwest France) which has been developed to integrate physical and biological processes during summer low-water periods. The physical part of this model is composed of a one-dimensional unsteady hydrodynamic model, allowing the resolution of the Saint-Venant equations, and a transport model which simulates downstream changes in solute concentrations. Biogeochemical processes are considered through the definition of functional compartments which make up the channel bed. These different compartments are defined both by the organisms involved in the solute transformation processes and by the physical and hydraulic characteristics of their habitat. Integration of these functional compartments within the model required investigations at different scales. The scale at which biological processes take place ranges from millimetres to metres. The scale of a reach, at which organization of the functional compartments along the river can be linked to hydrodynamic and morphological characteristics, ranges from 500 m to several kilometres. The regional scale is that at which homogeneous reaches can be integrated. A feedback between numerical results and field experiments has allowed improvements to in situ measurement to increase modelling accuracy. For example, the model allows estimation of variables, such as fluxes, that are difficult to measure in situ. The developed model can integrate various functional compartments and their biogeochemical functioning. Two application examples, focused on dissolved inorganic nitrogen, are presented in order to illustrate the numerical tool functioning: integration of equations on nitrification processes in the water body, and integration of consumption/production terms on epilithic biofilm resulting from in situ experimental mean values. The model we have developed constitutes a promising analytical tool that will be able to integrate previous and future studies.
机译:本文介绍了加龙河(法国西南部)的水生地球化学模型的基础,该模型已被开发为整合夏季低水时期的物理和生物过程。该模型的物理部分由一维非定常流体动力学模型(可解决Saint-Venant方程的解析)和模拟下游溶质浓度变化的输运模型组成。通过定义组成通道床的功能区室来考虑生物地球化学过程。这些不同的区室由溶质转化过程中涉及的生物及其栖息地的物理和水力特征共同定义。这些功能隔室在模型中的集成要求进行不同规模的研究。发生生物过程的规模范围从毫米到米。沿河功能区的组织可以与水动力和形态特征联系起来的范围为500 m至几公里。区域规模是可以整合均质河段的规模。数值结果和现场实验之间的反馈使原位测量得以改进,从而提高了建模精度。例如,该模型允许估算难以现场测量的变量(例如通量)。所开发的模型可以整合各种功能区室及其生物地球化学功能。为了说明数值工具的功能,提出了两个针对溶解无机氮的应用实例:水体硝化过程方程的积分,以及原位实验平均值在表层生物膜上的消耗/生产条件的积分。我们开发的模型构成了一个有前途的分析工具,将能够整合以前和将来的研究。

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