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在处理生活污水的热带水平潜流人工湿地中进行的反应传输模拟。

Reactive transport simulation in a tropical horizontal subsurface flow constructed wetland treating domestic wastewater.

机构信息

UNESCO-IHE, Institute for Water Education, P.O. BOX 3015, 2601DA Delft, The Netherlands.

出版信息

Sci Total Environ. 2013 Apr 1;449:309-19. doi: 10.1016/j.scitotenv.2013.01.069. Epub 2013 Feb 26.

DOI:10.1016/j.scitotenv.2013.01.069
PMID:23434579
Abstract

A promising approach to the simulation of flow and conversions in the complex environment of horizontal subsurface flow constructed wetlands (HSSF-CWs) is the use of reactive transport models, in which the transport equation is solved together with microbial growth and mass-balance equations for substrate transformation and degradation. In this study, a tropical pilot scale HSSF-CW is simulated in the recently developed CWM1-RETRASO mechanistic model. The model predicts organic matter, nitrogen and sulfur effluent concentrations and their reaction rates within the HSSF-CW. Simulations demonstrated that these reactions took place simultaneously in the same (fermentation, methanogenesis and sulfate reduction) or at different (aerobic, anoxic and anaerobic) locations. Anaerobic reactions occurred over large areas of the simulated HSSF-CW and contributed (on average) to the majority (68%) of the COD removal, compared to aerobic (38%) and anoxic (1%) reactions. To understand the effort and compare computing resources needed for the application of a mechanistic model, the CWM1-RETRASO simulation is compared to a process-based, semi-mechanistic model, run with the same data. CWM1-RETRASO demonstrated the interaction of components within the wetland in a better way, i.e. concentrations of microbial functional groups, their competition for substrates and the formation of intermediary products within the wetland. The CWM1-RETRASO model is thus suitable for simulations aimed at a better understanding of the CW system transformation and degradation processes. However, the model does not support biofilm-based modeling, and it is expensive in computing and time resources required to perform the simulations.

摘要

在水平潜流人工湿地 (HSSF-CWs) 这种复杂环境中模拟流动和转化,一种很有前途的方法是使用反应传输模型,其中将传输方程与微生物生长以及基质转化和降解的质量平衡方程一起求解。在这项研究中,使用最近开发的 CWM1-RETRASO 机理模型对热带中试规模的 HSSF-CW 进行了模拟。该模型预测了 HSSF-CW 中的有机物、氮和硫的出水浓度及其反应速率。模拟表明,这些反应同时发生在相同的(发酵、产甲烷和硫酸盐还原)或不同的(好氧、缺氧和厌氧)位置。厌氧反应发生在模拟 HSSF-CW 的大部分区域,对 COD 去除的贡献(平均而言)比好氧(38%)和缺氧(1%)反应更大。为了了解应用机理模型所需的努力和比较计算资源,将 CWM1-RETRASO 模拟与使用相同数据运行的基于过程的半机理模型进行了比较。CWM1-RETRASO 更好地展示了湿地内各组件之间的相互作用,即微生物功能群的浓度、它们对基质的竞争以及湿地内中间产物的形成。因此,CWM1-RETRASO 模型适合用于模拟,旨在更好地理解 CW 系统的转化和降解过程。然而,该模型不支持基于生物膜的建模,并且在进行模拟时需要大量的计算和时间资源。

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