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    题名: Integrated modeling of groundwater and surface water interactions in a manmade wetland
    作者: 葉高次;Huang, Guobiao;Yeh, Gour-Tsyh
    贡献者: 地球科學學院應用地質研究所
    关键词: Approximation;Aquifers;Data;Diffusion waves;Field tests;Fluxes;Groundwater;Groundwater levels;Hydraulic structures;Hydrodynamics;Hydrologic processes;Hydrology;Integrated approach;Integrated model;Levees;Manmade wetland;Mathematical models;Model matching;Modelling;Nutrient removal;Overland flow;Parameters;Phosphorus;Phosphorus removal;Physics;Removal;Scale (ratio);Seepage;Seepage loss;Storms;Stormwater;Subsurface flow;Surface and groundwater interaction;Surface water;Surface-groundwater relations;Three dimensional flow;Two dimensional flow;Uptake;WASH123D;Water flow;Water levels;Wetlands
    日期: 2012-10-01
    上传时间: 2026-04-23 15:00:14 (UTC+8)
    出版者: Chinese Geoscience Union;Taiwan: 中華民國地球科學學會
    摘要: 摘要: A manmade pilot wetland in south Florida, the Everglades Nutrient Removal (ENR) project, was modeled with a physics-based integrated approach using WASH123D (Yeh et al. 2006). Storm water is routed into the treatment wetland for phosphorus removal by plant and sediment uptake. It overlies a highly permeable surficial groundwater aquifer. Strong surface water and groundwater interactions are a key component of the hydrologic processes. The site has extensive field measurement and monitoring tools that provide point scale and distributed data on surface water levels, groundwater levels, and the physical range of hydraulic parameters and hydrologic fluxes. Previous hydrologic and hydrodynamic modeling studies have treated seepage losses empirically by some simple regression equations and, only surface water flows are modeled in detail. Several years of operational data are available and were used in model historical matching and validation. The validity of a diffusion wave approximation for two-dimensional overland flow (in the region with very flat topography) was also tested. The uniqueness of this modeling study is notable for (1) the point scale and distributed comparison of model results with observed data; (2) model parameters based on available field test data; and (3) water flows in the study area include two-dimensional overland flow, hydraulic structures/levees, three-dimensional subsurface flow and one-dimensional canal flow and their interactions. This study demonstrates the need and the utility of a physics-based modeling approach for strong surface water and groundwater interactions.
    出版者: Taiwan: 中華民國地球科學學會
    出版日期: 2012-10-01
    出處: TAO : Terrestrial, atmospheric, and oceanic sciences, 2012-10, Vol.23 (5), p.501-511
    資源來源: Chinese Electronic Periodical Services (CEPS)
    版權: 2012. This work is licensed under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
    識別號: ISSN: 1017-0839
    識別號: ISSN: 2223-8964
    識別號: ISSN: 2311-7680
    識別號: EISSN: 2311-7680
    識別號: DOI: 10.3319/TAO.2012.04.17.02(WMH)
    显示于类别:[應用地質研究所] 期刊論文

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