4.6 Article

Effects of evapotranspiration on treatment performance in constructed wetlands: Experimental studies and modeling

Journal

ECOLOGICAL ENGINEERING
Volume 71, Issue -, Pages 394-400

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.ecoleng.2014.07.052

Keywords

Constructed wetlands; Evapotranspiration; Tracer tests; Modeling; Typha latifolia; Cattails

Funding

  1. United States Department of Energy (USDOE) through the National Energy Technology Laboratory [DE-NT0005682]
  2. agency of the United States Government

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Evapotranspiration (ET) can affect treatment performance on constructed wetlands by enhancing constituent transport through the hydrosoil where treatment reactions occur. Additionally, ET can decrease volumetric flow thereby increasing hydraulic retention time and increasing concentrations of dissolved constituents. This research aims to assess the net effects of water loss attributed to ET on constructed wetland performance and determine the significance of plant transpiration on vertical transport of constituents. A flowing wetland lysimeter constructed using 265-L storage containers filled with sand and Typha latifolia was used to record ET and determine crop coefficient during summer 2011. Results indicate that ET from the lysimeter was 2.5 times greater than calculated reference ET (K-c = 2.5; R-2 = 0.96). The calculated crop coefficient was used in conjunction with a first-order tank-in-series model to predict removal of a conservative constituent (k= 0.2 d(-1)) and readily treatable constituent (k =1.2 d(-1)) in a constructed wetland (20 cm and 40 cm water depths, 4-day nominal HRT, and 100 mg L-1 constituent loading) operating under a range of ET (0, 10, 20, and 30 mm d(-1)). The model predicts that removal efficiency of the conservative constituent decreases with increasing ET, while removal efficiency of the readily treatable constituent increases with increasing ET. In addition, eight vertical tracer tests were performed on wetland cells with either trimmed or untrimmed T. latifolia to measure transport time of tracer solution from the water surface to a depth of 5 cm. Mean tracer arrival time differed significantly (p =1.2 x 10(-8)) between the untrimmed and trimmed cells (104 min versus 450 min, respectively) demonstrating that plant transpiration contributes significantly to vertical flow through hydrosoil. (C) 2014 Elsevier B.V. All rights reserved.

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