Authors: Caselles-Osorio, Aracelly¹; Porta, Alessandro; Porras, Montserrat; García, Joan²

Source: Water, Air, and Soil Pollution, Volume 183, Numbers 1-4, July 2007 , pp. 367-375(9)

Publisher: Springer

Abstract:

Two identical experimental subsurface-flow constructed wetlands were operated at relatively high organic loading rates (23 g COD m⁻² day⁻¹) for 4 months to evaluate their relative ability to remove either dissolved organic carbon (glucose, considered to be a readily biodegradable substrate) or particulate organic carbon (starch, considered to be a slowly biodegradable substrate). The systems were built using plastic containers (0.93 m long, 0.59 m wide and 0.52 m high) that were filled with an 0.35 m layer of wetted gravel (D₆₀ = 3.5 mm, uniformity coefficient C_u = D₆₀/D₁₀ = 1.7) and the water level was maintained at 0.05 m under the gravel surface to give a water depth of 0.30 m. The results indicated that there was no significant difference in COD removal between the two systems. Both systems generally had COD removal rates of over 90%, which is quite high if the heavy load applied is taken into account. The removal of ammonium was greater in the glucose-fed system (57%) in comparison with the starch-fed system (43%). Based on mass balance calculations and stoichiometric relationships, it was estimated that denitrification and sulphate reduction were minor pathways for the removal of organic matter. Indirect observations allowed to assume that methanogenesis made a highly significant contribution to the removal of organic matter.

Keywords: Horizontal flow; Microbial growth; Particle size; Performance; Reed beds

Document Type: Research article

DOI: http://dx.doi.org/10.1007/s11270-007-9385-1

Affiliations: 1: Email: acaselles@uniatlantico.edu.co 2: Email: joan.garcia@upc.edu

Publication date: 2007-07-01

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