Adsorption And Desorption Characteristics Of Fluoride In The Calcareous And Siliceous Sand Sheet Aquifers Of South-west Victoria, Australia
Price
Free (open access)
Transaction
Volume
111
Pages
16
Page Range
159 - 174
Published
2008
Size
589 kb
Paper DOI
10.2495/WP080161
Copyright
WIT Press
Author(s)
S. A. Salzman, G. Allinson, F. Stagnitti, R. J. Hill, L. Thwaites, D. Ierodiaconou, R. Carr, J. Sherwood & V. Versace
Abstract
This study assessed the sustainability of utilising groundwater systems to manage an aluminium smelter’s fluoridated trade wastewater stream. Replacing ocean discharge of the wastewater with land irrigation is one option. Using a groundwater model (developed using MODFLOW incorporating parameter estimation software (PEST-ASP)), we found that most of the groundwater flow takes place through surface sands. Fluoride is adsorbed in these sands during the drier summer months, but desorption is rapid when winter rain flushes the aquifer. Underlying clays and other layers prevent significant contamination of the deeper aquifer. Keywords: groundwater flow, fluoridated trade wastewater, adsorbed, desorption. 1 Introduction Fluoride is considered to be the third most important air pollutant after sulphur dioxide and ozone because it is highly toxic to some plant species [1]. Most fluoride in or on terrestrial plants results from aerial fluoride, but small amounts will be taken up from irrigation water [2], and soluble fluoride salts can be taken
Keywords
groundwater flow, fluoridated trade wastewater, adsorbed, desorption.