Home | Contact Us | Sitemap | 中文 | CAS | Director's Email
 
Location:Home > Papers > Recent Papers
Fluoride release from carbonate-rich fluorapatite during managed aquifer recharge: Model-based development of mitigation strategies TEXT SIZE: A A A
Fluoride-bearing apatite minerals such as fluorapatite (FAP: Ca-10(PO4)(5)F-2) and related carbonate-rich fluorapatites (CFA: Ca-10(PO4)(5)(CO3,F)F-2), which occur ubiquitously as trace components of rocks and sediments, may act as sources for geogenic groundwater fluoride contamination. CFA dissolution often occurs in conjunction with declining dissolved calcium concentrations. Therefore, managed aquifer recharge (MAR) operations using deionised or low calcium source water are at risk of disturbing the naturally persisting geochemical equilibrium between CFA and the ambient groundwater and induce fluoride mobilisation. In this study, we employ reactive transport modelling to investigate how an engineered manipulation of the MAR source water composition might mitigate such groundwater fluoride contamination. Based on a previously developed and calibrated model for Australia's largest groundwater replenishment operation, we investigate the efficiency of (i) raising aqueous calcium concentration through the addition of CaCl2 or Ca(OH)(2) amendment, (ii) raising aqueous sodium concentrations through the addition of NaCl or sea salt amendment and (iii) raising the pH. The modelling results illustrate in detail how the geochemical zonation around injection boreholes evolves over time and how this affects fluoride release and attenuation for the different amendment types. Treatments involving the addition of calcium and sodium in the source water are both found to be effective at reducing maximum groundwater fluoride concentrations during MAR, with calcium generally producing the greatest reduction in maximum fluoride concentrations. In contrast, increasing the injectate pH was found to be inefficient in reducing fluoride concentrations significantly due to the strong pH buffering effect of the aquifer sediments. (C) 2021 Elsevier Ltd. All rights reserved.
 

Publication name

 WATER RESEARCH Volume: 193 Article Number: 116880 DOI: 10.1016/j.watres.2021.116880 Published: APR 1 2021

Author(s)

 Schafer, David; Sun, Jing; Jamieson, James; Siade, Adam; Atteia, Olivier; Seibert, Simone; Higginson, Simon; Prommer, Henning

Corresponding author(s) 

 Prommer, Henning 
 Henning.Prommer@csiro.au  
 -Univ Western Australia, Sch Earth Sci, Crawley, WA 6009, Australia
 -CSIRO Land & Water, Private Bag 5, Wembley, WA 6913, Australia
 -Natl Ctr Groundwater Res & Training, GPO Box 2100, Adelaide, SA 5001, Australia

View here for the details 

Copyright © 2021 Institute Of Geochemistry, Chinese Academy of Sciences All Rights Reserved.
Address: 99 West Lincheng Road, Guanshanhu District, Guiyang, Guizhou Province 550081, P.R.China
Tel: +86-851-85895239 Fax: +86-851-85895239 Email: web_en@mail.gyig.ac.cn