The hydrochemistry of the Narrabri Formation, the shallow aquifer system of the alluvial fan of the Gwydir River (NSW, Australia), is analyzed to better understand the hydrogeological processes involved in aquifer recharge, and to set up future management options that preserve the quantity and quality of water resources. Results show that groundwater hydrochemistry in this alluvial aquifer is mainly controlled by silicate weathering and cation exchange. However, salt remobilization in specific sedimentary layers within this alluvial fan deposit may locally increase groundwater salinity. Mixing between stream leakage and aquifer groundwater controls the hydrochemistry of water resources and produces a decrease in its salinity, which is beneficial for human uses. (C) 2013 The Authors. Published by Elsevier B.V.
|Number of pages||4|
|Journal||Procedia earth and Planetary Science|
|Publication status||Published - 2013|
|Event||14th International Symposium on Water-Rock Interaction (WRI) - Avignon, France|
Duration: 9 Jun 2013 → 14 Jun 2013
Bibliographical noteCopyright the Author(s) 2013. Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.
- alluvial aquifer
- Gwydir River