Transient hydrological conditions implied by chloride mass balance in southeast Australian rivers

Cartwright, Ian, Gilfedder, Benjamin and Hofmann, Harald (2013) Transient hydrological conditions implied by chloride mass balance in southeast Australian rivers. Chemical Geology, 357 29-40. doi:10.1016/j.chemgeo.2013.08.028


Author Cartwright, Ian
Gilfedder, Benjamin
Hofmann, Harald
Title Transient hydrological conditions implied by chloride mass balance in southeast Australian rivers
Journal name Chemical Geology   Check publisher's open access policy
ISSN 0009-2541
1872-6836
Publication date 2013-10-24
Sub-type Article (original research)
DOI 10.1016/j.chemgeo.2013.08.028
Open Access Status Not Open Access
Volume 357
Start page 29
End page 40
Total pages 12
Place of publication Amsterdam, The Netherlands
Publisher Elsevier BV
Language eng
Subject 1906 Geochemistry and Petrology
1907 Geology
Abstract A robust correlation between electrical conductivity (EC) values and Cl concentrations in river water from southeast Australia allows detailed Cl fluxes to be calculated from continuous EC and river discharge records. Many Victorian rivers export significantly more Cl than is delivered to their catchments by rainfall. Cl* is defined as the mass of Cl exported in the rivers relative to that input by rainfall over a multi-year period (Cl*. =. 100% indicates that the river exports the same mass of Cl as is input by rainfall). There is a systematic relationship between catchment type and Cl*. Rivers draining cleared plains have Cl* values between 50 and 750%, rivers draining volcanic plains have Cl* values of 770-1600%, whereas rivers with large forested upland catchments have Cl* values of 50-110%. These values are minima as they do not account for Cl exported by groundwater from the catchments. The calculations are based on long-term (up to 22. year) records that span drought and high rainfall periods. The magnitude of Cl* is far higher than can be explained by errors in the calculations or variability in rainfall and runoff, and Cl/Br ratios preclude halite dissolution as a source of Cl. The excess Cl reflects hydrological changes in the catchments. Land clearing on the cleared plains has caused the rise of regional water tables which results in the export of Cl from saline groundwater via increased baseflow to the river systems. Drainage systems on the volcanic plains are re-establishing following impoundment by recent (<. 4.5. Ma) lava flows; Cl which accumulated in shallow groundwater around saline lakes and marshes developed on these volcanic plains is now being exported via the rivers. The upland catchments have undergone less landscape change and may be in chemical balance. The methodology outlined here provides a straightforward assessment of whether catchments are in chemical balance that may in turn indicate whether they are undergoing hydrological changes.
Keyword Groundwater-surface water interactions
Landscape change
Salinity
Q-Index Code C1
Q-Index Status Provisional Code
Institutional Status Non-UQ

Document type: Journal Article
Sub-type: Article (original research)
Collections: Non HERDC
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Created: Thu, 13 Mar 2014, 23:39:05 EST by Ashleigh Paroz on behalf of School of Earth Sciences