Articles | Volume 26, issue 1
https://doi.org/10.5194/hess-26-183-2022
https://doi.org/10.5194/hess-26-183-2022
Research article
 | 
14 Jan 2022
Research article |  | 14 Jan 2022

Implications of variations in stream specific conductivity for estimating baseflow using chemical mass balance and calibrated hydrograph techniques

Ian Cartwright

Viewed

Total article views: 2,301 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,685 557 59 2,301 142 33 44
  • HTML: 1,685
  • PDF: 557
  • XML: 59
  • Total: 2,301
  • Supplement: 142
  • BibTeX: 33
  • EndNote: 44
Views and downloads (calculated since 23 Sep 2021)
Cumulative views and downloads (calculated since 23 Sep 2021)

Viewed (geographical distribution)

Total article views: 2,301 (including HTML, PDF, and XML) Thereof 2,136 with geography defined and 165 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
Using specific conductivity (SC) to estimate groundwater inflow to rivers is complicated by bank return waters, interflow, and flows off floodplains contributing to baseflow in all but the driest years. Using the maximum SC of the river in dry years to estimate the SC of groundwater produces the best baseflow vs. streamflow trends. The variable composition of baseflow hinders calibration of hydrograph-based techniques to estimate groundwater inflows.