Articles | Volume 12, issue 19
https://doi.org/10.5194/bg-12-5597-2015
https://doi.org/10.5194/bg-12-5597-2015
Research article
 | 
01 Oct 2015
Research article |  | 01 Oct 2015

Seasonal hydrology drives rapid shifts in the flux and composition of dissolved and particulate organic carbon and major and trace ions in the Fraser River, Canada

B. M. Voss, B. Peucker-Ehrenbrink, T. I. Eglinton, R. G. M. Spencer, E. Bulygina, V. Galy, C. H. Lamborg, P. M. Ganguli, D. B. Montluçon, S. Marsh, S. L. Gillies, J. Fanslau, A. Epp, and R. Luymes

Viewed

Total article views: 4,112 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,791 1,845 476 4,112 145 85 99
  • HTML: 1,791
  • PDF: 1,845
  • XML: 476
  • Total: 4,112
  • Supplement: 145
  • BibTeX: 85
  • EndNote: 99
Views and downloads (calculated since 21 May 2015)
Cumulative views and downloads (calculated since 21 May 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Discussed (final revised paper)

Latest update: 27 Mar 2024
Download
Short summary
This study presents seasonal cycles of organic matter concentration and composition in the Fraser River. Dissolved organic matter patterns are linked to flushing of shallow soil layers during spring snowmelt and fall rain events. The preliminary Hg data set indicates significant changes in concentrations during the spring freshet. Organic carbon export, as both area-normalized yield and the proportion of basin primary productivity, in the Fraser River is typical of large rivers globally.
Altmetrics
Final-revised paper
Preprint