Water | |
Quantifying Reaeration Rates in Alpine Streams Using Deliberate Gas Tracer Experiments | |
Andrew Benson2  Matthew Zane1  Timothy E. Becker1  Ate Visser4  Stephanie H. Uriostegui1  Elizabeth DeRubeis3  Jean E. Moran3  Bradley K. Esser4  | |
[1] Department of Earth Science, University of California, Santa Barbara, CA 93106, USA; E-Mails:;Program of Environmental Studies, University of California, Santa Barbara, CA 93106, USA; E-Mail:;Department of Earth and Environmental Sciences, California State University East Bay, Hayward, CA 94542, USA; E-Mails:;Chemical Science Division, Lawrence Livermore National Laboratory, Livermore, CA 94551, USA; E-Mails: | |
关键词: reaeration; field tracer experiment; sulfur hexafluoride; xenon; alpine stream; dissolved oxygen; | |
DOI : 10.3390/w6041013 | |
来源: mdpi | |
【 摘 要 】
Gas exchange across the air-water interface is a critical process that maintains adequate dissolved oxygen (DO) in the water column to support life. Oxygen reaeration rates can be accurately measured using deliberate gas tracers, like sulfur hexafluoride (SF6) or xenon (Xe). Two continuous release experiments were conducted in different creeks in the Sierra Nevada of California: Sagehen Creek in September, 2009, using SF6 and Martis Creek in August, 2012, using both SF6 and Xe. Measuring gas loss along the creek, which was approximated with the one-dimensional advection-dispersion equation, allows for the estimation of the SF6 or Xe reaeration coefficient (
【 授权许可】
CC BY
© 2014 by the authors; licensee MDPI, Basel, Switzerland.
【 预 览 】
Files | Size | Format | View |
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RO202003190026523ZK.pdf | 1691KB | download |