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SIL Proceedings, 1922-2010
Internationale Vereinigung für Theoretische und Angewandte Limnologie: Verhandlungen
Volume 29, 2006 - Issue 3
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Original Articles

Is Rhodamine WT conservative in small stream studies? Results from upland and lowland reaches of a tropical stream

Pages 1645-1650 | Published online: 01 Dec 2017

References

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  • Bencala, K.E. & Walters, R.A., 1983: Simulation of solute transport in a mountain pool-and-riffle stream &mdash a transient storage model. — Water Resour. Res. 19: 718.
  • Cobb, E.D. & Bailey, J.F., 1965: Measurement of discharge by dye-dilution methods. — US Geol. Survey Surface Water Techniques, Book 1, Chapter 14.
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  • Runkel, R.L. & Chapra, S.C., 1994: An efficient numerical solution of the transient storage equations for solute transport in small streams &mdash reply. — Water Resour. Res. 30: 2863–2865.
  • Runkel, R.L., Mcknight, D.M. & Andrews, E.D., 1998: Analysis of transient storage subject to unsteady flow — diel flow variation in an antarctic stream. — J. N. Am. Benthol. Soc. 17: 143–154.
  • Sabatini, D.A. & Austin, T.A., 1991: Characteristics of Rhodamine WT and Fluorescein as adsorbing ground-water tracers. — Ground Water 29: 341.
  • Smart, P.L. & Laidlaw, I.M.S., 1977: An evaluation of some fluorescent dyes for water tracing. — Water Resour. Res. 13: 15–33.
  • White, D.S., 1993: Perspectives on defining and delimiting hyporheic zones. — J. N. Am. Benthol. Soc. 12: 61–69.

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