Controlling mechanisms for the trace metals, (Cu, Zn, Cd, Fe, Co and Ni) in anoxic sea water in Saanich Inlet, British Columbia, Canada
Author:
Publisher
Springer Science and Business Media LLC
Subject
Water Science and Technology,Oceanography
Link
http://link.springer.com/content/pdf/10.1007/BF02843983.pdf
Reference28 articles.
1. Anderson, J.J. and Devol, A.H., 1973. Deep water renewal in Saanich Inlet, an intermittently anoxic basin.Estuarine and Coastal Marine Science I: 1–10.
2. Boulegue, K. and G. Michard, 1978. Costantes de formation des ions polysulfures S 6 2− , S 5 2− , et S 4 2− en Phase Aqueuse.Journal Francais d’Hydrologie 9: 27–34 (in French).
3. Boulegue, J. and G. Michard 1979. Sulfur Speciations and Redox processes in Reducing Environments.In: Chemical Modeling in Aqueous Systems, (Jenne, ed.) ACS Symposium Series 93. Washington, DC, pp. 25–50.
4. Boulegue, J., 1983. Trace Metals (Fe, Cu, Zn, Cd) in Anoxic Environments.In: C.S. Wong et al. (Editors), Trace Metals In Sea Water. Plenum Press. New York, pp. 563–579.
5. Cline J.D. 1969. Spectrophotometric determination of hydrogen sulfide in natural waters.Limnology and Oceanography 14: 454–458.
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