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The nature and distribution of the suspended load of the middle Tay Estuary

Published online by Cambridge University Press:  05 December 2011

Fred H. Hubbard
Affiliation:
Department of Geology, University of Dundee, Dundee DD1 4HN, U.K.
Majid H. A. Hashim
Affiliation:
Faculty of Meteorology and Environmental Studies, King Abdulaziz University, Jeddah, Kingdom of Saudi Arabia
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Synopsis

The suspended loads at three stations in the middle estuary of the River Tay have been analysed monthly, at low and high water of the spring tides, over the period June 1983 to May 1984. Major mineral modal analyses were derived from bulk and mineral oxide analyses. The concentrations in the suspended loads of the trace metals Cr, Cu, Pb and Zn were determined. An efficient circulatory system operates within the middle estuary which largely retains the suspended loads acquired from the inner estuary, even at seasonal periods of high influx. The major mineral assemblage is quartz, chlorite, illite and kaolinite. There is some preferential landward return of quartz and chlorite. Chromium has an association with chlorite, while copper, lead and zinc seem linked with suspended particulate organic matter which, at least in part, is derived from sewage disposal into the estuary. Dissolved zinc is associated with dissolved organic matter.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1987

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References

Al-Dabbas, M. A. M. 1980. An examination of shell fragment distributions and geochemical features of Mytilus edulis in the Tay Estuary. Ph.D. Thesis, University of Dundee.Google Scholar
Al-Dabbas, M. A. M. & McManus, J. 1987. Shell fragments as indicators of bed sediment transport in the Tay Estuary. Proceedings of the Royal Society of Edinburgh 92B, 335344.Google Scholar
Craig, R. E. & Adams, J. A. 1970. The Firth of Tay, Hydrography and Plankton of Scottish Estuaries. Aberdeen: Report No. 3, DAFS Marine Laboratory, Aberdeen.Google Scholar
Döbereiner, C. 1982. On the aggregation and deposition of fine particles in the Tay Estuary. Ph.D. Thesis, University of Dundee.Google Scholar
Förstner, U. & Wittman, G. 1981. Metal pollution in the aquatic environment. Berlin: Springer.Google Scholar
Hashim, M. H. A. 1985. Tidal and seasonal chemical and mineralogical variation in the Tay Estuary. Ph.D. Thesis, University of Dundee.Google Scholar
Hubbard, F. H., McManus, J. & Al-Dabbas, M. A. M. 1981. Environmental influences on the shell mineralogy of Mytilus edulis. Geo-marine Letters 1, 267269.CrossRefGoogle Scholar
McGill, R. J. & Hubbard, F. H. 1981. Thin film k-value calibration for low atomic number elements using silicate mineral standards. In Proceedings of a Conference on Quantitative Microanalysis with High Spatial Resolution, UMIST, March 1981. Metals Society 111, 3034.Google Scholar
McManus, J. & Alizai, S. A. K. 1987. Variations in marsh surface levels in the upper Tay Estuary. Proceedings of the Royal Society of Edinburgh 92B, 345358.Google Scholar
Postma, H. 1967. Sediment transport and sedimentation in the marine environment. In Estuaries, ed. Lauff, G. H., pp. 224244. Washington: American Association for the Advancement of Science.Google Scholar
Price, N. B. & Angell, G. R. 1968. Determination of minor elements in rocks by thin film X-ray fluorescence techniques. Analytical Chemistry 40, 660663.CrossRefGoogle Scholar
Salomons, W. & Förstner, U. 1984. Metals in the hydrocycle. Berlin: Springer.Google Scholar
West, J. R. 1972. Water movements in the Tay Estuary. Proceedings of the Royal Society of Edinburgh 71B, 115129.Google Scholar