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79) 35 s e d i m e n t a t i o n rates, tigations. and should be given p r i o r i t y for s u b s e q u e n t inves- To c o m p l e m e n t this, surface sediment as w e l l as a sample from d e e p e r sections mined. (current contamination) (10-20 cm depth) could be exa- In e n v i r o n m e n t s w i t h a r e l a t i v e l y u n i f o r m s e d i m e n t a t i o n , for e x a m p l e in lakes and in m a r i n e coastal basins, w h e r e the d e p o s i t s are f i n e - g r a i n e d and o c c u r at a rate of 1 to 5 mm/yr, a more favourable p r o c e d u r e involves the taking of v e r t i c a l p r o f i l e s w i t h a g r a v i t y or valve corer (see Figure 3-2).

G r e a t L a k e s Res. 4, 287-294. W. et al. (1974) S e d i m e n t a t i o n rates and recent sediment h i s t o r y of Lakes Ontario, Erie and Huron. J. Sediment. Petrol. 44, 469-490. W. (1984) T o x i c C o n t a m i n a n t s in the N i a g a r a River, 1975-1982. Techn. Bull. Water Quality Branch, Ontario Region No. 134, 47 p. Burlington: Canada Centre for Inland Waters. W. D. (1983) C h l o r i n a t e d organic c o n t a m i n a n t s in w a t e r and suspended sediments of the lower Niagara River.

Ernst, pp. 12-17. Edinburgh: CEP Consultants. H. et al. (1988) Chernobyl radionuclides in the environment: Tracers for the tight coupling of atmospheric, terrestrial, and aquatic geochemical processes. Environ. Sci. Technol. 22, 510-516. Stumm, W. & Baccini, P. (1978) Man-made chemical perturbation of lakes. In L a k e s - Chemistry, Geology, Physics, ed. A. Lerman, pp. 91126. New York: Springer-Verlag. T. (1980) Applications of Hudson River basin PCB-transport studies. In C o n t a m i n a n t s and Sediments, ed.

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