Factors controlling the temporal variability in dissolved oxygen regime of salmon spawning gravels

Author:

Sear D. A.1,Pattison I.1,Collins A. L.2,Newson M. D.3,Jones J. I.4,Naden P. S.5,Carling P. A.1

Affiliation:

1. Department of Geography; University of Southampton; Highfield Southampton S017 1BJ UK

2. Soils, Agriculture and Water; ADAS; Woodthorne, Wergs Road Wolverhampton WV6 8TQ, West Midlands UK

3. Tyne Rivers Trust; Horesley Northumberland NE15 OPA UK

4. School of Biological and Chemical Sciences; Queen Mary University of London; Mile End Road London E1 4NS UK

5. Centre for Ecology and Hydrology; Crowmarsh Gifford Wallingford Oxon UK

Publisher

Wiley

Subject

Water Science and Technology

Reference81 articles.

1. Water temperatures within spawning beds in two chalk streams and implications for salmonid egg development;Acornley;Hydrological Processes,1999

2. Sediment transport and the siltation of salmonid spawning gravels in a groundwater dominated river;Acornley;Hydrological Processes,1999

3. Alonso CV Theurer FD Zachman DW 1996 Sediment Intrusion and dissolved oxygen transport model - SIDO 232

4. Detection of Regional Trends in Salmonid Habitat in Coastal Streams, Oregon;Anlauf;Transactions of the American Fisheries Society,2011

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