Observations on plant nutrients in some Norwegian fjords

Abstract
Repeated measurements of concentrations of oxygen and different plant-nutrient species from 30 different fjords, all located in a small area of the Norwegian west coast, are discussed with special emphasis to organic matter composition, nutrient regeneration and nutrient sinks below the euphotic lone. Assuming that the organic matter is composed according to the Redfield ratios we find that a substantial denitrification must take place in the bottom sediments of the fjords. The importance of the denitrification process increases with the load of organic matter on the bottoms.

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