Published:
August 1, 1987
Originator:
Chesapeake Bay Program

In general, it has been well established that nitrogen is the key nutrient most often controlling rates of primary production in estuarine water (Ryther and Dunstand 1071; Goldman et al. 1973; Boynton et al. 1982). Based on a survey of data from some 60 nearshore and estuarine waters, Boynton et al. (1982) reported that N:P ratios were generally less than 10 which indicate that primary producers would exhaust necessary supplies of nitrogen prior to phosphorus if there were sufficient demand for those compounds (Redfield 1934).

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