Redfield ratio

E523536

The Redfield ratio is a canonical stoichiometric relationship describing the consistent atomic proportions of carbon, nitrogen, and phosphorus found in marine organic matter and dissolved nutrients in the ocean.

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Statements (40)

Predicate Object
instanceOf biogeochemical ratio
oceanographic concept
stoichiometric relationship
acknowledges regional deviations from canonical stoichiometry
appliesPrimarilyTo open ocean conditions
appliesTo dissolved nutrients in the ocean
marine organic matter
assumes relatively constant elemental composition of marine organic matter
characterizes average composition of dissolved inorganic nutrients in the open ocean
average composition of marine particulate organic matter
average composition of marine phytoplankton
contrastedWith variable stoichiometry in coastal and upwelling regions
describes stoichiometric relationship of carbon, nitrogen, and phosphorus in marine systems
field biological oceanography
chemical oceanography
marine biogeochemistry
hasApproximateMassRatio C:N:P ≈ 41:7:1
hasCanonicalAtomicRatio C:N:P = 106:16:1
hasCarbonToNitrogenRatio C:N = 106:16
hasCarbonToPhosphorusRatio C:P = 106:1
hasNitrogenToPhosphorusRatio N:P = 16:1
hasTypicalUnit molar ratio
historicalPublicationYear 1934
implies fixed relationship between nutrient consumption and organic matter production in the open ocean
influences design of ocean fertilization experiments
interpretation of nutrient uptake measurements
parameterization of ecosystem models
namedAfter Alfred C. Redfield NERFINISHED
refinedInPublicationYear 1958
relatedTo biological pump
global carbon cycle
nitrogen cycle
nutrient limitation theory
phosphorus cycle
supports link between ocean nutrient inventories and biological processes
usedFor constraining global biogeochemical models
estimating export production from nutrient data
estimating nutrient limitation in the ocean
interpreting ocean nutrient distributions
modeling marine primary production

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Redfield notableFor Redfield ratio
subject surface form: Alfred C. Redfield