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J. Steele (1962)
ENVIRONMENTAL CONTROL OF PHOTOSYNTHESIS IN THE SEALimnology and Oceanography, 7
J. Talling (1957)
THE PHYTOPLANKTON POPULATION AS A COMPOUND PHOTOSYNTHETIC SYSTEMNew Phytologist, 56
(1960)
Beitr ~ ge zur Kenntnis optischer Eigenschaften der Gew ~ , sser und Prim ~ r - produktion
J. Talling (1957)
PHOTOSYNTHETIC CHARACTERISTICS OF SOME FRESHWATER PLANKTON DIATOMS IN RELATION TO UNDERWATER RADIATIONNew Phytologist, 56
J. Verduin (1956)
Primary Production in LakesLimnology and Oceanography, 1
J. Foster, S. Idso (1975)
Light and assimilation number in a small desert, recharged-groundwater pondOecologia, 18
(1970)
Models for calculating integral photosynthesis and some implications regarding structural properties of the community metabolism of aquatic systems, p. 455472
S. Idso (1969)
Atmospheric Attenuation of Solar Radiation.Journal of the Atmospheric Sciences, 26
H. Dwight, R. Romer (1934)
Tables of Integrals and Other Mathematical Data
J. Ryther (1956)
Photosynthesis in the Ocean as a Function of Light Intensity1Limnology and Oceanography, 1
J. Ryther, C. Yentsch (1957)
The Estimation of Phytoplankton Production in the Ocean from Chlorophyll and Light Data1Limnology and Oceanography, 2
J. Verduin (1956)
Energy Fixation and Utilization by Natural Communities in Western Lake ErieEcology, 37
(1965)
Standard correlations between pelagic photosynthesis and light
M. Abramowitz, I. Stegun, David Miller (1965)
Handbook of Mathematical Functions With Formulas, Graphs and Mathematical Tables (National Bureau of Standards Applied Mathematics Series No. 55)Journal of Applied Mechanics, 32
T. Kuehn, J. Ramsey, James Threlkeld (1970)
Thermal Environmental Engineering
R. Megard (1972)
PHYTOPLANKTON, PHOTOSYNTHESIS, AND PHOSPHORUS IN LAKE MINNETONKA, MINNESOTA1Limnology and Oceanography, 17
Emil Smith (1936)
Photosynthesis in Relation to Light and Carbon Dioxide.Proceedings of the National Academy of Sciences of the United States of America, 22 8
(1965)
Calculation models of photosynthesis-depth curves and some implications regarding day rate estimates in primary production measurements
R. Vollenweider (1958)
Sichttiefe und Produktion (Zusammenfassung), 13
Primary production in aquatic ecosystems is largely a function of irradiance, with photosynthetic response to light ranging from “light saturation” through “asymptotic inhibition” to “complete inhibition”. Equations describing these three basic types of response have been solved to yield instantaneous integral photosynthesis as a function of irradiance, chlorophyll a concentration, light extinction coefficient, and photosynthetic capacity of the phytoplankton at optimum irradiance. These results were used to calculate diurnal trends of instantaneous integral photosynthesis for several different latitudes and seasons and finally day-rate integrals of photosynthesis as a function of time of year at several latitudes. The final results allow rapid evaluation of the entire northern hemisphere in terms of potential sites for controlled aqua-culture facilities, using basic phytoplankton and water properties and standardized weather data. Results for the “complete inhibition” case can be used to evaluate both net and gross photosynthesis.
Oecologia – Springer Journals
Published: Jun 1, 1975
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