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Effect of nitrogen source and growth rate on phytoplankton-mediated changes in alkalinity1

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This article is published in Limnology and Oceanography.The article was published on 1980-03-01. It has received 132 citations till now. The article focuses on the topics: Phytoplankton.

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Total alkalinity: The explicit conservative expression and its application to biogeochemical processes

TL;DR: In this paper, an expression for total alkalinity (TA) in terms of the total concentrations of certain major ions (Na+, Cl−, Ca2+ etc) and the total concentration of various acid-base species (total phosphate etc) is derived from Dickson's original definition of TA under the constraint of electroneutrality.
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Impact of anthropogenic atmospheric nitrogen and sulfur deposition on ocean acidification and the inorganic carbon system

TL;DR: The alterations in surface water chemistry from anthropogenic nitrogen and sulfur deposition are a few percent of the acidification and DIC increases due to the oceanic uptake of anthropogenic CO2, however, the impacts are more substantial in coastal waters, where the ecosystem responses to ocean acidification could have the most severe implications for mankind.
Journal ArticleDOI

Acclimation and toxicity of high ammonium concentrations to unicellular algae

TL;DR: Chlorophytes were significantly more tolerant to high ammonium than diatoms, prymnesiophytes, dinoflagellates, and raphidophytes which were the least tolerant and toxicity is likely associated with the ammonium ion rather than ammonia.
Journal ArticleDOI

Production and export in a global ocean ecosystem model

TL;DR: The Hadley Centre Ocean Carbon Cycle (HadOCC) model as mentioned in this paper is a coupled physical-biogeochemical model of the ocean carbon cycle, which features an explicit representation of the marine ecosystem, which is assumed to be limited by nitrogen availability.
Journal ArticleDOI

Prediction of biological acid neutralization in acid-sensitive lakes

TL;DR: In this paper, the average mass transfer coefficients for sulfate and nitrate were obtained by two independent methods which agreed well with each other, and explained why lakes with short water residence times are especially susceptible to acidification.
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