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A practical handbook of seawater analysis

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The article was published on 1968-01-01 and is currently open access. It has received 11288 citations till now. The article focuses on the topics: Seawater.

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Journal ArticleDOI

Improving the fluorometric ammonium method: matrix effects, background fluorescence, and standard additions

TL;DR: In this article, the authors proposed a new method for measuring a sample's background fluorescence that includes the background signal of the reagent or its interaction with the matrix constituents of the sample.
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The relationship between phytoplankton biovolume and chlorophyll in a deep oligotrophic lake: decoupling in their spatial and temporal maxima

TL;DR: The results show that changes in chlorophyll content per cell occur as a photoacclimation response along a vertical profile, and point out a component of the successional trends which appear in a phytoplankton growth phase in a lake.
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Development and Validation of an Estuarine Biotic Integrity Index

TL;DR: The Estuarine Biotic Integrity Index is suggested to be a useful indicator of estuarine ecosystem status because it reflects the relationship between anthropogenic alterations inEstuarine ecosystems and the status of higher trophic levels.
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Utilization of ammonium and nitrate during austral summer in the Scotia Sea

TL;DR: The nitrogenous nutrition of the phytoplankton in the Scotia Sea was investigated with 15 N tracer techniques during the austral summer of 1979 as discussed by the authors, and the results showed that phyto-ankton showed a consistent preference for NH 4 + utilization relative to NO 3 −.
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Dissimilatory reduction of nitrate to ammonium, not denitrification or anammox, dominates benthic nitrate reduction in tropical estuaries

TL;DR: In this article, benthic denitrification (DN) and dissimilatory reduction of nitrate to ammonium (DNRA) using the isotope-pairing technique in three tropical estuaries in Thailand (Mae Klong), Indonesia (Cisadane), and Fiji (Vunidawa-Rewa) during rainy, dry, and intermediate seasons along the salinity gradient of each estuary.