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Data · dataset · 1970

Carbonate saturation in the water column of station M8_056 off Cap Sao Vincente, Portugal (Table 1)

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Changes in the dissolved oxygen content, the alkalinity, and the pH in sea water near the ocean floor are interpreted in terms of chemical and biochemical processes at the sediment water interface.

Description

A simple model provides a plausible explanation of the observed phenomena. Special emphasis is given to the importance of borate corrections in the calculation of the solution effects of calcium carbonate.

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Inferred from text
Chemical oceanography 76% · Tabular 65%
Provenance · 1 source records, 8 field assertions
SourceKeyLast seenRaw
DataCite10.1594/pangaea.61151814 d agoJSON v1
FieldAssertionExtractorEvidence
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concepts[field].anzsrc:field:370802enrichment · DataCitetaxonomy-embedding@1.1.0title+keywords+description (76%)
concepts[modality].local:modality:tabularenrichment · DataCitekeyword-concept-rules@1.0.0title+description (65%)
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