Solubility of aragonite in seawater--II. Effect of pressure on the onset and maintenance of dissolution

Details Solubility of aragonite in seawater--II. Effect of pressure on the onset and maintenance of dissolution Solubility of aragonite in seawater--II. Effect of pressure on the onset and maintenance of dissolution

Aug 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980gecoa..44.1077c&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 44, Issue 8, pp.1077-1080

Computer Science

Scientific paper

The apparent solubility product ( K ' sp ) of aragonite in a variety of seawater compositions has been determined at pressures from 0 to 1019 atm and a nomogram developed to allow the determination of the K ' sp when the apparent ion product (AIP) at one atmosphere and the collection depth of a water sample are known. This nomogram provides a basis from which the onset of aragonite dissolution can be determined for conditions representative of aragonite sedimentation through the changing water masses of the open ocean.

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