The apparent dissociation constants of carbonic acid were
determined as functions of temperature and salinity in seawater
at atmospheric pressure.
There is fair agreement between my values of K'₁ and those
of Buch et al. (1932), Lyman (1956), and Hansson (1971). My values,
on the average, are 6.7% lower than Buch et al.'s (1932), 4.6%
smaller than Lyman's (1956), and 4.0% higher than Hansson's (1972).
My values for K'₂ are smaller than those reported by other
workers. They differ by 3.4% from Hansson's (1972) values, and
26% from Buch's (1938). Lyman's (1956) values are larger than
mine by 3.2% at temperatures of 25°C and below, and greater by
13.4% at 35°C. / Graduation date: 1973
| Identifer | oai:union.ndltd.org:ORGSU/oai:ir.library.oregonstate.edu:1957/28375 |
| Date | 09 March 1973 |
| Creators | Mehrbach, Carl |
| Contributors | Pytkowicz, Ricardo M. |
| Source Sets | Oregon State University |
| Language | en_US |
| Detected Language | English |
| Type | Thesis/Dissertation |
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