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This report presents experimental data on the densities of saturated NaCl and KCl solutions from 10° to 105°C. Glass hydrometers were used to measure the specific gravity of saturated salt solutions, which were then converted to densities. The densities were fit to regression equations and compared to previous literature values. The new data set is considered the most reliable and should be used in models of brine migration in salt repositories from 10° to 85°C, while values from Haas (1976) are recommended

Author

Kashilal Indra

Language

EN