|
|
||||||||
ABSTRACT
Five salt solution systems containing HCO3- were concentrated by evaporation, in contact with laboratory atmosphere, to simulate 2-to 10-fold reduction in volume. The amounts of CaCO3 precipitated, final pH, and final solute concentrations were comprehensively predicted from the initial solute concentrations, degree of concentration of initial solution volume, and final PCO2. A flow diagram of the computational scheme is presented for IBM 7040 Data Processing System. The basic equilibrium relationships in the CaCO3 and HCO3--CO32- cycles are applicable to any aqueous systems which precipitate CaCO3 due to changes in solute concentration, partial pressure of CO2 or ambient temperature.
1 Contribution from the Department of Water Science and Engineering, University of California, Davis. This work was supported by funds from the Water Resources Center of the University of California. Computer facilities were made available through National Institutes of Health Grant FR00009.
2 Laboratory Technician IV and Professor of Water Science, respectively.
Received for publication June 28, 1965. Accepted for publication August 27, 1965.
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Journal of Plant Registrations | Journal of Environmental Quality |
The Plant Genome | |||