A comparison of closed- and open-system models for porewater pH and calcite-saturation state
- 3 April 2003
- journal article
- Published by Elsevier
- Vol. 57 (2) , 317-334
- https://doi.org/10.1016/0016-7037(93)90434-x
Abstract
No abstract availableKeywords
This publication has 66 references indexed in Scilit:
- Sulfate reduction in deep-sea sedimentsAmerican Journal of Science, 1991
- The solubility of calcite and aragonite in sulfate-free seawater and the seeded growth kinetics and composition of the precipitates at 25°CChemical Geology, 1989
- Reduced state relationship for limiting electrical conductances of aqueous ions over wide ranges of temperature and pressureThe Journal of Chemical Physics, 1987
- Anaerobic mineralization of marine sediment organic matter: Rates and the role of anaerobic processes in the oceanic carbon economyGeomicrobiology Journal, 1987
- The free-solution diffusion coefficient of boron: influence of dissolved organic matterMarine Chemistry, 1986
- Mass transfer enhanced by equilibrium reactionsIndustrial & Engineering Chemistry Fundamentals, 1982
- Dissolution of calcite in the deep-sea; theoretical prediction for the case of uniform size particles settling into a well-mixed sedimentAmerican Journal of Science, 1982
- Influence of diffusion coupling on diagenetic concentration profilesAmerican Journal of Science, 1981
- Algorithm 554: BRENTM, A Fortran Subroutine for the Numerical Solution of Nonlinear Equations [C5]ACM Transactions on Mathematical Software, 1980
- Early diagenesis in a reducing fjord, Saanich Inlet, British Columbia—I. chemical and isotopic changes in major components of interstitial waterGeochimica et Cosmochimica Acta, 1972