A steady-state diagenetic model for dissolved carbonate species and pH in the porewaters of oxic and suboxic sediments
- 1 July 1987
- journal article
- research article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 51 (7), 1985-1996
- https://doi.org/10.1016/0016-7037(87)90187-6
Abstract
No abstract availableKeywords
This publication has 45 references indexed in Scilit:
- Flux comparisons between sediments and sediment traps in the eastern tropical Pacific: Implications for atmospheric C02 variations during the Pleistocene1Limnology and Oceanography, 1985
- Carbonate chemistry in marine pore waters: MANOP sites C and SEarth and Planetary Science Letters, 1982
- Multicomponent electrolyte diffusion corrections for North Atlantic sedimentAmerican Journal of Science, 1982
- Mass transfer enhanced by equilibrium reactionsIndustrial & Engineering Chemistry Fundamentals, 1982
- Carbon dioxide hydration and dehydration kinetics in seawater1Limnology and Oceanography, 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
- The dissolution kinetics of biogenic calcium carbonates in seawaterGeochimica et Cosmochimica Acta, 1980
- Facilitated transport via carrier—mediated diffusion in membranes: Part II. Mathematical aspects and analysesAIChE Journal, 1974
- Nonequilibrium facilitated diffusion of oxygen through membranes of aqueous cobaltodihistidineBiochimica et Biophysica Acta (BBA) - Biomembranes, 1970